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Michael Taylor
Michael Taylor
Professor - Dept. of Geology, University of Kansas
Bestätigte E-Mail-Adresse bei ku.edu - Startseite
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Zitiert von
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Tectonic evolution of the early Mesozoic blueschist-bearing Qiangtang metamorphic belt, central Tibet
P Kapp, A Yin, CE Manning, TM Harrison, MH Taylor, L Ding
Tectonics 22 (4), 1043, 2003
5202003
Active structures of the Himalayan-Tibetan orogen and their relationships to earthquake distribution, contemporary strain field, and Cenozoic volcanism
M Taylor, A Yin
Geosphere 5 (3), 199-214, 2009
4512009
Conjugate strike-slip faulting along the Bangong-Nujiang suture zone accommodates coeval east-west extension and north-south shortening in the interior of the Tibetan Plateau
M Taylor, A Yin, FJ Ryerson, P Kapp, L Ding
Tectonics 22 (4), 1044, 2003
3152003
Tectonics of sedimentary basins: Recent advances
RV Ingersoll, G Gehrels, JC Gosse, G Dupont-Nivet, W Krijgsman, ...
281*2012
Trapping and migration of methane associated with the gas hydrate stability zone at the Blake Ridge Diapir: new insights from seismic data
MH Taylor, WP Dillon, IA Pecher
Marine Geology 164 (1-2), 79-89, 2000
2092000
Mechanics of V-shaped conjugate strike-slip faults and the corresponding continuum mode of continental deformation
A Yin, MH Taylor
Geological Society of America Bulletin 123 (9-10), 1798-1821, 2011
1512011
Database of active structures from the Indo-Asian collision
R Styron, M Taylor, K Okoronkwo
Eos, Transactions American Geophysical Union 91 (20), 181, 2010
1502010
Development of active low-angle normal fault systems during orogenic collapse: Insight from Tibet
P Kapp, M Taylor, D Stockli, L Ding
Geology 36 (1), 7-10, 2008
1482008
Evidence for faulting related to dissociation of gas hydrate and release of methane off the southeastern United States Peer reviewed article
WP Dillon, WW Danforth, DR Hutchinson, RM Drury, MH Taylor, JS Booth
130*1998
Current slip rates on conjugate strike-slip faults in central Tibet using synthetic aperture radar interferometry
M Taylor, G Peltzer
Journal of Geophysical Research 111 (B12), B12402, 2006
1192006
Oblique convergence, arc-parallel extension, and the role of strike-slip faulting in the High Himalaya
RH Styron, MH Taylor, MA Murphy
Geosphere 7 (2), 582-596, 2011
1152011
Tectonics of Sedimentary Basins: Recent Advances
MH Taylor, PA Kapp, BK Horton
John Wiley and Sons, 2012
103*2012
Limit of strain partitioning in the Himalaya marked by large earthquakes in western Nepal
MA Murphy, MH Taylor, J Gosse, CRP Silver, DM Whipp, C Beaumont
Nature Geoscience 7 (1), 38-42, 2014
932014
Limit of strain partitioning in the Himalaya marked by large earthquakes in western Nepal
MA Murphy, MH Taylor, J Gosse, CRP Silver, DM Whipp, C Beaumont
Nature Geoscience 7 (1), 38-42, 2014
932014
Seafloor collapse and methane venting associated with gas hydrate on the Blake Ridge: Causes and implications to seafloor stability and methanerelease
WP Dillon, JW Nealon, MH Taylor, MW Lee, RM Drury, CH Anton
Geophysical Monograph Series 124, 211-233, 2001
932001
Crustal structure of central Lake Baikal: Insights into intracontinental rifting (DOI 10.1029/2001JB000300)
US Brink, MH Taylor
JOURNAL OF GEOPHYSICAL RESEARCH-ALL SERIES- 107 (7; SECT 2), 2-2, 2002
91*2002
Open source archive of active faults for northwest South America
G Veloza, R Styron, M Taylor, A Mora
GSA Today 22 (10), 2012
892012
Accelerated extension of Tibet linked to the northward underthrusting of Indian crust
R Styron, M Taylor, K Sundell
Nature Geoscience 8 (2), 131-134, 2015
752015
Coseismic slip variation assessed from terrestrial lidar scans of the El Mayor–Cucapah surface rupture
PO Gold, ME Oskin, AJ Elliott, A Hinojosa-Corona, MH Taylor, O Kreylos, ...
Earth and Planetary Science Letters 366, 151-162, 2013
742013
Relationship of Mesozoic graben development, stress, shortening magnitude, and structural style in the Eastern Cordillera of the Colombian Andes
E Tesón, A Mora, A Silva, J Namson, A Teixell, J Castellanos, W Casallas, ...
Geological Society, London, Special Publications 377 (1), 257-283, 2013
722013
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