https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&feed=atom&action=history
Eastern Granite-Rhyolite Province (Basement) - Revision history
2024-03-28T21:35:57Z
Revision history for this page on the wiki
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Jennifer.Obrad at 20:13, 4 February 2021
2021-02-04T20:13:00Z
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17272&oldid=prev
Alan.Myers at 14:42, 22 October 2019
2019-10-22T14:42:42Z
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Alan.Myers
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17262&oldid=prev
Jennifer.Obrad at 14:19, 22 October 2019
2019-10-22T14:19:11Z
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|category1=Precambrian</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>|category1=Precambrian</div></td></tr>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17260&oldid=prev
Jennifer.Obrad: IlLex moved page Basement - Eastern Granite-Rhyolite Province to Eastern Granite-Rhyolite Province (Basement) without leaving a redirect
2019-10-22T14:17:04Z
<p>IlLex moved page <a href="/index.php?title=Basement_-_Eastern_Granite-Rhyolite_Province&action=edit&redlink=1" class="new" title="Basement - Eastern Granite-Rhyolite Province (page does not exist)">Basement - Eastern Granite-Rhyolite Province</a> to <a href="/wiki/Eastern_Granite-Rhyolite_Province_(Basement)" title="Eastern Granite-Rhyolite Province (Basement)">Eastern Granite-Rhyolite Province (Basement)</a> without leaving a redirect</p>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17033&oldid=prev
Jennifer.Obrad: /* References */
2019-10-07T22:09:53Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Marshak, S., and T. Paulsen, 1996, Midcontinent US fault and fold zones: a legacy of Proterozoic intracratonic extensional tectonism?: Geology, v. 24 (2), p. 151–154. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Marshak, S., and T. Paulsen, 1996, Midcontinent US fault and fold zones: a legacy of Proterozoic intracratonic extensional tectonism?: Geology, v. 24 (2), p. 151–154. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*McBride, J.H., and D.R. Kolata, 1999, Upper crust beneath the central Illinois basin, United States: Geological Society of America Bulletin, v. 111, p. 375–394. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*McBride, J.H., and D.R. Kolata, 1999, Upper crust beneath the central Illinois basin, United States: Geological Society of America Bulletin, v. 111, p. 375–394. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>*McBride, J.H., D.R. Kolata, and T.G. Hildenbrand, 2003, Geophysical constraints on understanding the origin of the Illinois basin and its underlying crust: Tectonophysics, v. </div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>*McBride, J.H., D.R. Kolata, and T.G. Hildenbrand, 2003, Geophysical constraints on understanding the origin of the Illinois basin and its underlying crust: Tectonophysics, v. 363, p. 45–78. <br> </div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>363, p. 45–78. <br> </div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*McBride, J.H., H.E. Leetaru, R.W. Keach, and E.I. McBride, 2016, Fine-scale structure of the Precambrian beneath the Illinois basin: Geosphere, v. 12, p. 585–606. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*McBride, J.H., H.E. Leetaru, R.W. Keach, and E.I. McBride, 2016, Fine-scale structure of the Precambrian beneath the Illinois basin: Geosphere, v. 12, p. 585–606. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Moores, E.M., 1991, Southwest US-East Antarctic (SWEAT) connection: a hypothesis: Geology, v. 19, p. 425–428. <br> </div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Moores, E.M., 1991, Southwest US-East Antarctic (SWEAT) connection: a hypothesis: Geology, v. 19, p. 425–428. <br> </div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Van Schmus, W.R., L.G. Medaris Jr., and P.O. Banks, 1975, Geology and age of the wolf river batholith, Wisconsin: Geological Society of America Bulletin, v. 86, p. 907–914. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Van Schmus, W.R., L.G. Medaris Jr., and P.O. Banks, 1975, Geology and age of the wolf river batholith, Wisconsin: Geological Society of America Bulletin, v. 86, p. 907–914. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Van Schmus, W.R., M.E. Bickford, and A. Turek, 1996, Proterozoic geology of the east-central midcontinent basement, ''in'' Geological Society of America Special Paper, v. 308, p. 7–32. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Van Schmus, W.R., M.E. Bickford, and A. Turek, 1996, Proterozoic geology of the east-central midcontinent basement, ''in'' Geological Society of America Special Paper, v. 308, p. 7–32. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Whitmeyer, S.J., and K.E. Karlstrom, 2007, Tectonic model for the Proterozoic growth of North America: Geosphere, v. 3, p. 220–259. <br></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*</ins>Whitmeyer, S.J., and K.E. Karlstrom, 2007, Tectonic model for the Proterozoic growth of North America: Geosphere, v. 3, p. 220–259. <br></div></td></tr>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17032&oldid=prev
