Kinematics, strain patterns, rheology, and geochronology of Woka ductile shear zone: Product of uplift of Gangdese batholith and Great Counter Thrust activity

Author:

Feng Yipeng1ORCID,Wang Genhou1,Meng Yuanku2,Li Dian3,Xu Xuming4,Lu Yang4,Li Jie4,Liu Han5

Affiliation:

1. School of Earth Sciences and Resources China University of Geosciences (Beijing) Haidian Beijing China

2. Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Earth Science and Engineering Shandong University of Science and Technology Qingdao China

3. Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation of Ministry of Natural Resources University of Technology Chengdu Chengdu China

4. Rock Analysis Laboratory Regional Geology Survey Institute Langfang China

5. Cheng du Center China Geological Survey Chengdu China

Funder

Natural Science Foundation of Shandong Province

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Reference77 articles.

1. Utilisation de I'orientation preferentielle du quartz comme marqueur de la deformation hercynienne dans le granite prehercynien du Mendic (Massif Central francais);Brunel M.;Comptes Rendus Academy Science Paris,1972

2. Tectonic features of the Mount JolmoLungma region in southern Tibet, China;Chang C. F.;Scientia Geologica Sinica,1973

3. Petrogenesis of Miocene adakitic diorite–porphyrite in middle Gangdese batholith, southern Tibet: Constraints from geochemistry, geochronology and Sr–Nd–Hf isotopes;Chen X. J.;Acta Petrologica Sinica,2014

4. Adakites from continental collision zones: Melting of thickened lower crust beneath southern Tibet

5. The Four Plutonic Belts of the Transhimalaya-Himalaya: a Chemical, Mineralogical, Isotopic, and Chronological Synthesis along a Tibet-Nepal Section

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