内蒙古额济纳地区奥陶纪火山岩地球化学特征及其地质意义

陈智斌; 于洋; 薄海军

doi:10.3799/dqkx.2018.346

Volume 45 Issue 2

Feb. 2020

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Chen Zhibin, Yu Yang, Bo Haijun, 2020. Geochemical Characteristics and Geological Significance of the Ordovician Volcanic Rock in Ejiana, Inner Mongolia. Earth Science, 45(2): 503-518. doi: 10.3799/dqkx.2018.346

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Chen Zhibin, Yu Yang, Bo Haijun, 2020. Geochemical Characteristics and Geological Significance of the Ordovician Volcanic Rock in Ejiana, Inner Mongolia. Earth Science, 45(2): 503-518. doi: 10.3799/dqkx.2018.346

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Geochemical Characteristics and Geological Significance of the Ordovician Volcanic Rock in Ejiana, Inner Mongolia

doi: 10.3799/dqkx.2018.346

Chen Zhibin^{1
,
,},
Yu Yang^{1
,
,
,},
Bo Haijun²

1.
Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
No.2 Gold Geological Party of CAPF, Huhhot 010010, China

Received Date: 2018-11-02
Publish Date: 2020-02-15

Abstract

Abstract

As the responses to the geological events on the southern margin of Central Asian Orogenic Belt in early Paleozoic, Ordovician volcanic rocks exposed in Ejin Banner, Inner Mongolia, offer important enlightenment for the evolution of Paleo-Asian Ocean. In this paper, the volcanic rocks and tuffs of Xianshuihu group and Baiyunshan group exposed in Hurengbasike area, Ejin Banner, are studied, including their petrology isotope chronology and geochemical characteristics such as major and trace elements. The results show that the lithology combination of Xianshuihu group is a series of basalt-basaltic andesite-andesite-rhyolite, as well as their volcanic lastic rocks, volcanic debris lava, while tuffs in baiyunshan group are mainly acidic. The volcanic rocks and tuffs belong to the sub-alkaline series, mainly showing the trends of calc-alkaline series evolution, and they are characterized by rich calcium and aluminum, poor magnesium, and larger TFeO/MgO ratios. Besides, the volcanic rocks have enriched LILE, LREE and depleted HFSE, with their REE distribution curves inclining to the right. Test results of SHRIMP zircon U-Pb isotope of the rhyolite sample from xianshuihu group yields a concordia age of 462±3 Ma(MSWD=1.6), indicating its formation era of late Ordovician, The tectonic setting of these volcanic rocks are different from the island arc volcanic rocks of Yihatuoli and Xirehada area in the west, belonging to the active continental margin, revealing the subduction of Zoolen Ocean in Mongolia towards the northern margin of Mingshui-Hanshan block during Middle Ordovician.
- volcanic rock,
- SHRIMP,
- chronology,
- Beishan orogen,
- Ejin Banner,
- Inner Mongolia,
- geochemistry

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References(105)

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Geochemical Characteristics and Geological Significance of the Ordovician Volcanic Rock in Ejiana, Inner Mongolia

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