Jennifer.Obrad: /* References */
2019-10-07T22:08:34Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Craddock, J.P., S.D. Craddock, A. Konstantinou, A.R. Kylander-Clark, and D.H. Malone, 2017a, Calcite twinning strain variations across the Proterozoic Grenville orogen and Keweenaw-Kapuskasing inverted foreland, USA and Canada. Geoscience Frontiers, v. 8, p. 1357–1384. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Craddock, J.P., S.D. Craddock, A. Konstantinou, A.R. Kylander-Clark, and D.H. Malone, 2017a, Calcite twinning strain variations across the Proterozoic Grenville orogen and Keweenaw-Kapuskasing inverted foreland, USA and Canada. Geoscience Frontiers, v. 8, p. 1357–1384. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Dalziel, I.W., 1991, Pacific margins of Laurentia and East Antarctica–Australia as a conjugate rift pair: evidence and implications for an Eocambrian supercontinent: Geology, v. 19, p. 598–601. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Dalziel, I.W., 1991, Pacific margins of Laurentia and East Antarctica–Australia as a conjugate rift pair: evidence and implications for an Eocambrian supercontinent: Geology, v. 19, p. 598–601. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>*Denison, R.E., M.E. Bickford, E.G. Lidiak, and E.B. Kisvarsanyi, 1987, Geology and Geochronology of Precambrian Rocks in the Central Interior Region of the United</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>*Denison, R.E., M.E. Bickford, E.G. Lidiak, and E.B. Kisvarsanyi, 1987, Geology and Geochronology of Precambrian Rocks in the Central Interior Region of the United States: U.S. Geological Survey, Professional Paper 1241-C. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>States: U.S. Geological Survey, Professional Paper 1241-C. <br></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Dewane, T.J., and W.R. Van Schmus, 2007, U–Pb geochronology of the Wolf River batholith, north-central Wisconsin: evidence for successive magmatism between 1484 Ma and 1468 Ma: Precambrian Research, v. 157, p. 215–234. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Dewane, T.J., and W.R. Van Schmus, 2007, U–Pb geochronology of the Wolf River batholith, north-central Wisconsin: evidence for successive magmatism between 1484 Ma and 1468 Ma: Precambrian Research, v. 157, p. 215–234. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Dickin, A.P., and M.D. Higgins, 1992, Sm/Nd evidence for a major 1.5 Ga crust-forming event in the central Grenville province: Geology, v. 20, p. 137–140. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Dickin, A.P., and M.D. Higgins, 1992, Sm/Nd evidence for a major 1.5 Ga crust-forming event in the central Grenville province: Geology, v. 20, p. 137–140. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>*Freiburg, J.T., D.G. Morse, H.E. Leetaru, R.P. Hoss, and Q. Yan, 2014, A Depositional and Diagenetic Characterization of the Mt. Simon Sandstone at the Illinois Basin –</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>*Freiburg, J.T., D.G. Morse, H.E. Leetaru, R.P. Hoss, and Q. Yan, 2014, A Depositional and Diagenetic Characterization of the Mt. Simon Sandstone at the Illinois Basin – Decatur Project Carbon Capture and Storage Site, Decatur, Illinois, USA: Illinois State Geological Survey, Circular 583, 59 p. and 3 digital appendices. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Decatur Project Carbon Capture and Storage Site, Decatur, Illinois, USA: Illinois State Geological Survey, Circular 583, 59 p. and 3 digital appendices. <br></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Gower, C.F., and R.D. Tucker, 1994, Distribution of pre-1400 Ma crust in the Grenville province: implications for rifting in Laurentia-Baltica during geon 14: Geology, v. 22, p. 827–830. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Gower, C.F., and R.D. Tucker, 1994, Distribution of pre-1400 Ma crust in the Grenville province: implications for rifting in Laurentia-Baltica during geon 14: Geology, v. 22, p. 827–830. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Hill, B.M., and M.E. Bickford, 2001, Paleoproterozoic rocks of central Colorado: accreted arcs or extended older crust?: Geology, v. 29, p. 1015–1018.<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Hill, B.M., and M.E. Bickford, 2001, Paleoproterozoic rocks of central Colorado: accreted arcs or extended older crust?: Geology, v. 29, p. 1015–1018.<br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>*Hoffman, P.F., 1989. Precambrian geology and tectonic history of North America, ''in'' Bally, A.W., and A.R. Palmer, eds., The Geology of North America—An Overview.