51
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Clift PD, Sun Z. The sedimentary and tectonic evolution of the Yinggehai-Song Hong basin and the southern Hainan margin, South China Sea: Implications for Tibetan uplift and monsoon intensification. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2005jb004048] [Citation(s) in RCA: 167] [Impact Index Per Article: 9.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Peter D. Clift
- School of Geosciences; University of Aberdeen; Aberdeen UK
| | - Zhen Sun
- Key Laboratory of Marginal Sea Geology; South China Sea Institute of Oceanology, Chinese Academy of Sciences; Guangzhou China
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52
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Braitenberg C, Wienecke S, Wang Y. Basement structures from satellite-derived gravity field: South China Sea ridge. ACTA ACUST UNITED AC 2006. [DOI: 10.1029/2005jb003938] [Citation(s) in RCA: 124] [Impact Index Per Article: 6.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
Affiliation(s)
| | - Susann Wienecke
- Department of Earth Sciences; Trieste University; Trieste Italy
| | - Yong Wang
- Institute of Geodesy and Geophysics; Chinese Academy of Sciences; Wuhan China
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53
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Shen ZK, Lü J, Wang M, Bürgmann R. Contemporary crustal deformation around the southeast borderland of the Tibetan Plateau. ACTA ACUST UNITED AC 2005. [DOI: 10.1029/2004jb003421] [Citation(s) in RCA: 435] [Impact Index Per Article: 22.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Zheng-Kang Shen
- State Key Laboratory of Earthquake Dynamics, Institute of Geology; China Earthquake Administration; Beijing China
| | - Jiangning Lü
- Department of Geophysics; Peking University; Beijing China
| | - Min Wang
- Institute of Earthquake Science; China Earthquake Administration; Beijing China
| | - Roland Bürgmann
- Department of Earth and Planetary Science; University of California; Berkeley California USA
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54
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Cheng WB. Crustal Structure of the High Magnetic Anomaly Belt, Western Taiwan, and its Implications for Continental Margin Deformation. MARINE GEOPHYSICAL RESEARCHES 2004; 25:79-93. [DOI: 10.1007/s11001-005-0735-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 09/01/2023]
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55
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Barckhausen U, Roeser HA. Seafloor spreading anomalies in the South China Sea revisited. CONTINENT-OCEAN INTERACTIONS WITHIN EAST ASIAN MARGINAL SEAS 2004. [DOI: 10.1029/149gm07] [Citation(s) in RCA: 87] [Impact Index Per Article: 4.4] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/25/2022]
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56
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Hall R, Morley CK. Sundaland basins. CONTINENT-OCEAN INTERACTIONS WITHIN EAST ASIAN MARGINAL SEAS 2004. [DOI: 10.1029/149gm04] [Citation(s) in RCA: 83] [Impact Index Per Article: 4.2] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/03/2022]
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57
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Kuhnt W, Holbourn A, Hall R, Zuvela M, Käse R. Neogene history of the Indonesian Throughflow. CONTINENT-OCEAN INTERACTIONS WITHIN EAST ASIAN MARGINAL SEAS 2004. [DOI: 10.1029/149gm16] [Citation(s) in RCA: 75] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/02/2022]
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58
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Aitchison JC, Davis AM. Evidence for the multiphase nature of the India-Asia collision from the Yarlung Tsangpo suture zone, Tibet. ACTA ACUST UNITED AC 2004. [DOI: 10.1144/gsl.sp.2004.226.01.12] [Citation(s) in RCA: 30] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/04/2022]
Abstract
AbstractRecent investigations in southern Tibet enable the testing and refinement of existing models for India-Asia collision. Presently available data indicate that marine deposition continued in the southern central portion of Tibet until at least the end of the Eocene. Sub-duction-related magmatism continued until the Mid-Oligocene, after which rapid uplift of the plateau was initiated. Mass-wasting of sediments into molasse basins did not commence until the latest Oligocene. The implications are that existing models, based on less-precise age constraints, invoking India-Asia collision at 55 Ma, are either flawed, or collision began at a different time. Recent work has produced sufficient data to allow the recognition of two different collisional events along the suture between India and Asia. Features related to each event require separate interpretation, and no collisional continuum should be assumed. In southern Tibet, a collision between the northern margin of India and a southfacing intra-oceanic island arc occurred at around 55 Ma, whereas continent-continent collision between India and Asia did not occur until at least 20 million years later.
