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《Geotectonica Et Metallogenia》 2006-01
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GEOCHEMISTRY AND PETROGENESIS OF CENOZOIC VOLCANIC ROCKS FROM SANSHUI BASIN: IMPLICATIONS FOR SPATIAL AND TEMPORAL VARIATION OF ROCK TYPES AND CONSTRAINTS ON THE FORMATION OF SOUTH CHINA SEA

XIAO Long 1,2,3, ZHOU Haiming4, DONG Yuexia5, ZENG Guangce2 and WANG Fangzheng2(1. Key Laboratory of Marginal Sea Geology, Chinese Academy of Sciences, Guangzhou, GD 510640, China; 2. Faculty of Earth Sciences, China University of Geosciences, Wuhan, HB 430074, China; 3. National Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan, HB 430074, China; 4. Petrochina Jidong Oilfield Company Exploration & Development Research Institute, Tangshan, Hebei 063004, China; 5. PetrocChina Jidong Oilfield Company, Tangshan, Hebei 063004, China)  
Cenozoic volcanic rocks are widely distributed in southeastern China, such as in Sanshui basin, Zhujiangkou basin, Leiqiong Peninsula and Beibuwan Gulf. Volcanic rocks within the Sanshui basin display bimodal characteristics and are composed of basalts and rhyolite/trachyte. Basalts and trachytes have similar distributive patterns of rare earth elements and trace elements, and Nd isotopes (ε Nd(T)=2.34~6.4). These suggest that they were generated from enriched mantle sources. Basalts were storied in deep magma chamber and experienced crystallization of olivine and clinopyroxene, while the felsic rhyolite and trachyte were derived from basalts that were input in shallow magma chambers, then by extensive fractionation of feldspar and apatite from transitional intermediate andesitic magma. Spatially, volcanism are younger and rock types are getting simpler from southeastern toward southern South China Sea, and are dominated by tholeiite and alkaline basalts. Their geochemical and isotopic features and variations in both space and time suggest that they were generated from continuing melting of upwelling asthenosphere mantle, similar to the case with mantle plume. The formation of the South China Sea might be associated with plume activity and resulted from continental rifting process.
【Fund】: 中国科学院边缘海地质重点实验室开放基金项目(MSGLCAS03-6);; 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;; 中国地质大学地质过程与矿产资源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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