Pattern and kinematic polarity of late Mesozoic extension in continental NE Asia: Perspectives from metamorphic core complexes

Author:

Wang Tao1,Zheng Yadong2,Zhang Jinjiang2,Zeng Lingsen1,Donskaya Tatiana3,Guo Lei1,Li Jianbo1

Affiliation:

1. Institute of Geology; Chinese Academy of Geological Sciences; Beijing; China

2. Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences; Peking University; Beijing; China

3. Institute of the Earth's Crust of the Siberian Branch of the Russian Academy of Sciences; Irkutsk; Russia

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference203 articles.

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2. A new terrane subdivision for Mongolia: Implications for the Phanerozoic crustal growth of central Asia;Badarch;J. Asian Earth Sci.,2002

3. Regional geology of Beijing municipality (in Chinese with English abstract);Beijing Bureau of Geology and Mineral Resources;Geol. Mem. Ser.,1991

4. First evidence for the manifestation of Mesozoic mafic-ultramafic magmatism within the Selenga-Stanovoi superterrane, southeastern framing of the Siberian craton;Buchko;Dokl. Earth Sci.,2005

5. The south Tibetan detachment system, Himalayan orogen: Extension contemporaneous with and parallel to shortening in a collisional mountain belt;Burchfiel;Mem. Geol. Soc. Am.,1992

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