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  • 1
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    In:  J. Geophys. Res., Kobe, Dec. 6-11, 1993, The Local Organizing Committee for the CRCM '93, vol. 105, no. B3, pp. 5583-5597, pp. TC6001, (ISSN: 1340-4202)
    Publication Date: 2000
    Keywords: Rheology ; Fracture ; Strike-slip ; Modelling ; two ; layer ; JGR ; 8110 ; Tectonophysics ; Continental ; tectonics--general ; (0905) ; 8150 ; Plate ; boundary--general ; (3040) ; 8159 ; Rheology--crust ; and ; lithosphere ; 8164 ; Stresses--crust ; and ; lithosphere
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  • 2
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    In:  J. Geophys. Res., Kobe, Dec. 6-11, 1993, The Local Organizing Committee for the CRCM '93, vol. 105, no. B3, pp. 5599-5613, pp. TC6001, (ISSN: 1340-4202)
    Publication Date: 2000
    Keywords: Rheology ; Fracture ; Strike-slip ; Modelling ; two ; layer ; Dislocation ; JGR ; 8010 ; Structural ; geology ; (new ; field, ; replaces ; single ; entry ; 8165) ; Fractures ; and ; faults ; 8107 ; Tectonophysics ; Continental ; neotectonics ; 8159 ; Rheology--crust ; and ; lithosphere ; 8164 ; Stresses--crust ; and ; lithosphere
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  • 3
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    In:  J. Geophys. Res., Luxembourg, Inst. Electrical & Electronics Engineers, vol. 106, no. B4, pp. 6793-6816, pp. B06303, (ISSN: 1340-4202)
    Publication Date: 2001
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; China ; Geodesy ; Himalya ; Sichuan ; XSH ; Rheology ; Two-dimensional ; non-Newtonian ; viscous ; Stokes ; Stress ; 3210 ; Mathematical ; geophysics ; (New ; field) ; Modeling ; JGR
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  • 4
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    Am. Ass. Petroleum Geologists, Memoir 45
    In:  Bull., Open-File Rept., The Pannonian Basin - A Study in Basin Evolution, London, Am. Ass. Petroleum Geologists, Memoir 45, vol. 3, no. 16, pp. 27-48, (ISBN 0080419208)
    Publication Date: 1988
    Keywords: EUROPROBE (Geol. and Geophys. in eastern Europe) ; Tectonics
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  • 5
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 1996-08-02
    Description: Crustal temperatures within collisional orogens are anomalously high compared with temperatures at comparable depths in stable continents, which is evidence of thermal processes that are fundamental to orogenesis. These temperatures can be explained by the redistribution of crust enriched in heat-producing elements through the accretion of crust from the down-going plate to the upper plate and surface erosion. With the use of geologically reasonable rates, the model results predict high temperatures (over 600°C) and inverted upper-plate geotherms (about 100°C over 20 kilometers) at shallow depths (20 to 40 kilometers) by 25 to 35 million years after collision. This study emphasizes the interdependence of deformational, surficial, and thermal processes.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Huerta -- Royden -- Hodges -- New York, N.Y. -- Science. 1996 Aug 2;273(5275):637-9.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/8662552" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 1997-05-02
    Description: Field observations and satellite geodesy indicate that little crustal shortening has occurred along the central to southern margin of the eastern Tibetan plateau since about 4 million years ago. Instead, central eastern Tibet has been nearly stationary relative to southeastern China, southeastern Tibet has rotated clockwise without major crustal shortening, and the crust along portions of the eastern plateau margin has been extended. Modeling suggests that these phenomena are the result of continental convergence where the lower crust is so weak that upper crustal deformation is decoupled from the motion of the underlying mantle. This model also predicts east-west extension on the high plateau without convective removal of Tibetan lithosphere and without eastward movement of the crust east of the plateau.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Royden -- Burchfiel -- King -- Wang -- Chen -- Shen -- Liu -- New York, N.Y. -- Science. 1997 May 2;276(5313):788-90.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉L. H. Royden, B. C. Burchfiel, R. W. King, E. Wang, Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA. Z. Chen, F. Shen, Y. Liu, Chengdu Institute of Geology and Mineral Resources, Chengdu, China.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/9115202" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 2008-08-23
