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根据中、美两国合作开展的西藏深反射地震结果,提出雅鲁藏布江缝合带（YZS）的“双陆内俯冲”构造模式和缝合带南、北分别存在着不同特征的、规模不一的部分熔融层；提出YZS处断裂向深部延深有限,认为YZS处地壳增厚有4种机制：①地壳规模的大的俯冲增厚；②上部地壳内的俯冲和背冲增厚；③下地壳内的底部垫托增厚和挤压增厚；④深部熔融体的向上挤入而引起的地壳增厚.提出可能存在两条大的伸展性断裂,造成江孜南、北地块间出现了大升降.
According to the deep reflection seismic result of Tibet and China carried out by China and the United States, it is proposed that the “double subduction” structural model of the Yarlung Zangbo suture zone (YZS) and the different characteristics of the " Part of the melted layer. It is proposed that there is a finite depth of extension at the YZS fault. There are four mechanisms for the thickening of the crust at YZS: ① large subduction and thickening of the crust; ② subduction and thrusting thickening in the upper crust; and ③ lower crust The thickening and extrusion thickening of the bottom padding in the inner layer; ④ thickening of the crust caused by the upward extrusion of deep melt, suggesting that there may be two large extensional faults, resulting in a large Lift.