Coexistence of MORB- and OIB-like dolerite intrusions in the Purang ultramafic massif, SW Tibet: A paradigm of plume-influenced MOR-type magmatism prior to subduction initiation in the Neo-Tethyan lithospheric mantle-Reference-Cited by-同舟云学术

Coexistence of MORB- and OIB-like dolerite intrusions in the Purang ultramafic massif, SW Tibet: A paradigm of plume-influenced MOR-type magmatism prior to subduction initiation in the Neo-Tethyan lithospheric mantle

Published:2019-01-25 Issue:7-8 Volume:131 Page:1276-1294
ISSN:0016-7606
Container-title:GSA Bulletin
language:en
Short-container-title:

Author:

Zheng Hao¹,Huang Qiangtai¹,Kapsiotis Argyrios¹,Lenaz Davide²,Velicogna Matteo²,Xu Chi¹,Cheng Chen¹,Xia Bin¹,Liu Weiliang¹,Xiao Yang¹,Yang Peng¹³

Affiliation:

1. Key Laboratory of Offshore Oil Exploration and Development of Guangdong Higher Education Institutes, Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, School of Marine Science, Sun Yat-sen University, Guangzhou 510275, China

2. Department of Mathematics and Geosciences, University of Trieste, Via Weiss 8, Trieste 34128, Italy

3. School of Earth and Environmental Sciences, The University of Queensland, Brisbane QLD 4072, Australia

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/131/7-8/1276/4745364/1276.pdf

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