Kidd, William S. F. - Department of Earth and Atmospheric Sciences, State University of New York at Albany

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Kidd, William S. F. - Department of Earth and Atmospheric Sciences, State University of New York at Albany

RosenbergThrust HighgateAnticline
Reprinted From Island Arcs, Deep Sea Trenches and Back-Arc Basins, Maurice
BIN ZHU1, B. CURRIE2, W.S.F. KIDD1, D.B. ROWLEY3, B. ZHANG4 1Earth & Atmospheric Sciences, Univ. at Albany, Albany, NY 12222 USA
Figure 4.1 Undeformed diabase dike cutting mylonitized gabbro of Shear Zone VII.
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 99, NO. B9, PAGES 18,175-18,201, SEPTEMBER 10, 1994 Tertiary structural evolution of the Gangdese thrust
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Landsat 7 Thematic Mapper image mosaic covering the same area as the geological map. TM Bands 5,4,2:R,G,B. Images from October, November 2001.
The Mings Bight Ophiolite Complex, Newfoundland: Appalachian oceanic crust W. S. F.KIDD AND JOHN F. DEWEY
The Karo-la Decollement, southern Tibet a Himalayan extensional structure domed by emplacement of the Late Miocene Karo-La Granite
arising from the Nanga Parbat Continental Dynamics Project Tectonic and geochronologic observations in Central and Southern Nanga Parbat-Haramosh Massif
Geologic Hazards Associated With a Proposed Dam on the Yarlung-
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ELSEVIER Earth and Planetary Science Letters 167 (1999) 121129 Early Miocene anatexis identified in the western syntaxis,
EXTENSION AND EXHUMATION OF THE HP/LT ROCKS IN THE HELLENIC FOREARC RIDGE
Cite abstracts as: Eos. Trans. AGU, 83(47), Fall Meet. Suppl., Abstract #####-##, 2002. 2002 Fall Meeting
TECTONICS, VOL. 17, NO. 1, PAGES 46-61, FEBRUARY 1998 Shallow structure of the Yadong-Gulu rift, southern Tibet, from
[The Journal of Geology, 2005, volume 113, p. 419438] 2005 by The University of Chicago. All rights reserved. 0022-1376/2005/11304-0003$15.00 Late Shortening and Extensional Structures and Veins in the Western
D.B. Rowley, W.S.F. Kidd, and L.L. Delano, 1979. Detailed stratigraphic and structural features of the Giddings Brook slice of the
It is widely believed that the Tibetan plateau is a late Cenozoic fea-ture produced by the Indo-Asian collision. However, because Tibet was
Magmatic compositions and source terranes estimated from melt inclusions in detrital Cr-rich spinels: An example from
Christoforianika KatsoulianikaKousounari
The eastern Himalayan syntaxis is host to the actively deforming metamorphic massif,
T. M. Kusky Center for Remote Sensing, Boston University, Boston,
New Map of Southern Nanga Parbat M.A. Edwards1
Shortening in the southern Lhasa block during India-Asia collisionY. Pan and W.S.F. Kidd Dept of Earth and Atmospheric Sciences, University at Albany, Albany NY 12222, USA.
Timing and amount of crustal shortening, Shuanghe area, Central Tibet W.S.F. KIDD1, M.A. EDWARDS2, Y. LI1, K.D. NELSON3, L. RATSCHBACHER2, Z. WU4
Introduction Melt inclusions (figure 1) found in mineral grains as tiny droplets trapped during crystal growth offer a
Bin Zhu, William S.F. Kidd, Earth & Atmospheric Sciences, University at Albany, Albany, NY 12222 David B. Rowley, Geophysical Sciences, Univ. of Chicago, Chicago, IL 60637
http://gsa.confex.com/gsa/2005NE/finalprogram/abstract_82963.htm Northeastern Section -40th Annual Meeting (March 1416, 2005)
http://gsa.confex.com/gsa/2006AM/finalprogram/abstract_106744.htm 2006 Philadelphia Annual Meeting (2225 October 2006)
http://gsa.confex.com/gsa/2006AM/finalprogram/abstract_113030.htm 2006 Philadelphia Annual Meeting (2225 October 2006)
29 Figure 2.1 A view of the Kirklar Formation, looking southwest toward the Gelintas
1-6 Figure 1.3. View of the field area, looking south-southwest. Left side of the picture shows the
The Department 2 The University 3
January, 2008 Curriculum Vitae
http://gsa.confex.com/gsa/2005AM/finalprogram/abstract_96987.htm 2005 Salt Lake City Annual Meeting (October 1619, 2005)
File DR1. Garnet dissolution calculations following Kohn and Spear (2000) Measurements and calculations for sample GP-5
[The Journal of Geology, 2004, volume 112, p. 417434] 2004 by The University of Chicago. All rights reserved. 0022-1376/2004/11204-0003$15.00 Chemical Compositions and Tectonic Significance of Chrome-Rich
2006 Fall Meeting Cite abstracts as Author(s) (2006), Title, Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract xxxxx-xx
http://gsa.confex.com/gsa/2007AM/finalprogram/abstract_131843.htm 2007 GSA Denver Annual Meeting (2831 October 2007)
Cite abstracts as: Eos. Trans. AGU, 83(47), Fall Meet. Suppl., Abstract #####-##, 2002. 2002 Fall Meeting
