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墨脱断裂带背崩乡段深部电性结构研究

王刚 张翔 常小鹏 葛欣旺 野柳帅 方慧 裴发根 肖都 张小博 张耀阳 彭炎 白大为 乔汉青

地球与行星物理论评(中英文)2025,Vol.56Issue(6):699-709,11.
地球与行星物理论评(中英文)2025,Vol.56Issue(6):699-709,11.DOI:10.19975/j.dqyxx.2025-030

墨脱断裂带背崩乡段深部电性结构研究

The deep electrical structure of Motuo fault zone in Beibeng area

王刚 1张翔 2常小鹏 2葛欣旺 2野柳帅 2方慧 3裴发根 3肖都 1张小博 4张耀阳 1彭炎 4白大为 1乔汉青4

作者信息

  • 1. 深部探测与成像全国重点实验室中国地质科学院地球物理地球化学勘查研究所,天津 300300||自然资源部地球物理电磁法探测技术重点实验室,天津 300300
  • 2. 中国地质调查局地球物理调查中心,天津 300300
  • 3. 深地探测与矿产勘查全国重点实验室中国地质科学院地球物理地球化学勘查研究所,天津 300300||自然资源部地球物理电磁法探测技术重点实验室,天津 300300
  • 4. 自然资源部地球物理电磁法探测技术重点实验室,天津 300300
  • 折叠

摘要

Abstract

To elucidate the contact relationship between Indian and Eurasian plates along the Yarlung-Zangbo suture zone(IYS)and associated geodynamic processes,we acquired a high-resolution magnetotelluric(MT)pro-file extending 20 km across the Motuo fault zone near Beibeng Township,Motuo County,eastern Xizang.This NW-SE oriented transect employed 30 MT stations with approximately 300-m spacing,covering frequency bands of 10000-0.0001 Hz to resolve crustal structure down to 30 km depth.Key findings from the electrical resistivity model reveal:(1)At shallow crustal levels(<5 km depth),the Motuo fault system exhibits a negative flower struc-ture characterized by downward-converging conductive shear zones,diagnostic of dominant strike-slip deforma-tion.(2)Preservation of Indian slab subduction traces beneath the Lhasa Block along the IYS,with possible deve-lopment of a pop-up structure in the Indian upper crust near the eastern Himalayan syntaxis.(3)The resistive Lhasa Terrane upper crust is~20 km thick-33%thinner than the 30-km average in southern Xizang.This disparity im-plies either:(ⅰ)incomplete syn-collisional crustal shortening due to strain partitioning into strike-slip faults,or(ⅱ)absence of crustal growth episodes that thickened the Lhasa Terrane.(4)A mid-crustal conductor at 15-30 km depth aligns with the suture zone.Its upward-flaring geometry indicates southward migration of melts from the Lhasa lower crust,which is facilitated by transpressional uplift along the IYS.These results demonstrate that the Motuo fault system operates as a crustal-scale transfer zone,where strike-slip kinematics preserve early collisional features while enabling melt migration through reactivated suture structures.The integrated model provides new constraints on strain accommodation mechanisms during continental indentation.

关键词

雅鲁藏布江缝合带/墨脱断裂带/大地电磁测深/内部结构

Key words

Yarlung-Zangbo suture zone/Motuo fault zone/magnetotelluric/structural framework

分类

天文与地球科学

引用本文复制引用

王刚,张翔,常小鹏,葛欣旺,野柳帅,方慧,裴发根,肖都,张小博,张耀阳,彭炎,白大为,乔汉青..墨脱断裂带背崩乡段深部电性结构研究[J].地球与行星物理论评(中英文),2025,56(6):699-709,11.

基金项目

中国地质调查局地质调查资助项目(DD20250102801,DD20240101902) (DD20250102801,DD20240101902)

华北—东北大地电磁子网一期(2024ZD1000203-06) (2024ZD1000203-06)

国家自然科学基金资助项目(41804075)Supported by the China Geological Survey(Grant Nos.DD20250102801,DD20240101902),China Magnetotelluric Array(Grant No.2024ZD1000203-06)and the National Natural Science Foundation of China(Grant No.41804075) (41804075)

地球与行星物理论评(中英文)

2097-1893

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