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《Geotectonica Et Metallogenia》 2006-01
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SPATIAL DISTRIBUTION AND PETROLOGICAL CHARACTERISTICS OF THE BIMODAL VOLCANIC ROCKS FROM SANSHUI BASIN, GUANGDONG PROVINCE: IMPLICATION FOR BASIN DYNAMICS

DONG Yuexia 1,2, XIAO Long 3,4, ZHOU Haiming5, ZENG Guangce3, WANG Fangzheng3, WANG Xudong2, XIANG Hua3, ZHAO Taiping4 and LIU Xiaoming6(1. Basin & Reservior Research Center, China University of Petrolum, Beijing 102249, China; 2. Petrochina Jidong Oilfield Company Exploration & Development Research Institute, Tangshan, HB 063004, China; 3.Faculty of Earth Sciences, China University of Geosciences, Wuhan, Hubei 430074, China; 4. CAS Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou,GD 510640, China; 5. Petrochina Jidong Oilfield Company, Tangshan, HB 063004, China; 6. Department of Geology, Northwest University, Xi'an, SX 710069, China)  
Late Cretaceous and Cenozoic volcanic rocks are widely distributed within the Sanshui basin, Guangdong province. These volcanic rocks consist of basalts (SiO2=44.45%~54.46%; K2O+Na2O=3%~6%) and trachyte/rhyolites (SiO2=59.23%~73.27%; K2O+Na2O=7.5%~12%), and display bimodal features in chemical composition. They were formed by thirteen-stage eruption. In the earlier stages (from first to third stage) trachyte and rhyolites dominated volcanics that are located at the eastern and western margins were generated, in contrast, at late stages (from fourth to thirteen stages) volcanic basalts were formed and located at the center of the basin. These features suggest significant transition from shallow magma chamber to deep ones, along with stronger and deeper rifting. Both felsic and mafic magmas were sourced from upwelling mantle by decompressed melting and fractional crystallization processes. Active rifting had resulted in eruptions from shallow to deep, while asymmetric extension forces caused more extensive crustal thining in the east side, which may be genetically associated with the formation of Zhujiangkou basin.
【Fund】: 中国石油冀东油田分公司“广东三水盆地火成岩特征研究与油气成藏优选”项目;; 中国科学院边缘海重点实验室开放基金(MSGLCAS3-6);; 中国地质大学GPMR国家重点实验室开放基金(GPMR2002-16)联合资助.
【CateGory Index】: P588.14
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9 Sun Mingliang; Chen Jianfa(Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000) Liao Yongsheng(Shengli Institute of Geology, CNPC, Dongying 257015);HELIUMISOTOPIC CHARACTERISTICS, GENESIS OF CO_2 IN NATURAL GASES AND DISTRIBUTION OF TERTIARY MAGAMATITE IN THE JIYANG DEPRESSION[J];GEOCHIMICA;1996-05
10 ZhuBing.uan ① WangYixian ① WangHuifen ① ChenDaogong ② ChenDuofu ① (① Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640) (②Department of Earth and Space Sciences, China University of Science and Technol;HUANGSHAN-WENZHOU GEOCHEMICAL SECTION AND ITS CORRIDOR AREA OF LITHOSPHERE IN SOUTHEAST CHINA[J];GEOCHIMICA;1997-02
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