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Affiliation(s)
- Jonathan C. Aitchison
- Tibet Research Group, Department of Earth Sciences, University of Hong Kong
Pokfulam Road, Hong Kong SAR, China
| | - Aileen M. Davis
- Tibet Research Group, Department of Earth Sciences, University of Hong Kong
Pokfulam Road, Hong Kong SAR, China
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59
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Problem of positioning Paleogene Eurasia: A review. Efforts to resolve the issue. Implications for the India-Asia collision. ACTA ACUST UNITED AC 2004. [DOI: 10.1029/149gm02] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register]
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60
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Wang P. Cenozoic deformation and the history of sea-land interactions in Asia. CONTINENT-OCEAN INTERACTIONS WITHIN EAST ASIAN MARGINAL SEAS 2004. [DOI: 10.1029/149gm01] [Citation(s) in RCA: 35] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/05/2022]
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61
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Wang J, Yin A, Harrison MT, Grove M, Zhou J, Zhang Y, Xie G. Thermochronological constraints on two pulses of Cenozoic high-K magmatism in eastern Tibet. ACTA ACUST UNITED AC 2003. [DOI: 10.1360/03yd9063] [Citation(s) in RCA: 16] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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62
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Replumaz A, Tapponnier P. Reconstruction of the deformed collision zone Between India and Asia by backward motion of lithospheric blocks. ACTA ACUST UNITED AC 2003. [DOI: 10.1029/2001jb000661] [Citation(s) in RCA: 344] [Impact Index Per Article: 16.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- A. Replumaz
- Laboratoire Dynamique de la Lithosphère; Université Claude Bernard-Lyon 1; Villeurbanne France
| | - P. Tapponnier
- Laboratoire de Tectonique, Mécanique de la Lithosphère; Institut de Physique du Globe de Paris; Paris France
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63
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Gilley LD, Harrison TM, Leloup PH, Ryerson FJ, Lovera OM, Wang JH. Direct dating of left-lateral deformation along the Red River shear zone, China and Vietnam. ACTA ACUST UNITED AC 2003. [DOI: 10.1029/2001jb001726] [Citation(s) in RCA: 236] [Impact Index Per Article: 11.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
Affiliation(s)
- Lisa D. Gilley
- Department of Earth and Space Sciences and Institute for Geophysics and Planetary Physics; University of California; Los Angeles California USA
| | - T. Mark Harrison
- Department of Earth and Space Sciences and Institute for Geophysics and Planetary Physics; University of California; Los Angeles California USA
| | - P. H. Leloup
- Centre National de la Recherche Scientifique; Institut de Physique du Globe de Paris; Paris France
| | - F. J. Ryerson
- Institute of Geophysics and Planetary Physics; Lawrence Livermore National. Laboratory; Livermore California USA
| | - Oscar M. Lovera
- Department of Earth and Space Sciences and Institute for Geophysics and Planetary Physics; University of California; Los Angeles California USA
| | - Jiang-Hai Wang
- Guangzhou Institute of Geochemistry; Chinese Academy of Sciences; Guangzhou China
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64
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Lebedev S, Nolet G. Upper mantle beneath Southeast Asia fromSvelocity tomography. ACTA ACUST UNITED AC 2003. [DOI: 10.1029/2000jb000073] [Citation(s) in RCA: 217] [Impact Index Per Article: 10.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- Sergei Lebedev
- Department of Geosciences; Princeton University; Princeton New Jersey USA
| | - Guust Nolet
- Department of Geosciences; Princeton University; Princeton New Jersey USA
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65
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Lin AT, Watts AB. Origin of the West Taiwan basin by orogenic loading and flexure of a rifted continental margin. ACTA ACUST UNITED AC 2002. [DOI: 10.1029/2001jb000669] [Citation(s) in RCA: 152] [Impact Index Per Article: 6.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
Affiliation(s)
- A. T. Lin
- Department of Earth Sciences; University of Oxford; Oxford UK
| | - A. B. Watts