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>*Hoffman, P.F., 1989. Precambrian geology and tectonic history of North America, ''in'' Bally, A.W., and A.R. Palmer, eds., The Geology of North America—An Overview. Decade of North American Geology, Volume A: Geological Society of America, p. 447–512. <br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>Decade of North American Geology, Volume A: Geological Society of America, p. 447–512. <br></div></td><td colspan="2" class="diff-side-added"></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Hoppe, W.J., C.W. Montgomery, and W.R. Van Schmus, 1983, Age and significance of Precambrian basement samples from northern Illinois and adjacent states. Journal of Geophysical Research, Solid Earth v. 88, p. 7276–7286. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Hoppe, W.J., C.W. Montgomery, and W.R. Van Schmus, 1983, Age and significance of Precambrian basement samples from northern Illinois and adjacent states. Journal of Geophysical Research, Solid Earth v. 88, p. 7276–7286. <br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Karlstrom, K.E., and S.A. Bowring, 1988, Early Proterozoic assembly of tectonostratigraphic terranes in southwestern North America: Journal of Geology, v. 96, p. 561–576. <br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>*Karlstrom, K.E., and S.A. Bowring, 1988, Early Proterozoic assembly of tectonostratigraphic terranes in southwestern North America: Journal of Geology, v. 96, p. 561–576. <br></div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17031&oldid=prev
Jennifer.Obrad: /* References */
2019-10-07T22:03:35Z
<p><span dir="auto"><span class="autocomment">References</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 22:03, 7 October 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Barnes, M.A., C.R. Rohs, E.Y. Anthony, W.R. Van Schmus, and R.E. Denison, 1999, Isotopic and elemental chemistry of subsurface Precambrian igneous rocks, west Texas and eastern New Mexico: Rocky Mountain Geology, v. 34, p. 245–262.<br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Bickford, M.E., W.R. Van, and I. Zietz, 1986, Proterozoic history of the midcontinent region of North America: Geology, v. 14, p. 492–496. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Bickford, M.E., W.R. Van Schmus, K.E. Karlstrom, P.A. Mueller, and G.D. Kamenov, 2015, Mesoproterozoic–trans-Laurentian magmatism: a synthesis of continent-wide age distributions, new SIMS U-Pb ages, zircon saturation temperatures, and Hf and Nd isotopic compositions: Precambrian Research, v. 265, p. 286–312. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Bowring, S.A., and K.E. Karlstrom, 1990, Growth, stabilization, and reactivation of Proterozoic lithosphere in the southwestern United States: Geology, v. 18, p. 1203–1206. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Bowring, S.A., T.B. Housh, W.R. Van Schmus, and F.A. Podosek, 1992, A major Nd isotopic boundary along the southern margin of Laurentia: Eos, v. 73, p. 333.<br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Craddock, J.P., S.D. Craddock, A. Konstantinou, A.R. Kylander-Clark, and D.H. Malone, 2017a, Calcite twinning strain variations across the Proterozoic Grenville orogen and Keweenaw-Kapuskasing inverted foreland, USA and Canada. Geoscience Frontiers, v. 8, p. 1357–1384. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Dalziel, I.W., 1991, Pacific margins of Laurentia and East Antarctica–Australia as a conjugate rift pair: evidence and implications for an Eocambrian supercontinent: Geology, v. 19, p. 598–601. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Denison, R.E., M.E. Bickford, E.G. Lidiak, and E.B. Kisvarsanyi, 1987, Geology and Geochronology of Precambrian Rocks in the Central Interior Region of the United</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">States: U.S. Geological Survey, Professional Paper 1241-C. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Dewane, T.J., and W.R. Van Schmus, 2007, U–Pb geochronology of the Wolf River batholith, north-central Wisconsin: evidence for successive magmatism between 1484 Ma and 1468 Ma: Precambrian Research, v. 157, p. 215–234. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Dickin, A.P., and M.D. Higgins, 1992, Sm/Nd evidence for a major 1.5 Ga crust-forming event in the central Grenville province: Geology, v. 20, p. 137–140. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Freiburg, J.T., D.G. Morse, H.E. Leetaru, R.P. Hoss, and Q. Yan, 2014, A Depositional and Diagenetic Characterization of the Mt. Simon Sandstone at the Illinois Basin –</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Decatur Project Carbon Capture and Storage Site, Decatur, Illinois, USA: Illinois State Geological Survey, Circular 583, 59 p. and 3 digital appendices. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Gower, C.F., and R.D. Tucker, 1994, Distribution of pre-1400 Ma crust in the Grenville province: implications for rifting in Laurentia-Baltica during geon 14: Geology, v. 22, p. 827–830. