Volume 27 Issue 4
Aug.  2021
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TU Jiyao, JI Jianqing, ZHONG Dalai, et al., 2021. The strong activities of the Namula fault zone in the eastern Himalayan syntaxis since Pliocene, constraints from thermochronological data. Journal of Geomechanics, 27 (4): 679-690. DOI: 10.12090/j.issn.1006-6616.2021.27.04.056
Citation: TU Jiyao, JI Jianqing, ZHONG Dalai, et al., 2021. The strong activities of the Namula fault zone in the eastern Himalayan syntaxis since Pliocene, constraints from thermochronological data. Journal of Geomechanics, 27 (4): 679-690. DOI: 10.12090/j.issn.1006-6616.2021.27.04.056

The strong activities of the Namula fault zone in the eastern Himalayan syntaxis since Pliocene, constraints from thermochronological data

doi: 10.12090/j.issn.1006-6616.2021.27.04.056
Funds:

the National Natural Science Foundation of China 41603055

the Special Fund of the Institute of Geophysics, China Earthquake Administration DQJB20X10

More Information
  • Received: 2021-05-11
  • Revised: 2021-06-25
  • Published: 2021-08-28
  • To reveal the strong activities of the Namula fault zone in the eastern Himalayan syntaxis since Pliocene, this paper reports biotite 40Ar/39Ar and apatite fission track ages of 3 rock samples from the Namula fault zone, and quantitatively interpret these ages and the published ages from the adjacent areas, using a modeling code "Pecube". Biotite 40Ar/39Ar ages range from 4.44±0.71 Ma to 3.45±0.24 Ma, and apatite fission track ages range from 3.7±0.4 Ma to 1.8±0.2 Ma. The ages and simulation results show that, prior to ~3 Ma the highest exhumation rate had been located in the south of the Namula fault zone and was about 2.5 km/Ma, and the Namula fault zone had a motion feature of normal fault; Since ~3 Ma the highest exhumation rate have been located in the north of the Namula fault zone and was about 1.3 km/Ma, and the Namula fault zone had a motion feature of thrust fault. The evolution of the Namula fault zone's motion, probably have resulted from the south to north migration of the fast crust exhumation area in the eastern Himalayan syntaxis since ~8 Ma.

     

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