Importance of melt circulation and crust-mantle interaction in the lithospheric evolution beneath the North China Craton: Evidence from Mesozoic basalt-borne clinopyroxene xenocrysts and pyroxenite xenoliths

Lithos

Volumn 96, Issue 1-2, 2007, Pages 67-89

  Zhang, Hong Fu ^a   Ying, Ji Feng ^a   Shimoda, Gen ^b   Kita, Noriko T ^b   Morishita, Yuichi ^b   Shao, Ji An ^c   Tang, Yan Jie ^a  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b NATIONAL INSTITUTE OF ADVANCED INDUSTRIAL SCIENCE AND TECHNOLOGY AIST   (Japan)

^c PEKING UNIVERSITY   (China)

Author keywords

Clinopyroxene xenocryst; Crust mantle interaction; Lithospheric evolution; North China Craton; Pyroxenite xenolith

Indexed keywords

BASALT; CHEMICAL COMPOSITION; CLINOPYROXENE; CRUST-MANTLE BOUNDARY; GRANULITE FACIES; HOST ROCK; ION EXCHANGE; LITHOSPHERE; MELT INCLUSION; MESOZOIC; PYROXENITE; XENOLITH; ZONING;

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

EID: 34248575335     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2006.10.002     Document Type: Article

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