Nonglacial origin for low-δ18O neoproterozoic magmas in the South China Block: Evidence from new in-situ oxygen isotope analyses using SIMS

Geology

Volumn 39, Issue 8, 2011, Pages 735-738

  Wang, Xuan Ce ^a,b,c   Li, Zheng Xiang ^b   Li, Xian Hua ^a   Li, Qiu Li ^a   Tang, Guo Qiang ^a   Zhang, Qi Rui ^a   Liu, Yu ^a  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b CURTIN UNIVERSITY   (Australia)

^c UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

CONTINENTAL RIFTING; GEOCHEMICAL PROXIES; HIGH TEMPERATURE; IN-SITU; IN-SITU TECHNIQUES; MAGMATISMS; NEOPROTEROZOIC; NEOPROTEROZOIC GLACIATIONS; OXYGEN ISOTOPE COMPOSITION; OXYGEN ISOTOPES; PALEOCLIMATES; SOUTH CHINA BLOCK; SOUTHERN CHINA; SUPRACRUSTAL ROCKS; TEMPORAL CHANGE; TWO STAGE;

ANALYTICAL GEOCHEMISTRY; GLACIAL GEOLOGY; IGNEOUS ROCKS; ISOTOPES; OXYGEN; SILICATE MINERALS; TECTONICS;

GEOCHRONOLOGY;

GLACIATION; IGNEOUS GEOCHEMISTRY; IGNEOUS ROCK; ISOTOPIC ANALYSIS; ISOTOPIC COMPOSITION; MAGMA; MAGMATISM; OROGENY; OXYGEN ISOTOPE; PLUME; PROTEROZOIC; RIFTING; SUPRACRUSTAL ROCK;

CHINA; SOUTH CHINA BLOCK;

EID: 79960599209     PISSN: 00917613     EISSN: 19432682     Source Type: Journal    
DOI: 10.1130/G31991.1     Document Type: Article

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