Carbonic metamorphism at ultrahigh-temperatures: Evidence from North China Craton

Earth and Planetary Science Letters

Volumn 266, Issue 1-2, 2008, Pages 149-165

  Santosh, M ^a   Tsunogae, T ^b   Ohyama, H ^b   Sato, K ^c   Li, J H ^d   Liu, S J ^d  

^a KOCHI UNIVERSITY   (Japan)

^b UNIVERSITY OF TSUKUBA   (Japan)

^c Tokyo Institute of Technology ^*  (Japan)

^d PEKING UNIVERSITY   (China)

Author keywords

carbonic metamorphism; CO2; Columbia supercontinent; fluid inclusions; North China craton; ultrahigh temperature granulites

Indexed keywords

CARBONIC METAMORPHISM; MAFIC MAGMATIC INTRUSIONS; MESOPERTHITES; MICROTHERMOMETRIC; PALEOPROTEROZOIC KHONDALITE BELT;

IGNEOUS ROCKS; LASER SPECTROSCOPY; RAMAN SPECTROSCOPY; SILICATE MINERALS; TEMPERATURE;

MINERALOGY;

COLLAPSE; CONTINENTAL COLLISION; EMPLACEMENT; EXHUMATION; FLUID INCLUSION; GRANULITE FACIES; OROGENIC BELT; PRECAMBRIAN; RAMAN SPECTROSCOPY; SUPERCONTINENT; SUPRACRUSTAL ROCK; ULTRAHIGH TEMPERATURE METAMORPHISM;

ASIA; CHINA; EURASIA; FAR EAST; NORTH CHINA BLOCK;

EID: 38349077126     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2007.10.058     Document Type: Article

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