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ＩＮＤＥＰＴＨＭＴ研究结果表明，在雅鲁藏布江未发现反映深断裂的电性显示，而在江孜和仁布之间见有规模宏大、底界深达５５ｋｍ、向北倾斜的低阻高导体。这表明该区可能为雅鲁藏布江缝合带在地表出露的实际位置。高导体范围内存在３组反映断裂构造的电性梯度带和畸变带。３条断裂带向北倾斜，沿纵深向主断裂带Ｆ３汇聚。其北侧，发育多条南倾断裂，它们共同构成雅鲁藏布江缝合带发散状断裂构造特征。大规模高导体的存在与地下热状态是密切相关的。
INDEPTHMT results show that in the Brahmaputra, no evidence of deep faults is found, while there is a large-scale, low-resistivity and high-conductivity conductor with a depth of 55 km in the bottom between Gyangze and Renbu. This shows that the area may be the actual location of the Brahmaputra suture exposed on the surface of the earth. There are three sets of electrical gradient and distortion bands in the high conductor range reflecting the fault structure. The three faults are inclined northward and converge to the main fault F3 along the depth. On its northern side, a number of southern-dipping faults are developed, which together constitute the divergent structural features of the Yarlung Zangbo suture. The existence of large-scale high-conductor and underground thermal state are closely related.