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Hill, B.M., and M.E. Bickford, 2001, Paleoproterozoic rocks of central Colorado: accreted arcs or extended older crust?: Geology, v. 29, p. 1015–1018.<br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Hoffman, P.F., 1989. Precambrian geology and tectonic history of North America, ''in'' Bally, A.W., and A.R. Palmer, eds., The Geology of North America—An Overview.</ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Decade of North American Geology, Volume A: Geological Society of America, p. 447–512. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Hoppe, W.J., C.W. Montgomery, and W.R. Van Schmus, 1983, Age and significance of Precambrian basement samples from northern Illinois and adjacent states. Journal of Geophysical Research, Solid Earth v. 88, p. 7276–7286. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Karlstrom, K.E., and S.A. Bowring, 1988, Early Proterozoic assembly of tectonostratigraphic terranes in southwestern North America: Journal of Geology, v. 96, p. 561–576. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Karlstrom, K.E., and E.D. Humphreys, 1998, Persistent influence of Proterozoic accretionary boundaries in the tectonic evolution of southwestern North America: Rocky Mountain Geology, v. 33, p. 161–179. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Kolata, D.R., and W.J. Nelson, 2010, Tectonic history, ''in'' Kolata, D.R., and C.K. Nimz eds., Geology of Illinois, Illinois State Geological Survey, p. 77–89. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Lidiak, E.G., R.F. Marvin, H.H. Thomas, and M.N. Bass, 1966, Geochronology of the midcontinent region of the United States: Part 4. Eastern region: Journal of Geophysical Research, v. 71, p. 5427–5438. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Marshak, S., and T. Paulsen, 1996, Midcontinent US fault and fold zones: a legacy of Proterozoic intracratonic extensional tectonism?: Geology, v. 24 (2), p. 151–154. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*McBride, J.H., and D.R. Kolata, 1999, Upper crust beneath the central Illinois basin, United States: Geological Society of America Bulletin, v. 111, p. 375–394. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*McBride, J.H., D.R. Kolata, and T.G. Hildenbrand, 2003, Geophysical constraints on understanding the origin of the Illinois basin and its underlying crust: Tectonophysics, v. </ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">363, p. 45–78. <br> </ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*McBride, J.H., H.E. Leetaru, R.W. Keach, and E.I. McBride, 2016, Fine-scale structure of the Precambrian beneath the Illinois basin: Geosphere, v. 12, p. 585–606. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Moores, E.M., 1991, Southwest US-East Antarctic (SWEAT) connection: a hypothesis: Geology, v. 19, p. 425–428. <br> </ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Mosher, S., 1998, Tectonic evolution of the southern Laurentian Grenville orogenic belt: Geological Society of America Bulletin, v. 110, p. 1357–1375. <br> </ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Patchett, P.J., 1989, Radiogenic isotope geochemistry of rare earth elements: Reviews in Mineralogy and Geochemistry, v. 21, p. 25–44. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Patchett, P.J., and J. Ruiz, 1989, Nd isotopes and the origin of Grenville-age rocks in Texas: implications for Proterozoic evolution of the United States mid-continent region: Journal of Geology, v. 97, p. 685–695. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Pratt, T., R. Culotta, E. Hauser, D. Nelson, L. Brown, S. Kaufman, and W. Hinze, 1989, Major Proterozoic basement features of the eastern midcontinent of North America revealed by recent COCORP profiling: Geology, v. 17, p. 505–509. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Pratt, T.L., E.C. Hauser, and K.D. Nelson, 1992, Widespread buried Precambrian layered sequences in the US Mid-Continent: evidence for large Proterozoic depositional basins: American Association of Petroleum Geologists Bulletin, v. 76, p. 1384–1401. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Rivers, T., 1997, Lithotectonic elements of the Grenville province: review and tectonic implications: Precambrian Research, v. 86, p. 117–154. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Van Schmus, W.R., L.G. Medaris Jr., and P.O. Banks, 1975, Geology and age of the wolf river batholith, Wisconsin: Geological Society of America Bulletin, v. 86, p. 907–914. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">*Van Schmus, W.R., M.E. Bickford, and A. Turek, 1996, Proterozoic geology of the east-central midcontinent basement, ''in'' Geological Society of America Special Paper, v. 308, p. 7–32. <br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">Whitmeyer, S.J., and K.E. Karlstrom, 2007, Tectonic model for the Proterozoic growth of North America: Geosphere, v. 3, p. 220–259. <br></ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{{Codes}}</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>{{Codes}}</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17030&oldid=prev