- Department of Earth Sciences; University of Oxford; Oxford UK
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66
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Abstract
The South China Sea is poorly understood in terms of its marine biota, ecology and the human impacts upon it. What is known is most often contained in reports and workshop and conference documents that are not available to the wider scientific community. The South China Sea has an area of some 3.3 million km2 and depths range from the shallowest coastal fringe to 5377 m in the Manila Trench. It is also studded with numerous islets, atolls and reefs many of which are just awash at low tide. It is largely confined within the Tropic of Cancer and, therefore, experiences a monsoonal climate being influenced by the Southwest Monsoon in summer and the Northeast Monsoon in winter. The South China Sea is a marginal sea and, therefore, largely surrounded by land. Countries that have a major influence on and claims to the sea include China, Malaysia, the Philippines and Vietnam, although Thailand, Indonesia and Taiwan have some too. The coastal fringes of the South China Sea are home to about 270 million people that have had some of the fastest developing and most vibrant economies on the globe. Consequently, anthropogenic impacts, such as over-exploitation of resources and pollution, are anticipated to be huge although, in reality, relatively little is known about them. The Indo-West Pacific biogeographic province, at the centre of which the South China Sea lies, is probably the world's most diverse shallow-water marine area. Of three major nearshore habitat types, i.e., coral reefs, mangroves and seagrasses, 45 mangrove species out of a global total of 51, most of the currently recognised 70 coral genera and 20 of 50 known seagrass species have been recorded from the South China Sea. The island groups of the South China Sea are all disputed and sovereignty is claimed over them by a number of countries. Conflicts have in recent decades arisen over them because of perceived national rights. It is perhaps because of this that so little research has been undertaken on the South China Sea. What data are available, however, and if Hong Kong is used, as it is herein, as an indicator of what the perturbations of other regional cities upon the South China Sea are like, then it is impacted grossly and an ecological disaster has probably already, but unknowingly, happened.
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Affiliation(s)
- B Morton
- The Swire Institute of Marine Science and Department of Ecology and Biodiversity, The University of Hong Kong, Cape d' Aguliar, Shek O, China.
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67
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Tapponnier P, Zhiqin X, Roger F, Meyer B, Arnaud N, Wittlinger G, Jingsui Y. Oblique stepwise rise and growth of the Tibet plateau. Science 2001; 294:1671-7. [PMID: 11721044 DOI: 10.1126/science.105978] [Citation(s) in RCA: 256] [Impact Index Per Article: 11.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Two end member models of how the high elevations in Tibet formed are (i) continuous thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) time-dependent, localized shear between coherent lithospheric blocks. Recent studies of Cenozoic deformation, magmatism, and seismic structure lend support to the latter. Since India collided with Asia approximately 55 million years ago, the rise of the high Tibetan plateau likely occurred in three main steps, by successive growth and uplift of 300- to 500-kilometer-wide crustal thrust-wedges. The crust thickened, while the mantle, decoupled beneath gently dipping shear zones, did not. Sediment infilling, bathtub-like, of dammed intermontane basins formed flat high plains at each step. The existence of magmatic belts younging northward implies that slabs of Asian mantle subducted one after another under ranges north of the Himalayas. Subduction was oblique and accompanied by extrusion along the left lateral strike-slip faults that slice Tibet's east side. These mechanisms, akin to plate tectonics hidden by thickening crust, with slip-partitioning, account for the dominant growth of the Tibet Plateau toward the east and northeast.
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Affiliation(s)
- P Tapponnier
- Institut de Physique du Globe, 4 Place Jussieu, 75252 Paris, France.
