(Q60962863)

English

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

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scholarly article

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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 (English)

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author name string

Michael Taylor

1

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An Yin

2

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Frederick J. Ryerson

3

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Paul Kapp

4

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Lin Ding

5

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publication date

August 2003

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22

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4

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Normal faulting in central Tibet since at least 13.5 Myr ago

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Field evidence for active normal faulting in Tibet

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Uniform postglacial slip-rate along the central 600 km of the Kunlun Fault (Tibet), from 26Al, 10Be, and 14C dating of riser offsets, and climatic origin of the regional morphology

1 reference

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1 reference

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Quaternary extension in southern Tibet: Field observations and tectonic implications

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1 reference

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Current plate motions

1 reference

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inferred from DOI database lookup

Tibetan, Variscan, and Precambrian Basement Reactivation: Products of Continental Collision

1 reference

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based on heuristic

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The Tectonic Evolution of the Tibetan Plateau

1 reference

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inferred from DOI database lookup

Tectonic transpression in Caledonian Spitsbergen

1 reference

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based on heuristic

inferred from DOI database lookup

Change from Late Tertiary compression to Quaternary extension in southern Tibet during the India-Asia Collision

1 reference

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based on heuristic

inferred from DOI database lookup

Fault plane solutions of earthquakes and active tectonics of the Tibetan Plateau and its margins

1 reference

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based on heuristic

inferred from DOI database lookup

Formation and evolution of strike-slip faults, rifts, and basins during the India-Asia Collision: An experimental approach

1 reference

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based on heuristic

inferred from DOI database lookup

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1 reference

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1 reference

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based on heuristic

inferred from DOI database lookup

Identifiers

10.1029/2002TC001361

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