Lake Level Changes and Holocene Extension Rate Across the NS‐Trending Peiku Co‐Gyirong Faults, Southern Tibet

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Lake Level Changes and Holocene Extension Rate Across the NS‐Trending Peiku Co‐Gyirong Faults, Southern Tibet

Abstract: The unabated collision between the Indian and Eurasian plates has triggered large-scale strike-slip faulting and distributed normal faulting within the interior of the Tibet Plateau (e.g.,

Cited by 4 publications

References 69 publications

Late Quaternary normal faulting along the western boundary fault of Peiku Co graben in southern Nyalam-Coqen rift: Implications for extensional deformation in southern Tibet and seismic hazard

Late Quaternary normal faulting along the western boundary fault of Peiku Co graben in southern Nyalam-Coqen rift: Implications for extensional deformation in southern Tibet and seismic hazard

Tenfold lower late quaternary throw rates in central Tibet compared to southern Tibet reflect different extensional deformation mechanisms

Timing and characteristics of co-seismic surface ruptures in the Yadong rift, southern Tibet

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