GIG OpenIR  > 同位素地球化学国家重点实验室
Zhang, L. Y.1,2; Fan, W. M.1,2,3; Ding, L.1,2; Ducea, M. N.4,5; Pullen, A.6; Li, J. X.1,2; Sun, Y. L.1,2; Yue, Y. H.1; Cai, F. L.1,2; Wang, C.1; Peng, T. P.2,7; Sein, Kyaing8
Quaternary Volcanism in Myanmar: A Record of Indian Slab Tearing in a Transition Zone From Oceanic to Continental Subduction
Source PublicationGEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
2020-08-01
Volume21Issue:8Pages:20
DOI10.1029/2020GC009091
Language英语
WOS Research AreaGeochemistry & Geophysics
WOS IDWOS:000577130200008
Indexed BySCI
Citation statistics
Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/57383
Collection同位素地球化学国家重点实验室
Corresponding AuthorZhang, L. Y.
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
4.Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA
5.Univ Bucuresti, Fac Geol & Geofiz, Bucharest, Romania
6.Clemson Univ, Dept Environm Engn & Earth Sci, Clemson, SC USA
7.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Peoples R China
8.Myanmar Geosci Soc, Yangon, Myanmar
Recommended Citation
GB/T 7714
Zhang, L. Y.,Fan, W. M.,Ding, L.,et al. Quaternary Volcanism in Myanmar: A Record of Indian Slab Tearing in a Transition Zone From Oceanic to Continental Subduction[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2020,21(8):20.
APA Zhang, L. Y..,Fan, W. M..,Ding, L..,Ducea, M. N..,Pullen, A..,...&Sein, Kyaing.(2020).Quaternary Volcanism in Myanmar: A Record of Indian Slab Tearing in a Transition Zone From Oceanic to Continental Subduction.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,21(8),20.
MLA Zhang, L. Y.,et al."Quaternary Volcanism in Myanmar: A Record of Indian Slab Tearing in a Transition Zone From Oceanic to Continental Subduction".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 21.8(2020):20.
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