Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China
University of Chinese Academy of Sciences, Beijing 100049, China
Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China
Bo Li
Research Institute of Petroleum Exploration & Development-Northwest (NWGI), PetroChina Lanzhou 730020, China
Qizhe Tang
School of Information Engineering, Huzhou University, Huzhou, Zhejiang 313000, China
Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii 96822, USA
Dongzhou Zhang
Hawaii Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii 96822, USA
Wenge Zhou
Key Laboratory of High-Temperature and High-Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, Guizhou 550081, China
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Total article views: 2,606 (including HTML, PDF, and XML)
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1,699
834
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2,606
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Total article views: 3,876 (including HTML, PDF, and XML)
Thereof 3,699 with geography defined
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Total article views: 2,606 (including HTML, PDF, and XML)
Thereof 2,500 with geography defined
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Total article views: 1,270 (including HTML, PDF, and XML)
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Eclogite is a major factor in the initiation of delamination during orogenic collision. According to the equations of state of main minerals of eclogite under high temperature and high pressure, the densities of eclogite along two types of delamination in Tibet are provided. The effects of eclogite on the delamination process are discussed in detail. A high abundance of garnet, a high Fe content, and a high degree of eclogitization are more conducive to instigating the delamination.
Eclogite is a major factor in the initiation of delamination during orogenic collision....
