山东昌乐新生代碱性玄武岩与地幔捕虏体中各类单斜辉石的地球化学特征及其意义

刘晓寒; 孔凡梅; 李旭平; 魏贵东; 刘浩; 王笑; 贺振鹏

doi:10.3799/dqkx.2018.360

Volume 44 Issue 4

Apr. 2019

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Liu Xiaohan, Kong Fanmei, Li Xuping, Wei Guidong, Liu Hao, Wang Xiao, He Zhenpeng, 2019. Geochemical Characteristics of Clinopyroxenes from Cenozoic Alkalic Basalts and Mantle Xenoliths in Changle, Shandong Province and Its Significance. Earth Science, 44(4): 1169-1185. doi: 10.3799/dqkx.2018.360

Citation:

Liu Xiaohan, Kong Fanmei, Li Xuping, Wei Guidong, Liu Hao, Wang Xiao, He Zhenpeng, 2019. Geochemical Characteristics of Clinopyroxenes from Cenozoic Alkalic Basalts and Mantle Xenoliths in Changle, Shandong Province and Its Significance. Earth Science, 44(4): 1169-1185. doi: 10.3799/dqkx.2018.360

Citation:

Liu Xiaohan, Kong Fanmei, Li Xuping, Wei Guidong, Liu Hao, Wang Xiao, He Zhenpeng, 2019. Geochemical Characteristics of Clinopyroxenes from Cenozoic Alkalic Basalts and Mantle Xenoliths in Changle, Shandong Province and Its Significance. Earth Science, 44(4): 1169-1185. doi: 10.3799/dqkx.2018.360

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Geochemical Characteristics of Clinopyroxenes from Cenozoic Alkalic Basalts and Mantle Xenoliths in Changle, Shandong Province and Its Significance

doi: 10.3799/dqkx.2018.360

School of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao 266590, China

Received Date: 2018-09-17
Publish Date: 2019-04-15

Abstract

Abstract

Changle is located both in the eastern section of the North China craton (NCC) and the middle part of Tancheng-Lujiang (Tan-Lu) fault zone that is characterized with widespread Cenozoic alkaline basalts wrapping a number of mantle xenoliths inside. For the better understanding of the evolution mechanism of the North China craton, three major types of clinopyroxenes are recognized on the basis of the petrography, mineralogy and mineral geochemical characteristics in this study. The first type is the protosomatic clinopyroxene occurred in mantle-derived xenoliths.The content of major and trace elements in this kind of clinopyroxenes show decoupling phenomenon with inconsistent tendencies. Moreover, the LREE and HREE characteristics of the protosomatic clinopyroxenes show that they had experienced multi-stage mantle metasomatism and different degrees of partial melting (no more than 10% partial melting in the spinel phase) and the metasomatic melts include mantle-derived alkali (K) and Al-enriched silicate melts/fluids, possibly contain the carbonate melts. The second kind is cribriform clinopyroxene in mantle-derived xenoliths known as the co-product of partial melting and melt metasomatism. The effect of partial melting exhibits a gradually strengthening from the non-meshing part to the areas far away from sieve mesh, then the areas around the sieve mesh. The areas far away from the sieve mesh record characteristics of a prior metasomatism of alkali (K) and Al-enriched melt before the basaltic magmatism while the areas around the sieve mesh show the strongest effect of late stage basaltic melts. The third type is the the clinopyroxenes in the corona of the protosomatic clinopyroxene or sieve-textured clinopyroxene in mantle-derived xenoliths and the clinopyroxene phenocrystsin alkaline basalts that share the similar geochemical compositions and P-T conditions that reveal a HFSE positive anomaly and a LILE negative anomaly that are strongly influenced by the OIB characteristic host basalt. The characteristics of multiple-stage "melt-effect" and different degrees of partial melting of the clinopyroxenes in the Changle Cenozoic alkaline basalt are the performance of the embodiment of lithospheric mantle heterogeneity in the study area.
- Cenozoic alkaline basalts,
- clinopyroxene,
- mantle xenolith,
- geochemistry

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References(84)

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Geochemical Characteristics of Clinopyroxenes from Cenozoic Alkalic Basalts and Mantle Xenoliths in Changle, Shandong Province and Its Significance

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