内蒙古哈珠地区石炭纪白山组火山岩:北山北部晚古生代活动陆缘岩浆作用的产物

任云伟; 任邦方; 牛文超; 孙立新; 李敏; 张阔; 张家辉; 段连峰

doi:10.3799/dqkx.2018.261

Volume 44 Issue 1

Jan. 2019

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Article Navigation > Earth Science > 2019 > 44(1): 312-327

Ren Yunwei, Ren Bangfang, Niu Wenchao, Sun Lixin, Li Min, Zhang Kuo, Zhang Jiahui, Duan Lianfeng, 2019. Carboniferous Volcanics from the Baishan Formation in the Hazhu Area, Inner Mongolia: Implications for the Late Paleozoic Active Continental Margin Magmatism in the Northern Beishan. Earth Science, 44(1): 312-327. doi: 10.3799/dqkx.2018.261

Citation:

Ren Yunwei, Ren Bangfang, Niu Wenchao, Sun Lixin, Li Min, Zhang Kuo, Zhang Jiahui, Duan Lianfeng, 2019. Carboniferous Volcanics from the Baishan Formation in the Hazhu Area, Inner Mongolia: Implications for the Late Paleozoic Active Continental Margin Magmatism in the Northern Beishan. Earth Science, 44(1): 312-327. doi: 10.3799/dqkx.2018.261

Citation:

Ren Yunwei, Ren Bangfang, Niu Wenchao, Sun Lixin, Li Min, Zhang Kuo, Zhang Jiahui, Duan Lianfeng, 2019. Carboniferous Volcanics from the Baishan Formation in the Hazhu Area, Inner Mongolia: Implications for the Late Paleozoic Active Continental Margin Magmatism in the Northern Beishan. Earth Science, 44(1): 312-327. doi: 10.3799/dqkx.2018.261

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Carboniferous Volcanics from the Baishan Formation in the Hazhu Area, Inner Mongolia: Implications for the Late Paleozoic Active Continental Margin Magmatism in the Northern Beishan

doi: 10.3799/dqkx.2018.261

Tianjin Center of China Geological Survey, Tianjin 300170, China

Received Date: 2018-04-27
Publish Date: 2019-01-15

Abstract

Abstract

The character of Late Paleozoic magmatic events has great significance for the study of tectonic evolution in the northern Beishan. A systematic study of geochemistry, geochronology and Lu-Hf isotopes is made on Baishan Formation volcanic rocks in the Beishan Hazhu area of Inner Mongolia. The results show that Baishan Formation volcanic rocks are composed of basaltic andesite, andesite, dacitic and rhyolitic volcanic rocks. The diagenetic ages of andesite, dacite and rhyolite from the LA-ICP-MS zircon U-Pb dating are 325.6±1.4 Ma, 313.5±3.4 Ma and 314.7±1.7 Ma respectively, all which belong to the later period of Early Carboniferous epoch-medium period of Late Carboniferous epoch. Geochemical studies show that the Baishan Formation volcanic rocks are characterized by apparent "component polarity feature" in spatial distribution, displaying regional north-to-south evolution from intermediate volcanic rocks (calc-alkaline series) to acid volcanic rocks (high-K calc-alkaline series), with the increased content of K₂O and ratio of K₂O/Na₂O, in which basaltic andesite and andesite belong to higher content of Al₂O₃, lower content of TiO₂ and lower content of Ni and Cr. Additionally, microelements of all volcanic samples generally show depletion of high field strength elements such as Nb, Ta, P, Ti and apparent right-leaning distribution patterns of the REE with depletion in LREE and enrichment in HREE. The above characteristics suggest that the Baishan Formation volcanic rocks are formed from active continental margin arc in the process of southern subduction oceanic crust. Additionally, andesite in the Baishan Formation is characterized by higher value of ε_Hf(t) (7.0-14.1)and the young average crustal model age T_DM^C (437-891 Ma), Rb/Sr ratio (0.01-0.15) near the upper mantle and Nb/Ta ration (12.59-18.80) between mean values of crust and mantle; rhyolite is characterized by later value of ε_Hf(t) (4.3-8.2) and the older average crustal model age T_DM^C (804-1 054 Ma), Rb/Sr ratio (0.80-1.73) that is much larger than the mean values of crust and Nb/Ta ration (10.66-13.08) near the mean values of crust, which all indicate that magma source region was mainly new crust and mantle material near the ocean side and it was evolved gradually into the increasing of more continental crust (older crust) material close to the inland side. Based on the above analysis and combined with the previous data, it is concluded that Beishan Hazhu area Late Paleozoic Carboniferous Baishan Formation volcanic rocks were formed in the subduction process of Hong Shishan Ocean into the south side of micro plot of Mazong Mountain-Han Mountain, and it had been resulted from magmatism of the active continental margin.
- Beishan orogenic belt,
- Baishan Formation,
- geochemistry,
- zircon U-Pb age,
- petrogenesis,
- Hazhu area

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Carboniferous Volcanics from the Baishan Formation in the Hazhu Area, Inner Mongolia: Implications for the Late Paleozoic Active Continental Margin Magmatism in the Northern Beishan

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