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68
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High resolution bathymetry of China seas and their surroundings. CHINESE SCIENCE BULLETIN-CHINESE 2001. [DOI: 10.1007/bf02900631] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/22/2022]
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69
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Leloup PH, Arnaud N, Lacassin R, Kienast JR, Harrison TM, Trong TTP, Replumaz A, Tapponnier P. New constraints on the structure, thermochronology, and timing of the Ailao Shan-Red River shear zone, SE Asia. ACTA ACUST UNITED AC 2001. [DOI: 10.1029/2000jb900322] [Citation(s) in RCA: 492] [Impact Index Per Article: 21.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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70
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Replumaz A, Lacassin R, Tapponnier P, Leloup PH. Large river offsets and Plio-Quaternary dextral slip rate on the Red River fault (Yunnan, China). ACTA ACUST UNITED AC 2001. [DOI: 10.1029/2000jb900135] [Citation(s) in RCA: 173] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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71
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Clift PD, Lin J. Patterns of extension and magmatism along the continent-ocean boundary, South China margin. ACTA ACUST UNITED AC 2001. [DOI: 10.1144/gsl.sp.2001.187.01.24] [Citation(s) in RCA: 65] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/04/2022]
Abstract
AbstractEarly Oligocene sea-floor spreading in the South China Sea was preceded by at least two episodes (in Maastrichtian and Mid-Eocene time) of continental extension that generated a series of rift basins on the South China margin, which are separated from the continent-ocean boundary (COB) by an outer structural high. Regional multichannel seismic profiles showing faulting of the pre-rift basement allow the amount of extension in the upper crust to be measured. The total subsidence across the South China margin is far in excess of that predicted using a forward flexural-cantilever model of extension and the degree of faulting measured seismically in the upper crust. This mismatch suggests preferential extension of the lower crust, increasing towards the COB to account for the subsidence. The same feature is seen in the Nam Con Som Basin, which is located close to the southwest end of an extinct propagating spreading ridge offshore from Vietnam. However, in the Beibu Gulf Basin, which is not adjacent to the COB, subsidence is approximately compatible with uniform extension in the upper and lower crust across the entire basin, if not at all locations. We predict that extension of the lower crust exceeds that in the lithospheric mantle along the COB. Heat-flow measurements at Ocean Drilling Program (ODP) sites on the Chinese continental slope and on the conjugate Dangerous Grounds margin yield values consistent with, or slightly higher than, those predicted by models of uniform extension in the lithosphere. Although there is no magmatism comparable with the seaward-dipping volcanic rocks of rifted volcanic margins, there is seismic evidence of rift-related volcanic rocks spanning a width ofc.25 km landward of the COB. Simple adiabatic melting models do not predict magmatism, and we suggest that the presence of water in the mantle lithosphere, together with residual pre-rift heat, may instead be responsible for increasing melting here. Deep-water syn-rift sediments recovered by the ODP near the COB indicate that volcanism was submarine and that rifting culminated in a mass wasting event that marks a break-up unconformity. The average extension in South China Sea is much less than that seen in the extreme ‘non-volcanic’ Iberian margin. The South China margin may represent an intermediary form of continental extension between the end member extremes of the Iberia-type non-volcanic and the Greenland-type volcanic margin.
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Affiliation(s)
- Peter D. Clift
- Department of Geology and Geophysics, Woods Hole Oceanographic Institution Woods Hole, MA 02543, USA
| | - Jian Lin
- Department of Geology and Geophysics, Woods Hole Oceanographic Institution Woods Hole, MA 02543, USA
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72
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Gilder SA, Leloup PH, Courtillot V, Chen Y, Coe RS, Zhao X, Xiao W, Halim N, Cogné JP, Zhu R. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via Middle Triassic to Early Cenozoic paleomagnetic data. ACTA ACUST UNITED AC 1999. [DOI: 10.1029/1999jb900123] [Citation(s) in RCA: 224] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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73
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Fluteau F, Ramstein G, Besse J. Simulating the evolution of the Asian and African monsoons during the past 30 Myr using an atmospheric general circulation model. ACTA ACUST UNITED AC 1999. [DOI: 10.1029/1999jd900048] [Citation(s) in RCA: 141] [Impact Index Per Article: 5.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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74
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Li S, Lin C, Zhang Q, Yang S, Wu P. Episodic rifting of continental marginal basins and tectonic events since 10 Ma in the South China Sea. CHINESE SCIENCE BULLETIN-CHINESE 1999. [DOI: 10.1007/bf03182877] [Citation(s) in RCA: 26] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/19/2022]
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75
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Wittlinger G, Tapponnier P, Poupinet G, Mei J, Danian S, Herquel G, Masson F. Tomographic evidence for localized lithospheric shear along the altyn tagh fault. Science 1998; 282:74-6. [PMID: 9756478 DOI: 10.1126/science.282.5386.74] [Citation(s) in RCA: 186] [Impact Index Per Article: 7.2] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/02/2022]
Abstract
Seismic tomography across the Altyn Tagh fault, at the north edge of the Tibetan Plateau, reveals a low P-wave velocity anomaly below the fault down to 140 kilometers. This anomaly probably reflects strike-slip shear in the lithosphere. Slip-partitioning may also induce a wedge of crust from the Tarim Basin to plunge into the mantle.
