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FU Jiangang, LI Guangming, WANG Genhou, HUANG Yong, ZHANG Linkui, DONG Suiliang, LIANG Wei. 2018. Establishment of the North Himalayan double gneiss domes: evidence from field identification of the Cuonadong dome, south Tibet[J]. Geology in China, 45(4): 783-802. doi: 10.12029/gc20180410
Citation: FU Jiangang, LI Guangming, WANG Genhou, HUANG Yong, ZHANG Linkui, DONG Suiliang, LIANG Wei. 2018. Establishment of the North Himalayan double gneiss domes: evidence from field identification of the Cuonadong dome, south Tibet[J]. Geology in China, 45(4): 783-802. doi: 10.12029/gc20180410
shu

Establishment of the North Himalayan double gneiss domes: evidence from field identification of the Cuonadong dome, south Tibet

  • 1.

    Chengdu Institute of Geology and Mineral Resources, China Geological Survey, Chengdu 610081, Sichuan, China

  • 2.

    School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China

    • Fund Project: Supported by National Natural Science Foundation of China (No. 41602214), Ministry of Science and Technology Program (No. 2016YFC060308), and China Geological Survey Program (No. DD20160015)
More Information
  • Author Bio: FU Jiangang, male, born in 1987, Ph.D, majors in structural geology and metallogenic theory; Email:fujiangangcd@163.com
  • Corresponding author: LI Guangming, male, born in 1965, professor, engages in mineral resource exploration and metallogenic prediction; E-mail:13982257109@163.com 
Received Date:  22 May 2016
Revised Date:  26 August 2017
Publish Date:  25 August 2018
    Abstract

  • The Cuonadong dome, which is firstly reported in this study, is exposed as an east-southern important part of the North Himalayan gneiss domes (NHGD), . The Cuonadong dome is located in the southern part of the Zhaxikang ore concentration area, which is divided into three tectono-lithostratigraphic units by two circle faults around the dome, which is geometrically from upper to lower (or from outer to inner) in order of cap rocks, decollement system and core, with the outer fault being upper detachment fault and the inner fault being lower detachment fault. The Cuonadong dome is a magmatic orthogneiss and leucogranite mantled by orthogneiss and metasedimentary rocks, which in turn are overlain by Jurassic metasedimentary and sedimentary rocks. The grades of metamorphism and structural deformation increase towards the core, which is consistent with the low to high degree metamorphic schist, tourmaline granitic biotite gneiss, garnet mica gneiss, and mylonitic quartz mica gneiss of the Ridang Formation. Their typical metamorphic minerals include garnet, staurolite, sillimanite and kyanite. The Cuonadong dome has preserved evidence for four major deformational events:southward thrust, early approximately N-S extensional deformation, main approximately E-W extensional deformation, and late collapse structural deformation around the core of the Cuonadong dome, which are consistent with four groups of lineation, respectively. The form of the Cuonadong dome resulted from the main E-W extension which resulted from eastward flow of middle or lower crust from beneath Tibet accommodated by northward oblique underthrusting of Indian crust beneath Tibet. The establishment of the Cuonadong dome has enhanced and enriched the significance of the E-W extension of the NHGD, which is further divided into two structural dome zones according to the different extensional directions:approximately NS extensional North Himalayan gneiss domes (NS-NHGD) and E-W extensional North Himalayan gneiss domes (EW-NHGD).

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