作者: Xibin Tan , Yiduo Liu , Yuan-Hsi Lee , Renqi Lu , Xiwei Xu
DOI: 10.1016/J.EPSL.2018.12.001
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摘要: Abstract Knowledge of how strain is partitioned and accommodated in crustal shortening provides fundamental constraints on evaluating tectonic models of orogenic plateaus. A number of tectonic models have been proposed for the central Longmen Shan along the eastern Tibetan Plateau margin, including mid-crustal channel flow, upper crustal shortening, and whole crust shearing. However, it remains controversial whether these models work in the Min Shan–northern Longmen Shan area, and if so, how the models …