The main tectonic deformation in the Pamir Western Kunlun foreland fold and thrust belt started in Early Pliocene ( about 4.6 Ma ago), and migrated gradually from the orogen to the foreland basin, with the faulting and folding becoming younger and weakened in the basin.
帕米尔&西昆仑北麓前陆褶皱冲断带的主要构造变形时间始于上新世早期(距今约4.6Ma),断层、褶皱的变形时代由山前向盆地逐步变新,变形强度由山脉向塔里木盆地逐步减弱。
The V shape coupling relationship between the basin and the range is located between the Tarim basin and the West Kunlun tectonic belt, just above the upwarped area of Moho.
塔里木盆地南缘与西昆仑构造带间呈V型盆山耦合关系,其下方恰好是莫霍面上隆区。
Tectonic electrical characteristics and a-model subducting patterns of Southwest Tarim basin-west Kunlun area
塔里木盆地西南部&西昆仑地区构造电性特征与A型俯冲模式
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