Jennifer.Obrad: /* Environments of deposition */
2019-10-04T20:59:13Z
<p><span dir="auto"><span class="autocomment">Environments of deposition</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 20:59, 4 October 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Seismic reflection data reveal the EGRP as being structurally complex in Illinois (Pratt et al., 1989). Before the Paleozoic Illinois Basin formed, a similar structural depression, referred to as the proto-Illinois Basin, formed between 1.48 Ga and 500 Ma (Kolata and Nelson, 2010) and may be evidence of rifting in central Illinois (Marshak and Paulsen, 1996). Despite the lack of drill holes penetrating Precambrian rocks perceived to be part of the proto-Illinois Basin, evidence for the early basin is two-fold:<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Seismic reflection data reveal the EGRP as being structurally complex in Illinois (Pratt et al., 1989). Before the Paleozoic Illinois Basin formed, a similar structural depression, referred to as the proto-Illinois Basin, formed between 1.48 Ga and 500 Ma (Kolata and Nelson, 2010) and may be evidence of rifting in central Illinois (Marshak and Paulsen, 1996). Despite the lack of drill holes penetrating Precambrian rocks perceived to be part of the proto-Illinois Basin, evidence for the early basin is two-fold:<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>:(1) A prominent layered sequence of subhorizontal seismic reflectors appears to sag into a depression that lies north of the Illinois Basin depocenter (McBride et al., 2003). This layered succession is referred to as the Centralia sequence (Pratt et al., 1989, 1992) and exhibits a geometry that strongly suggests a succession of layered rocks that have been postulated as sedimentary or volcanic in origin (McBride and Kolata, 1999).<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>:(1) A prominent layered sequence of subhorizontal seismic reflectors appears to sag into a depression that lies north of the Illinois Basin depocenter (McBride et al., 2003). This layered succession is referred to as the Centralia sequence (Pratt et al., 1989, 1992) and exhibits a geometry that strongly suggests a succession of layered rocks that have been postulated as sedimentary or volcanic in origin (McBride and Kolata, 1999).<br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:(2) The Centralia sequence is overlain by the Mt. Simon Sandstone, which has a depocenter in east-central Illinois approximately 300km (186 mi) north of the post-Mt. Simon Paleozoic sediment depocenter (the Illinois Basin in southern Illinois; Freiburg et al., 2014). The thickness trends of the Mt. Simon roughly coincide with that of the underlying Centralia succession, suggesting a similar subsidence event that accommodates both units (McBride et al., 2003). Prominent pinch-out boundaries of the Centralia sequence are observed on seismic profiles in west-central and south-central Illinois (Pratt et al., 1989; McBride and Kolata, 1999; McBride et al., 2003) and may correspond to a rift <del style="font-weight: bold; text-decoration: none;">bound-ary</del>, as marked by the Nd line of Van Schmus et al. (1996) and McBride et al. (2016).<br></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;"><br></ins></div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:(2) The Centralia sequence is overlain by the Mt. Simon Sandstone, which has a depocenter in east-central Illinois approximately 300km (186 mi) north of the post-Mt. Simon Paleozoic sediment depocenter (the Illinois Basin in southern Illinois; Freiburg et al., 2014). The thickness trends of the Mt. Simon roughly coincide with that of the underlying Centralia succession, suggesting a similar subsidence event that accommodates both units (McBride et al., 2003). Prominent pinch-out boundaries of the Centralia sequence are observed on seismic profiles in west-central and south-central Illinois (Pratt et al., 1989; McBride and Kolata, 1999; McBride et al., 2003) and may correspond to a rift <ins style="font-weight: bold; text-decoration: none;">boundary</ins>, as marked by the Nd line of Van Schmus et al. (1996) and McBride et al. (2016).<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Economic importance==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Economic importance==</div></td></tr>
</table>
Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17029&oldid=prev
Jennifer.Obrad: /* Remarks */
2019-10-04T20:21:04Z
<p><span dir="auto"><span class="autocomment">Remarks</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 20:21, 4 October 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Remarks==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Remarks==</div></td></tr>
