河北阳原新生代玄武岩中橄榄岩捕虏体矿物化学:华北岩石圈地幔演化

陈曦; 郑建平

Volume 34 Issue 1

Jan. 2009

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Article Navigation > Earth Science > 2009 > 34(1): 203-219

CHEN Xi, ZHENG Jian-ping, 2009. Mineral Chemistry of Peridotite Xenoliths in Yangyuan Cenozoic Basalts: Significance for Lithospheric Mantle Evolution beneath the North China Craton. Earth Science, 34(1): 203-219.

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Mineral Chemistry of Peridotite Xenoliths in Yangyuan Cenozoic Basalts: Significance for Lithospheric Mantle Evolution beneath the North China Craton

CHEN Xi,
ZHENG Jian-ping^,

Faculty of Earth Sciences, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2008-10-24
Publish Date: 2009-01-25

Abstract

Abstract

The compositions of the minerals and peridotites, especially trace elements of clinopyroxene (Cpx) can well reflect the characteristics of the subcontinental lithospheric mantle (SCLM). Based on the petrographical study of peridotite xenoliths in Yangyuan Cenozoic basalts and chemical study of minerals, the paper mainly analyzes the LAM-ICP-MS trace element com- positions of Cpx from the Yangyuan peridotitic xenoliths and discusses the nature and evolution of the Cenozoic SCLM beneath the center of the Trans-North China orogen. The SCLM beneath the Yangyuan area is heterogeneous, forming from the different partial melting of the primitive mantle: most melted less than 5% of the total, except a few among 15%-20%. The coex- istence of the fertile and refractory-transitional mantle was better explained by the effects of heterogeneous erosion, transformation and replacement of asthenospheric materials on the cratonic lithosphere mantle.
- peridotites,
- mineral chemistry,
- asthenospheric erosion,
- mantle replacement,
- heterogeneity,
- North China craton

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Mineral Chemistry of Peridotite Xenoliths in Yangyuan Cenozoic Basalts: Significance for Lithospheric Mantle Evolution beneath the North China Craton

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