Indian punch rifts Tibet

Paul A Kapp, Jerome H. Guynn

Research output: Contribution to journalArticle

107 Citations (Scopus)

Abstract

The strikes of late Cenozoic normal faults in Tibet fan systematically from a northwesterly to northeasterly direction from west to east. They exhibit an axis of symmetry that bisects the Himalayan arc and trends subparallel to India-Asia motion. The two-dimensional stress field inferred from the spatial pattern of normal-fault orientations can be explained solely by collisional stresses localized along a southern part of the Himalayan arc. Continued insertion of Indian crust into Tibet can explain the persistence of extension and may be increasing plateau crustal thickness and elevation coeval with rifting.

Original languageEnglish (US)
Pages (from-to)993-996
Number of pages4
JournalGeology
Volume32
Issue number11
DOIs
StatePublished - Nov 2004

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normal fault
crustal thickness
stress field
rifting
symmetry
persistence
plateau
crust
Asia
trend

Keywords

  • Continental collision
  • Extension
  • Himalayan arc
  • India
  • Plateau development
  • Tibet

ASJC Scopus subject areas

  • Geology

Cite this

Indian punch rifts Tibet. / Kapp, Paul A; Guynn, Jerome H.

In: Geology, Vol. 32, No. 11, 11.2004, p. 993-996.

Research output: Contribution to journalArticle

Kapp, PA & Guynn, JH 2004, 'Indian punch rifts Tibet', Geology, vol. 32, no. 11, pp. 993-996. https://doi.org/10.1130/G20689.1
Kapp, Paul A ; Guynn, Jerome H. / Indian punch rifts Tibet. In: Geology. 2004 ; Vol. 32, No. 11. pp. 993-996.
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