Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang

CHEN Jiping; LUO Ting; WANG Hui; LIAO Qun'an; ZHANG Xionghua; CHEN Enke; WANG Jiejie; MENG Qinyu; LIU Xiaoming

Northwestern Geology > 2016 > 49(4): 51-61.

CHEN Jiping, LUO Ting, WANG Hui, et al. Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang[J]. Northwestern Geology, 2016, 49(4): 51-61.

Citation:

CHEN Jiping, LUO Ting, WANG Hui, et al. Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang[J]. Northwestern Geology, 2016, 49(4): 51-61.

Citation:

CHEN Jiping, LUO Ting, WANG Hui, et al. Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang[J]. Northwestern Geology, 2016, 49(4): 51-61.

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Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang

1. Shaanxi Center of Geological Survey, Xi'an 710068, Shaanxi, China;
2. School of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China;
3. State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, Shaanxi, China

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Received Date: March 01, 2016
Revised Date: May 02, 2016
Available Online: July 28, 2022
Published Date: December 04, 2016

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Abstract

Abstract

Huangshandong, Xiangshan and Tudun plutons are multiple-phase intrusive complexs, which show clear intrusive contact boundaries with wall rock. These intrusions are mainly composed of peridotite and gabbro. Peridotite has orthopyroxene or plagioclase, while clinopyroxene is augite or diopside. The Huangshandong, Xiangshan and Tudun plutons are mainly tholeiitic in composition, and some of them show calc-alkaline and alkaline characteristics. Chondrite-normalized rare earth element patterns show flat feature or slight enrichment in LREE. Zircon Hf isotopic compositions indicate that the Huangshandong, Xiangshan and Tudun intrusive complexes are derived from the depleted mantle source.Huangshandong, Xiangshan and Tudun plutons are not the remnants of subducted oceanic crust or Alaska-type rocks, but they are formed by the underplating of depleted mantle source.
- mafic-ultramafic rocks,
- zircon,
- Hf isotope,
- source characteristics,
- eastern Tianshan

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Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang

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Zircon Hf Isotope Characteristics and Source of Mafic-ultramafic Intrusions in Huangshan Region, Xinjiang

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