Is there a Neo-Tethy's subduction record earlier than arc volcanic rocks in the Sangri Group?

Acta Petrologica Sinica

Volumn 22, Issue 3, 2006, Pages 661-668

  Dong, YanHui ^a,b   Xu, JiFeng ^a   Zeng, QingGao ^c   Wang, Qiang ^a   Mao, GuoZheng ^c   Li, Jie ^a,b  

^a GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^b UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

^c Regional Geological Surveying Party of the Bureau and Exploration   (China)

Author keywords

LAM ICP MS dating; Neo tethys; Sangri Group; Tibetan Plateau; Yeba Formation

Indexed keywords

INDUCTIVELY COUPLED PLASMA MASS SPECTROMETRY; MASS SPECTROMETERS; ROCKS; VOLCANOES;

LAM-ICP-MS; NEO-TETHYS; SANGRI GROUP; TIBETAN PLATEAU; YEBA FORMATION;

VOLCANIC ROCKS;

FORMATION MECHANISM; INDUCTIVELY COUPLED PLASMA METHOD; JURASSIC-CRETACEOUS BOUNDARY; SUBDUCTION; TETHYS; VOLCANIC ERUPTION; VOLCANIC ROCK; ZIRCON;

ASIA; CHINA; EURASIA; FAR EAST; QINGHAI-XIZANG PLATEAU;

EID: 84978015127     PISSN: 10000569     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

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