Fault slip rates and crustal strain partitioning in the southeastern borderland of the Tibetan Plate

来源 :2014中国科学院计算地球动力学重点实验室国际学术研讨会暨实验室学术年会(2014计算地球动力学前沿问题国际学术研讨会暨 | 被引量 : 0次 | 上传用户:my_code
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The southeastern borderland of the Tibetan Plateau is one of the channelsfor the lower-crustal flow beneath the Tibetan Plateau.Quantitative study oncrustal motion and deformation provide important insights into deformation pattern of the whole Tibetan Plateau.
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