25 Figure 3.1 Mafic schist belonging to the Northern Group on west shore of Brents Cove.
2006 Fall Meeting Cite abstracts as Author(s) (2006), Title, Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract xxxxx-xx
2005 Geological Society of America. For permission to copy, contact Copyright Permissions, GSA, or editing@geosociety.org. Geology; December 2005; v. 33; no. 12; p. 961964; doi: 10.1130/G21832.1; 4 figures. 961
2002 Fall Meeting Cite abstracts as: Eos. Trans. AGU, 83(47), Fall Meet. Suppl., Abstract #####-##, 2002.
4 JANUARY 2001, GSA TODAY Peter K. Zeitler, Anne S. Meltzer, Department
INTRODUCTION The western Himalaya syntaxis includes the
2005 Fall Meeting Cite abstracts as Author(s) (2005), Title, Eos Trans. AGU, 86(52), Fall Meet. Suppl., Abstract xxxxx-xx
Can. J. Earth Sci. 40: 17731787 (2003) doi: 10.1139/E03-076 2003 NRC Canada Tectonic setting of outer trench slope volcanism
2002 Fall Meeting Cite abstracts as: Eos. Trans. AGU, 83(47), Fall Meet. Suppl., Abstract #####-##, 2002.
New York State Geological Association 67th Annual meeting & Eastern Section of the American Association of Petroleum Geologists 26th Annual meeting, Union College, Schenectady, NY, October 13-15, 1995
The Main Mantle Thrust (MMT) is the regional contact between collider India and the overthrust Kohistan-Ladakh series in the Pakistan Himalaya. Early Himalayan-age
MAPPING OF THE DETACHMENT FAULT IN KYTHERA ISLAND AND STUDY OF THE RELATED
===================ZetaAge Program v. 4.8 (Brandon 8/13/02)=================== FILENAME: D:\FTZ\U38Y\TEMP\QZ12.FTZ
Hudson-Champlain-Mohawk Valley-Taconic Allochthon manuscript compilation map for GSA Continent-Ocean Transect E1 by W.S.F. Kidd, submitted Sept 1982 1:250,000 scale (cross-section vertical = horizontal scale)
Quartzite filling paleo-valley Quartzite absent in continuous outcrop
Fluid evolution and thermal structure in the rapidly exhuming gneiss complex of Namche BarwaGyala Peri, eastern Himalayan
0 1 2 3 4 5 river profile
29 Figure 5: Type 2 melange containing a block of quartzite.
http://gsa.confex.com/gsa/2009NE/finalprogram/abstract_155494.htm Northeastern Section -44th Annual Meeting (2224 March 2009)
1 "The beauty of the scene presented by the land upon all sides is very impressing; yet at
22 Figure 2-2: Small fold adjacent to fault zone, Bonanza Creek.
2009 Joint Assembly Cite abstracts as Author(s) (2009), Title, Eos Trans. AGU, 90(22), Jt. Assem. Suppl., Abstract xxxxx-xx
19 Figure 3.1 Outcrop of folded Pawlet Formation located on Route 22 north of junction
ELSEVIER Tectonophysics260 (1996) 1-19 TECTONOPHYSICS
Figure 4. Browns Pond Formation at Schodack Landing Figure 5. Breccia within the Middle Granville Slate
http://gsa.confex.com/gsa/2008NE/finalprogram/abstract_135420.htm Northeastern Section -43rd Annual Meeting (27-29 March 2008)
EVIDENCE AGAINST THE ALLOCHTHONOUS NATURE OF THE STANBRIDGE NAPPE AT HIGHGATE GORGE, NORTHWESTERN VERMONT
AKIHO MIYASHIRO Miyashiro, Akiho ALBANY Akiho Miyashiro died unexpectedly Thursday, July 24,
27 Poorly cleaved, massive, light-weathering Bomoseen graywacke outcrop located on
2006 Fall Meeting Cite abstracts as Author(s) (2006), Title, Eos Trans. AGU, 87(52), Fall Meet. Suppl., Abstract xxxxx-xx
2007 Fall Meeting Cite abstracts as Author(s) (2007), Title, Eos Trans. AGU, 88(52), Fall Meet. Suppl., Abstract xxxxx-xx
TECTONICS, VOL. 17, NO. 1, PAGES 28-45, FEBRUARY 1998 Yadong cross structure and South Tibetan Detachment
15 Figure 2-3. Member A of the Luscombe Formation
Thermo Fisher Student Venture Fund $50K and Business Development Aid for a Commercially Viable Science Technology Applicable to
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73.00''73.15'' 72.45' 0 kilometer 10
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Local Geology Lithostructural Units Folded and Faulted Flysch 25 Figure 6 Three yellow-brown unlithified bentonite beds (top, center, bottom) in gently
Structural Map of the Phyllite-Quartzite Unit
The northern and eastern faces of Table Mountain as viewed from the South Arm of 30
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1000 2000 3000 4000 .5 0 1 KILOMETER
30 Figure 3.1: Arkosic sandstone from the Potsdam Formation. Kline Hill [21], 5 km west
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