中条山上玉坡地区黑云母片岩成岩时代及成因

张晗; 孙丰月; 胡安新

doi:10.3799/dqkx.2013.002

Volume 38 Issue 1

Jan. 2013

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ZHANG Han, SUN Feng-yue, HU An-xin, 2013. Geochemistry and Geochronology of Shangyupo Biotite Schist in the Zhongtiaoshan Mountains: Implications for Its Petrogenesis. Earth Science, 38(1): 10-24. doi: 10.3799/dqkx.2013.002

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ZHANG Han, SUN Feng-yue, HU An-xin, 2013. Geochemistry and Geochronology of Shangyupo Biotite Schist in the Zhongtiaoshan Mountains: Implications for Its Petrogenesis. Earth Science, 38(1): 10-24. doi: 10.3799/dqkx.2013.002

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Geochemistry and Geochronology of Shangyupo Biotite Schist in the Zhongtiaoshan Mountains: Implications for Its Petrogenesis

doi: 10.3799/dqkx.2013.002

1.
College of Earth Science, Jilin University, Changchun 130061, China
2.
Institute of Mineral Resources, China Academy of Geological Sciences, Beijing 100037, China

Received Date: 2012-02-15
Publish Date: 2013-01-15

Abstract

Abstract

The primary compositions of the anticline core at Shangyupo are Beiyu meta-granitoid, meta-rhyolite and meta-mafic rocks. The age and petrogenesis of the biotite schist have been under debate for a very long time. The petrology features and geochemistry of Shangyupo amphibole/scapolite biotite schist are cricoid gradually distributed from the anticlinal core to its edge. The K, Ca, Na, Rr, Sr and Ba have been changed systematically by the high salinity fluid from the ductile shear belts, and Ta and LREE are also shown to have been dramatically changed in this event. LA-MC-ICPMS zircon U-Pb dating for the Shangyupo meta-rhyolite and the meta-ryholite of Jiangxian group yield the weighted mean ²⁰⁷Pb/²⁰⁶Pb age of 2 160.5±7.8 Ma and 2 161.3±1.5 Ma respectively. The Shangyupo meta-ryhorite and biotite schist may have been formed during the Jiangxian volcano event between 2.20~2.15 Ga, based on the chronology and comparison to related rocks. The HFSE pairs show that the biotite schist is a subalkaline mafic rocks instead of the alkaline mafic rocks as previously suggested. The Jiangxian event may represent a tensional event related to the subduction, based on the comprehensive geological information of Zhongtiaoshan area.
- Zhongtiaoshan Mountains,
- biotite schist,
- lithogeochemistry,
- fluid,
- LA-MC-ICPMS zircon U-Pb dating

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References(46)

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Geochemistry and Geochronology of Shangyupo Biotite Schist in the Zhongtiaoshan Mountains: Implications for Its Petrogenesis

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