内蒙古集宁橄榄岩包体微区微量元素与Sr同位素特征及其岩石圈地幔演化的指示意义

王瑞雪; 刘勇胜; 宗克清; 胡兆初

doi:10.3799/dqkx.2017.041

Volume 42 Issue 4

Apr. 2017

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Article Navigation > Earth Science > 2017 > 42(4): 511-526

Wang Ruixue, Liu Yongsheng, Zong Keqing, Hu Zhaochu, 2017. In-Situ Trace Elements and Sr Isotopes in Peridotite Xenoliths from Jining: Implications for Lithospheric Mantle Evolution. Earth Science, 42(4): 511-526. doi: 10.3799/dqkx.2017.041

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Wang Ruixue, Liu Yongsheng, Zong Keqing, Hu Zhaochu, 2017. In-Situ Trace Elements and Sr Isotopes in Peridotite Xenoliths from Jining: Implications for Lithospheric Mantle Evolution. Earth Science, 42(4): 511-526. doi: 10.3799/dqkx.2017.041

Citation:

Wang Ruixue, Liu Yongsheng, Zong Keqing, Hu Zhaochu, 2017. In-Situ Trace Elements and Sr Isotopes in Peridotite Xenoliths from Jining: Implications for Lithospheric Mantle Evolution. Earth Science, 42(4): 511-526. doi: 10.3799/dqkx.2017.041

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In-Situ Trace Elements and Sr Isotopes in Peridotite Xenoliths from Jining: Implications for Lithospheric Mantle Evolution

doi: 10.3799/dqkx.2017.041

Wang Ruixue^1
,,
Liu Yongsheng^{2,3
,
,},
Zong Keqing^2,3,
Hu Zhaochu^2,3

1.
School of Lisiguang, China University of Geosciences, Wuhan430074, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan430074, China

Received Date: 2016-11-25
Publish Date: 2017-04-15

Abstract

Abstract

Further research on the lithospheric mantle beneath western North China craton is significant in order to understand the degree and evolution of its thinning and transformation thoroughly. Mantle peridotite xenoliths in the Cenozoic alkaline basalts from Jining of western North China craton provide important constraints on the nature and evolution of the lithospheric mantle beneath this area. The samples were analyzed by using LA-ICP-MS and LA-MC-ICP-MS to obtain major element, trace element and Sr isotopic compositions. According to the mineral composition, the peridotites were classified into two groups: (1) Clinopyroxene (Cpx)-poor peridotites (Cpx < 8%), which might have experienced high-degree partial melting, suggest relict of old and refractory lithospheric mantle under this area. (2) lherzolites (Cpx > 13%). They might have experienced low-degree partial melting, representing the fertilized lithospheric mantle. Cpx grains in Type 1 peridotite have relatively low REE contents and show slightly LREE-enriched patterns, while Cpx grains in Type 2 peridotite show both LREE-enriched and slightly LREE-depleted REE patterns. Most Cpx grains show core-rim variations in strong incompatible elements and Sr isotopic compositions. These features indicate that the peridotites could have experienced metamorphism. Variations of (La/Yb)_N and Ti/Eu ratios imply multistage metasomatism, which could have been caused by silicate and carbonatite melts/fluids associated with the Paleo-Asian oceanic plate subduction.
- western North China craton,
- Jining,
- perdotite xenoliths,
- in situ,
- Sr isotope,
- Paleo-Asian oceanic plate,
- geochemistry

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References(99)

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