华南晚奥陶世次火山岩的发现：早古生代与俯冲有关的英安岩?

易立文; 马昌前; 王连训; 赖中信; 李湘玉; 杨亚楠; 吴飞; 胡晏如

doi:10.3799/dqkx.2014.061

Volume 39 Issue 6

Jun. 2014

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Article Navigation > Earth Science > 2014 > 39(6): 637-653

Yi Liwen, Ma Changqian, Wang Lianxun, Lai Zhongxin, Li Xiangyu, Yang Ya'nan, Wu Fei, Hu Yanru, 2014. Discovery of Late Ordovician Subvolcanic Rocks in South China: Existence of Subduction-Related Dacite from Early Paleozoic?. Earth Science, 39(6): 637-653. doi: 10.3799/dqkx.2014.061

Citation:

Yi Liwen, Ma Changqian, Wang Lianxun, Lai Zhongxin, Li Xiangyu, Yang Ya'nan, Wu Fei, Hu Yanru, 2014. Discovery of Late Ordovician Subvolcanic Rocks in South China: Existence of Subduction-Related Dacite from Early Paleozoic?. Earth Science, 39(6): 637-653. doi: 10.3799/dqkx.2014.061

Citation:

Yi Liwen, Ma Changqian, Wang Lianxun, Lai Zhongxin, Li Xiangyu, Yang Ya'nan, Wu Fei, Hu Yanru, 2014. Discovery of Late Ordovician Subvolcanic Rocks in South China: Existence of Subduction-Related Dacite from Early Paleozoic?. Earth Science, 39(6): 637-653. doi: 10.3799/dqkx.2014.061

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Discovery of Late Ordovician Subvolcanic Rocks in South China: Existence of Subduction-Related Dacite from Early Paleozoic?

doi: 10.3799/dqkx.2014.061

Yi Liwen^{1, 2
,},
Ma Changqian^{1
,
,},
Wang Lianxun^{1, 3},
Lai Zhongxin⁴,
Li Xiangyu⁵,
Yang Ya'nan¹,
Wu Fei¹,
Hu Yanru¹

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
School of Geosciences and Info-Physics, Central South University, Changsha 410083, China
3.
Geological Institute, University of Tübingen, Tübingen 72076, Germany
4.
293 Brigade, Guangdong Province Nuclear Industry Geological Bureau, Guangzhou 510800, China
5.
Hunan Institute of Geological Survey, Changsha 410116, China

Received Date: 2013-11-01
Publish Date: 2014-06-15

Abstract

Abstract

Though Early Paleozoic granites are widely distributed in South China, contemporary volcanic and subvolcanic rocks are rare. This study analyzed dacites from Hekou and Shangdong in Northern Guangdong Province, using detailed LA-ICPMS zircon U-Pb geochronology and Sr-Nd-Hf isotopic geochemistry. The results show that the dacite was formed in 448.7±1.7 Ma, and associated with Late Ordovician volcanism. These rocks are generally porphyritic with prophyroclastic or embayed quartz. The matrixes are normally cryptocrystalline. These features fit well with typical subvolcanic rocks. Geochemically, the dacite is high-K calc-alkaline series. They are enriched in LREE, depleted with Ta, Nb and are extremely low in Cr, Ni contents. Isotopic data show that they have I_Sr=0.709 0-0.714 0, ε_Nd(t)=-8.9 to -9.3, ε_Hf(t)=-8.06 to -3.80, consistent with the isotopic compositions of the Caledonian granitoids in South China. The model ages of two stages based on zircon Hf isotopes range from 1.67 Ga to 1.93 Ga, consistent with the whole rock Nd dating (1.91-1.94 Ga), implying that the dacite might have originated from the Paleoproterozoic crustal materials. This new finding of Hekou and Shangdong Ordovician dacite confirms the existence of Early Paleozoic subduction magmatism in this area.
- South China,
- dacite,
- zircon U-Pb geochronology,
- isotopes,
- Caledonian,
- geochemistry

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References(126)

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