Magma Chamber and Crustal Channel Flow Structures in the Tengchong Volcano Area From 3-D MT Inversion at the Intracontinental Block Boundary Southeast of the Tibetan Plateau-Reference-Cited by-同舟云学术

Magma Chamber and Crustal Channel Flow Structures in the Tengchong Volcano Area From 3-D MT Inversion at the Intracontinental Block Boundary Southeast of the Tibetan Plateau

Published:2018-12 Issue:12 Volume:123 Page:11,112-11,126
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Ye Tao¹^ORCID,Huang Qinghua¹^ORCID,Chen Xiaobin²,Zhang Huiqian¹^ORCID,Chen Y. John¹³^ORCID,Zhao Li¹,Zhang Yong¹^ORCID

Affiliation:

1. Department of Geophysics; Peking University; Beijing China

2. Institute of Geology; China Earthquake Administration; Beijing China

3. Department of Ocean Science and Engineering; Southern University of Science and Technology; Shenzhen China

Funder

National Natural Science Foundation of China

Himalaya Project, China Earthquake Administration

National Basic Research (973) Program of China, Ministry of Science and Technology, China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018JB015936/fullpdf

Reference71 articles.

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4. BGMRYP (Bureau of Geology and Mineral Resources of Yunnan Province) 1990 Geological map of Yunnan Province of the People's Republic of China, 1:1000000

5. Rupture mechanism and seismotectonics of the Ms 6.5 Ludian earthquake inferred from three-dimensional magnetotelluric imaging;Cai;Geophysical Research Letters,2017

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