华夏早古生代俯冲作用(Ⅱ)：大爽高镁-镁质安山岩新证据

彭松柏; 刘松峰; 林木森; 吴长峰; 韩庆森

doi:10.3799/dqkx.2016.079

Volume 41 Issue 6

Jun. 2016

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Article Navigation > Earth Science > 2016 > 41(6): 931-947

Peng Songbai, Liu Songfeng, Lin Musen, Wu Changfeng, Han Qingsen, 2016. Early Paleozoic Subduction in Cathaysia (Ⅱ): New Evidence from the Dashuang High Magnesian-Magnesian Andesite. Earth Science, 41(6): 931-947. doi: 10.3799/dqkx.2016.079

Citation:

Peng Songbai, Liu Songfeng, Lin Musen, Wu Changfeng, Han Qingsen, 2016. Early Paleozoic Subduction in Cathaysia (Ⅱ): New Evidence from the Dashuang High Magnesian-Magnesian Andesite. Earth Science, 41(6): 931-947. doi: 10.3799/dqkx.2016.079

Citation:

Peng Songbai, Liu Songfeng, Lin Musen, Wu Changfeng, Han Qingsen, 2016. Early Paleozoic Subduction in Cathaysia (Ⅱ): New Evidence from the Dashuang High Magnesian-Magnesian Andesite. Earth Science, 41(6): 931-947. doi: 10.3799/dqkx.2016.079

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Early Paleozoic Subduction in Cathaysia (Ⅱ): New Evidence from the Dashuang High Magnesian-Magnesian Andesite

doi: 10.3799/dqkx.2016.079

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Center for Global Tectonics, China University of Geosciences, Wuhan 430074, China
3.
College of Zijin Minning, Fuzhou University, Fuzhou 350108, China
4.
The Western Geological Party of Fujian, Xiamen 361000, China

Received Date: 2016-02-23
Publish Date: 2016-06-15

Abstract

Abstract

The nature of early Paleozoic Caledonian orogeny (Guangxi movement), as one of the key geolocial problems of tectonic evolution in South China, has been controversial for a long time. In this study we report a suite of early Paleozoic basaltic andesite-andesite volcanic rocks located at the Dashuang in the Cenxi area of southeastern Guangxi in South China. Petrogeochemical data of the basaltic andesite-andesite show the contents of SiO₂=47.8%-58.8%, Al₂O₃=13.35%-14.25%, CaO=3.79%-5.61% and TiO₂=0.46%-0.56%. It also shows high contents of MgO=4.39%-9.96%, Ni=141×10^-6-210×10^-6 and Cr=427×10^-6-750×10^-6, indicating that they belong to high magnesian (HM)-magnesian (M) basaltic andesite-andesite from calc-alkaline to transitional series. The volcanic rocks exhibit enriched-LREE, weak negative δEu abnormally (0.73-0.92), (La/Yb)_N=3.4-7.9, (La/Sm)_N=3.15-4.95. Basaltic andesite-andesite is characterized by pronounced enrichment of LILEs (e.g. Rb, Ba, Th, U, K, Pb), relative depletion of HFSEs (e.g. Nb, Ta, Ti), and low Ti/V=14.7-21.8. All these show typical characteristics of high magnesian (HM)-magnesian (M) basaltic andesite-andesite (sanukite). The LA-ICP-MS zircon U-Pb age of the magnesian andesite is 443±4 Ma, showing that the formation ages of the volcanic rock series should be between the Late Ordovician and Early Silurian epoch. In conclusion, we suggest that the Dashuang volcanic rocks are the suite of high magnesian (HM)-magnesian (M) basaltic andesite-andesite series formed in the forearc tectonic environment in Late Ordovician-Early Silurian epoch, which provides key evidence for Early Paleozoic oceanic crust subduction between Yangtze Craton and Cathaysia block along Qinzhou-Hangzhou tectonic suture belt in South China.
- Cenxi area,
- high magnesian-magnesian andesite (sanukite),
- petrology,
- geochemistry,
- Early Paleozoic subduction,
- tectonic

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References(118)

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Early Paleozoic Subduction in Cathaysia (Ⅱ): New Evidence from the Dashuang High Magnesian-Magnesian Andesite

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