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Affiliation(s)
- G Wittlinger
- G. Wittlinger, G. Herquel, F. Masson, Institut de Physique du Globe de Strasbourg, Centre National de la Recherche Scientifique, Universite Louis Pasteur, 5 rue R. Descartes 67084 Strasbourg, France. P. Tapponnier, Laboratoire de Tectoniq
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76
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Manighetti I, Tapponnier P, Gillot PY, Jacques E, Courtillot V, Armijo R, Ruegg JC, King G. Propagation of rifting along the Arabia-Somalia Plate Boundary: Into Afar. ACTA ACUST UNITED AC 1998. [DOI: 10.1029/97jb02758] [Citation(s) in RCA: 154] [Impact Index Per Article: 5.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/10/2022]
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77
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Flower M, Tamaki K, Hoang N. Mantle extrusion: A model for dispersed volcanism and DUPAL-like asthenosphere in East Asia and the western Pacific. MANTLE DYNAMICS AND PLATE INTERACTIONS IN EAST ASIA 1998. [DOI: 10.1029/gd027p0067] [Citation(s) in RCA: 87] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/03/2022]
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78
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Lee TY, Lo CH, Chung SL, Chen CY, Wang PL, Lin WP, Hoang N, Chi CT, Yem NT. 40Ar/39Ar dating result of Neogene basalts in Vietnam and its tectonic implication. MANTLE DYNAMICS AND PLATE INTERACTIONS IN EAST ASIA 1998. [DOI: 10.1029/gd027p0317] [Citation(s) in RCA: 27] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 01/03/2023]
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79
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Lacassin R, Maluski H, Leloup PH, Tapponnier P, Hinthong C, Siribhakdi K, Chuaviroj S, Charoenravat A. Tertiary diachronic extrusion and deformation of western Indochina: Structural and40Ar/39Ar evidence from NW Thailand. ACTA ACUST UNITED AC 1997. [DOI: 10.1029/96jb03831] [Citation(s) in RCA: 189] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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80
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Effect of orogeny, plate motion and land–sea distribution on Eurasian climate change over the past 30 million years. Nature 1997. [DOI: 10.1038/386788a0] [Citation(s) in RCA: 463] [Impact Index Per Article: 17.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/08/2022]
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81
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Manighetti I, Tapponnier P, Courtillot V, Gruszow S, Gillot PY. Propagation of rifting along the Arabia-Somalia Plate Boundary: The Gulfs of Aden and Tadjoura. ACTA ACUST UNITED AC 1997. [DOI: 10.1029/96jb01185] [Citation(s) in RCA: 157] [Impact Index Per Article: 5.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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82
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Roques D, Matthews SJ, Rangin C. Constraints on strike-slip motion from seismic and gravity data along the Vietnam margin offshore Da Nang: implications for hydrocarbon prospectivity and opening of the East Vietnam Sea. ACTA ACUST UNITED AC 1997. [DOI: 10.1144/gsl.sp.1997.126.01.20] [Citation(s) in RCA: 13] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/04/2022]
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83
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Mat-Zin IC, Swarbrick RE. The tectonic evolution and associated sedimentation history of Sarawak Basin, eastern Malaysia: a guide for future hydrocarbon exploration. ACTA ACUST UNITED AC 1997. [DOI: 10.1144/gsl.sp.1997.126.01.15] [Citation(s) in RCA: 25] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/04/2022]
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84
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85
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Peltzer G, Saucier F. Present-day kinematics of Asia derived from geologic fault rates. ACTA ACUST UNITED AC 1996. [DOI: 10.1029/96jb02698] [Citation(s) in RCA: 229] [Impact Index Per Article: 8.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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86
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Gilder SA, Gill J, Coe RS, Zhao X, Liu Z, Wang G, Yuan K, Liu W, Kuang G, Wu H. Isotopic and paleomagnetic constraints on the Mesozoic tectonic evolution of south China. ACTA ACUST UNITED AC 1996. [DOI: 10.1029/96jb00662] [Citation(s) in RCA: 395] [Impact Index Per Article: 14.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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87
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88
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89
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90
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Ducrocq S, Chaimanee Y, Suteethorn V, Jaeger JJ. Mammalian faunas and the ages of the continental Tertiary fossiliferous localities from Thailand. ACTA ACUST UNITED AC 1995. [DOI: 10.1016/0743-9547(95)00021-6] [Citation(s) in RCA: 51] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/25/2022]
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