<tr><td colspan="2" class="diff-side-deleted"></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div><ins style="font-weight: bold; text-decoration: none;">The Centralia sequence (as mentioned above), is defined by seismic reflection. It's lithology is not well defined.</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br/></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==References==</div></td></tr>
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Jennifer.Obrad
https://ilstratwiki.web.illinois.edu/index.php?title=Eastern_Granite-Rhyolite_Province_(Basement)&diff=17028&oldid=prev
Jennifer.Obrad: /* Environments of deposition */
2019-10-04T20:19:20Z
<p><span dir="auto"><span class="autocomment">Environments of deposition</span></span></p>
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 20:19, 4 October 2019</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Seismic reflection data reveal the EGRP as being structurally complex in Illinois (Pratt et al., 1989). Before the Paleozoic Illinois Basin formed, a similar structural depression, referred to as the proto-Illinois Basin, formed between 1.48 Ga and 500 Ma (Kolata and Nelson, 2010) and may be evidence of rifting in central Illinois (Marshak and Paulsen, 1996). Despite the lack of drill holes penetrating Precambrian rocks perceived to be part of the proto-Illinois Basin, evidence for the early basin is two-fold:<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>Seismic reflection data reveal the EGRP as being structurally complex in Illinois (Pratt et al., 1989). Before the Paleozoic Illinois Basin formed, a similar structural depression, referred to as the proto-Illinois Basin, formed between 1.48 Ga and 500 Ma (Kolata and Nelson, 2010) and may be evidence of rifting in central Illinois (Marshak and Paulsen, 1996). Despite the lack of drill holes penetrating Precambrian rocks perceived to be part of the proto-Illinois Basin, evidence for the early basin is two-fold:<br></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>:(1) A prominent layered sequence of subhorizontal seismic reflectors appears to sag into a depression that lies north of the Illinois Basin depocenter (McBride et al., 2003). This layered succession is referred to as the Centralia sequence (Pratt et al., 1989, 1992) and exhibits a geometry that strongly suggests a succession of layered rocks that have been postulated as sedimentary or volcanic in origin (McBride and Kolata, 1999).<br></div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>:(1) A prominent layered sequence of subhorizontal seismic reflectors appears to sag into a depression that lies north of the Illinois Basin depocenter (McBride et al., 2003). This layered succession is referred to as the Centralia sequence (Pratt et al., 1989, 1992) and exhibits a geometry that strongly suggests a succession of layered rocks that have been postulated as sedimentary or volcanic in origin (McBride and Kolata, 1999).<br></div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:(2) The Centralia sequence is overlain by the Mt. Simon Sandstone, which has a depocenter in east-central Illinois approximately 300km (186 mi) north of the post-Mt. Simon Paleozoic sediment depocenter (the Illinois Basin in southern Illinois; Freiburg et al., 2014). The thickness trends of the Mt. Simon roughly coincide with that of the underlying Centralia succession, suggesting a similar subsidence event that accommodates both units (McBride et al., 2003). Prominent pinch-out boundaries of the Centralia sequence are observed on seismic profiles in west-central and south-central Illinois (Pratt et al., 1989; McBride and Kolata, 1999; McBride et al., 2003) and may correspond to a rift bound-ary, as marked by the Nd line of Van Schmus et al. (1996) and McBride et al. (2016<del style="font-weight: bold; text-decoration: none;">) (Figs. 1 and 2</del>).<br></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:(2) The Centralia sequence is overlain by the Mt. Simon Sandstone, which has a depocenter in east-central Illinois approximately 300km (186 mi) north of the post-Mt. Simon Paleozoic sediment depocenter (the Illinois Basin in southern Illinois; Freiburg et al., 2014). The thickness trends of the Mt. Simon roughly coincide with that of the underlying Centralia succession, suggesting a similar subsidence event that accommodates both units (McBride et al., 2003). Prominent pinch-out boundaries of the Centralia sequence are observed on seismic profiles in west-central and south-central Illinois (Pratt et al., 1989; McBride and Kolata, 1999; McBride et al., 2003) and may correspond to a rift bound-ary, as marked by the Nd line of Van Schmus et al. (1996) and McBride et al. (2016).<br></div></td></tr>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Economic importance==</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>==Economic importance==</div></td></tr>
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Jennifer.Obrad