http://wiki.geodynamics.umaine.edu/index.php?action=history&feed=atom&title=Glacial_Loading_and_Tectonics_Figure_1 2026-10-29T02:10:08Z Revision history for this page on the wiki MediaWiki 1.30.0 http://wiki.geodynamics.umaine.edu/index.php?title=Glacial_Loading_and_Tectonics_Figure_1&diff=402&oldid=prev 2015-03-18T16:05:51Z

<p></p> <table class="diff diff-contentalign-left" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr style="vertical-align: top;" lang="en"> <td colspan="2" style="background-color: white; color:black; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: white; color:black; text-align: center;">Revision as of 16:05, 18 March 2015</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1" >Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</td></tr> <tr><td class='diff-marker'>&#160;</td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>[[File:GLTFig1.png|center|500px]]</div></td><td class='diff-marker'>&#160;</td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>[[File:GLTFig1.png|center|500px]]</div></td></tr> <tr><td class='diff-marker'>&#160;</td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>'''Figure 1.'''</div></td><td class='diff-marker'>&#160;</td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>'''Figure 1.'''</div></td></tr> <tr><td class='diff-marker'>−</td><td style="color:black; 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>STEEP01 and STEEP02 refraction profiles (Worthington et al. 2012; Christeson et al. 2010). A. Location map of local tectonics, Kayak Island Zone (KIZ), Pamplona Fault Zone (PFZ), Dangerous River Zone (DRZ), the Fairweather fault, and Transition fault, and the STEEP01 and STEEP02 transects. B. Comparison of STEEP02 velocities with other oceanic plateaus (Christeson et al. 2010). C. Velocity model from the STEEP01 transect and D. Veloctiy model from the STEEP02 transect with the mantle, moho, and Yakutat basement. Vertical exaggeration is 2:1 for both profiles. Contour lines are 1 km/s.</div></td><td class='diff-marker'>+</td><td style="color:black; 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>STEEP01 and STEEP02 refraction profiles (Worthington et al. 2012; Christeson et al. 2010). &#160;</div></td></tr> <tr><td colspan="2">&#160;</td><td class='diff-marker'>+</td><td style="color:black; 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>&#160;</div></td></tr> <tr><td colspan="2">&#160;</td><td class='diff-marker'>+</td><td style="color:black; 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>A. Location map of local tectonics, Kayak Island Zone (KIZ), Pamplona Fault Zone (PFZ), Dangerous River Zone (DRZ), the Fairweather fault, and Transition fault, and the STEEP01 and STEEP02 transects.</div></td></tr> <tr><td colspan="2">&#160;</td><td class='diff-marker'>+</td><td style="color:black; 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>&#160;</div></td></tr> <tr><td colspan="2">&#160;</td><td class='diff-marker'>+</td><td style="color:black; 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>B. Comparison of STEEP02 velocities with other oceanic plateaus (Christeson et al. 2010). C. Velocity model from the STEEP01 transect and D. Veloctiy model from the STEEP02 transect with the mantle, moho, and Yakutat basement. Vertical exaggeration is 2:1 for both profiles. Contour lines are 1 km/s.</div></td></tr> </table>

Nick http://wiki.geodynamics.umaine.edu/index.php?title=Glacial_Loading_and_Tectonics_Figure_1&diff=392&oldid=prev 2015-03-18T15:45:34Z

<p></p> <table class="diff diff-contentalign-left" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr style="vertical-align: top;" lang="en"> <td colspan="2" style="background-color: white; color:black; text-align: center;">← Older revision</td> <td colspan="2" style="background-color: white; color:black; text-align: center;">Revision as of 15:45, 18 March 2015</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1" >Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</td></tr> <tr><td class='diff-marker'>&#160;</td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>[[File:GLTFig1.png|center|500px]]</div></td><td class='diff-marker'>&#160;</td><td style="background-color: #f9f9f9; color: #333333; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #e6e6e6; vertical-align: top; white-space: pre-wrap;"><div>[[File:GLTFig1.png|center|500px]]</div></td></tr> <tr><td colspan="2">&#160;</td><td class='diff-marker'>+</td><td style="color:black; 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;">'''Figure 1.'''</ins></div></td></tr> <tr><td colspan="2">&#160;</td><td class='diff-marker'>+</td><td style="color:black; 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;">STEEP01 and STEEP02 refraction profiles (Worthington et al. 2012; Christeson et al. 2010). A. Location map of local tectonics, Kayak Island Zone (KIZ), Pamplona Fault Zone (PFZ), Dangerous River Zone (DRZ), the Fairweather fault, and Transition fault, and the STEEP01 and STEEP02 transects. B. Comparison of STEEP02 velocities with other oceanic plateaus (Christeson et al. 2010). C. Velocity model from the STEEP01 transect and D. Veloctiy model from the STEEP02 transect with the mantle, moho, and Yakutat basement. Vertical exaggeration is 2:1 for both profiles. Contour lines are 1 km/s.</ins></div></td></tr> </table>

Nick http://wiki.geodynamics.umaine.edu/index.php?title=Glacial_Loading_and_Tectonics_Figure_1&diff=380&oldid=prev 2015-03-18T15:38:36Z

<p>Created page with &quot;<a href="/index.php/File:GLTFig1.png" title="File:GLTFig1.png">center|500px</a>&quot;</p> <p><b>New page</b></p><div>[[File:GLTFig1.png|center|500px]]</div>

Nick