    Description: The geological evolution of the Tibetan plateau is best viewed in a context broader than the India-Eurasia collision zone. After collision about 50 million years ago, crust was shortened in western and central Tibet, while large fragments of lithosphere moved from the collision zone toward areas of trench rollback in the western Pacific and Indonesia. Cessation of rapid Pacific trench migration ( approximately 15 to 20 million years ago) coincided with a slowing of fragment extrusion beyond the plateau and probably contributed to the onset of rapid surface uplift and crustal thickening in eastern Tibet. The latter appear to result from rapid eastward flow of the deep crust, probably within crustal channels imaged seismically beneath eastern Tibet. These events mark a transition to the modern structural system that currently accommodates deformation within Tibet.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Royden, Leigh H -- Burchfiel, B Clark -- van der Hilst, Robert D -- New York, N.Y. -- Science. 2008 Aug 22;321(5892):1054-8. doi: 10.1126/science.1155371.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 01890, USA. lhroyden@mit.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18719275" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
    Publication Date: 2012-07-21
    Description: The western Hellenic subduction zone (WHSZ) exhibits well-documented along-strike variations in lithosphere density (i.e., oceanic versus continental), subduction rates, and overriding plate extension. Differences in slab density are believed to drive deformation rates along the WHSZ; however, this hypothesis has been difficult to test given the limited seismic constraints on the structure of the WHSZ, particularly beneath northern Greece. Here, we present high-resolution seismic images across northern and southern Greece to constrain the slab composition and mantle wedge geometry along the WHSZ. Data from two temporary arrays deployed across Greece in a northern line (NL) and southern line (SL) are processed using a 2D teleseismic migration algorithm based on the Generalized Radon Transform. Images of P- and S-wave velocity perturbations reveal N60E dipping low-velocity layers beneath both NL and SL. The ∼8 km thick layer beneath SL is interpreted as subducted oceanic crust while the ∼20 km thick layer beneath NL is interpreted as subducted continental crust. The thickness of subducted continental crust inferred within the upper mantle suggests that ∼10 km of continental crust has accreted to the overriding plate. The relative position of the two subducted crusts implies ∼70–85 km of additional slab retreat in the south relative to the north. Overall, our seismic images are consistent with the hypothesis that faster sinking of the denser, oceanic portion of the slab relative to the continental portion can explain the different rates of slab retreat and deformation in the overriding plate along the WHSZ.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Publication Date: 1990-12-14
    Description: The Kangmar metamorphic-igneous complex is one of the most accessible examples of an enigmatic group of gneiss domes (the North Himalayan belt) that lies midway between the Greater Himalaya and the Indus-Tsangpo suture in southern Tibet. Structural analysis suggests that the domal structure formed as a consequence of extensional deformation, much like the Tertiary metamorphic core complexes in the North American Cordillera. Unlike its North American counterparts, the Kangmar dome developed in an entirely convergent tectonic setting. The documentation of metamorphic core complexes in the Himalayan orogen supports the emerging concept that extensional processes may play an important role in the evolution of compressional mountain belts.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Chen, Z -- Liu, Y -- Hodges, K V -- Burchfiel, B C -- Royden, L H -- Deng, C -- New York, N.Y. -- Science. 1990 Dec 14;250(4987):1552-6.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17818283" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 10
    Publication Date: 1992-11-27
    Description: The South Tibetan detachment system separates the high-grade metamorphic core of the Himalayan orogen from its weakly metamorphosed suprastructure. It is thought to have developed in response to differences in gravitational potential energy produced by crustal thickening across the mountain front. Geochronologic data from the Rongbuk Valley, north of Qomolangma (Mount Everest) in southern Tibet, demonstrate that at least one segment of the detachment system was active between 19 and 22 million years ago, an interval characterized by large-scale crustal thickening at lower structural levels. These data suggest that decoupling between an extending upper crust and a converging lower crust was an important aspect of Himalayan tectonics in Miocene time.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hodges, K V -- Parrish, R R -- Housh, T B -- Lux, D R -- Burchfiel, B C -- Royden, L H -- Chen, Z -- New York, N.Y. -- Science. 1992 Nov 27;258(5087):1466-70.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17755108" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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