Synchronous N-S and E-W extension at the Tibet-to-Himalaya transition in NW Bhutan

F. J. Cooper, Kip Hodges, R. R. Parrish, N. M W Roberts, M. S A Horstwood

Research output: Contribution to journalArticle

11 Citations (Scopus)

Abstract

Despite 50Myr of continuous continent-continent collision, contractional structures in the Himalayan-Tibetan orogen are today limited to the northern and southern margins of the system, while extension dominates much of the interior. On the Tibetan Plateau, Cenozoic E-W extension has been accommodated by strike-slip faults and extensional grabens, while N-S extension at the Tibet-to-Himalaya transition has been accommodated by the South Tibetan fault system (STFS). The genetic relationship between N-S and E-W extension is disputed, although age constraints indicate temporal overlap of at least 7Myr. In NW Bhutan the two intersect where the STFS basal detachment is cut by the Yadong cross structure (YCS), an extensional half graben that provides a rare opportunity to constrain relative timings. We report U-Pb zircon dates from four STFS footwall leucogranites consistent with episodic magmatism during the middle-late Miocene and in situ U(-Th)-Pb monazite and xenotime dates from three metasedimentary rocks ranging from late Oligocene to middle Miocene. We suggest that amphibolite facies footwall metamorphism was ongoing at the time the basal STFS detachment initiated as a ductile structure in the middle-late Miocene. Late-stage granitic intrusions may reflect footwall melting during extensional exhumation along the STFS, but post-metamorphic and post-intrusion fabrics suggest that most displacement occurred after emplacement of the youngest granites. Some of the oldest YCS-related fabrics are found in a deformed 14Ma leucogranite, implying middle Miocene ductile deformation. This observation, along with evidence for subsequent brittle YCS deformation, suggests that N-S and E-W extensional structures in the area had protracted and overlapping deformation histories. Key Points Relationship between N-S and E-W extension in Himalayan-Tibetan orogen is unclear In NW Bhutan, N-S and E-W extensional structures intersect Both sets of structures had protracted and overlapping deformation histories

Original languageEnglish (US)
Pages (from-to)1375-1395
Number of pages21
JournalTectonics
Volume34
Issue number7
DOIs
StatePublished - Jul 1 2015

Fingerprint

Bhutan
Tibet
footwall
Miocene
continents
detachment
intrusion
Strike-slip faults
histories
xenotime
leucogranite
ductile deformation
metasedimentary rock
monazite
history
Melting
amphibolite facies
strike-slip fault
exhumation
graben

Keywords

  • geochronology
  • leucogranite
  • monazite
  • South Tibetan fault system
  • Yadong cross structure
  • zircon

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics

Cite this

Cooper, F. J., Hodges, K., Parrish, R. R., Roberts, N. M. W., & Horstwood, M. S. A. (2015). Synchronous N-S and E-W extension at the Tibet-to-Himalaya transition in NW Bhutan. Tectonics, 34(7), 1375-1395. https://doi.org/10.1002/2014TC003712

Synchronous N-S and E-W extension at the Tibet-to-Himalaya transition in NW Bhutan. / Cooper, F. J.; Hodges, Kip; Parrish, R. R.; Roberts, N. M W; Horstwood, M. S A.

In: Tectonics, Vol. 34, No. 7, 01.07.2015, p. 1375-1395.

Research output: Contribution to journalArticle

Cooper, FJ, Hodges, K, Parrish, RR, Roberts, NMW & Horstwood, MSA 2015, 'Synchronous N-S and E-W extension at the Tibet-to-Himalaya transition in NW Bhutan', Tectonics, vol. 34, no. 7, pp. 1375-1395. https://doi.org/10.1002/2014TC003712
Cooper, F. J. ; Hodges, Kip ; Parrish, R. R. ; Roberts, N. M W ; Horstwood, M. S A. / Synchronous N-S and E-W extension at the Tibet-to-Himalaya transition in NW Bhutan. In: Tectonics. 2015 ; Vol. 34, No. 7. pp. 1375-1395.
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