The Distribution and Composition Characteristics of Siliceous Rocks from Qinzhou Bay-Hangzhou Bay Joint Belt, South China: Constraint on the Tectonic Evolution of Plates in South China
Li, Hongzhong1,2; Zhai, Mingguo1; Zhang, Lianchang1; Zhou, Yongzhang2,3; Yang, Zhijun2,3; He, Junguo2,3; Liang, Jin2,3; Zhou, Liuyu2,3
刊名SCIENTIFIC WORLD JOURNAL
2013
ISSN号1537-744X
DOI10.1155/2013/949603
文献子类Article
英文摘要The Qinzhou Bay-Hangzhou Bay joint belt is a significant tectonic zone between the Yangtze and Cathaysian plates, where plentiful hydrothermal siliceous rocks are generated. Here, the authors studied the distribution of the siliceous rocks in the whole tectonic zone, which indicated that the tensional setting was facilitating the development of siliceous rocks of hydrothermal genesis. According to the geochemical characteristics, the Neopalaeozoic siliceous rocks in the north segment of the Qinzhou Bay-Hangzhou Bay joint belt denoted its limited width. In comparison, the Neopalaeozoic Qinzhou Bay-Hangzhou Bay joint belt was diverse for its ocean basin in the different segments and possibly had subduction only in the south segment. The ocean basin of the north and middle segments was limited in its width without subduction and possibly existed as a rift trough that was unable to resist the terrigenous input. In the north segment of the Qinzhou Bay-Hangzhou Bay joint belt, the strata of hydrothermal siliceous rocks in Dongxiang copper-polymetallic ore deposit exhibited alternative cycles with the marine volcanic rocks, volcanic tuff, and metal sulphide. These sedimentary systems were formed in different circumstances, whose alternative cycles indicated the release of internal energy in several cycles gradually from strong to weak.
WOS关键词EAST PACIFIC RISE ; RARE-EARTH ; GEOCHEMICAL CHARACTERISTICS ; GEOLOGICAL CHARACTERISTICS ; DEPOSITIONAL-ENVIRONMENTS ; SULFIDE DEPOSITS ; CHERT ; SEDIMENTS ; PROVENANCE ; CALIFORNIA
WOS研究方向Science & Technology - Other Topics
语种英语
出版者HINDAWI PUBLISHING CORPORATION
WOS记录号WOS:000327179400001
资助机构Natural Science Foundation of China(41303025 ; Natural Science Foundation of China(41303025 ; 973 Program of China(2012CB406601) ; 973 Program of China(2012CB406601) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; 41373025 ; 41373025 ; 41273040) ; 41273040) ; Natural Science Foundation of China(41303025 ; Natural Science Foundation of China(41303025 ; 973 Program of China(2012CB406601) ; 973 Program of China(2012CB406601) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; 41373025 ; 41373025 ; 41273040) ; 41273040) ; Natural Science Foundation of China(41303025 ; Natural Science Foundation of China(41303025 ; 973 Program of China(2012CB406601) ; 973 Program of China(2012CB406601) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; 41373025 ; 41373025 ; 41273040) ; 41273040) ; Natural Science Foundation of China(41303025 ; Natural Science Foundation of China(41303025 ; 973 Program of China(2012CB406601) ; 973 Program of China(2012CB406601) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Subject and Special Fund of the Ministry of Science and Technology of The State Key Laboratory of Geological Processes and Mineral Resources(GPMR200804) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; Guangdong Provincial Natural Science Foundation(S2013010012528) ; 41373025 ; 41373025 ; 41273040) ; 41273040)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/87099]  
专题中国科学院地质与地球物理研究所
通讯作者Li, Hongzhong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resource, Beijing 100029, Peoples R China
2.Guangdong Prov Key Lab Geol Proc & Mineral Resour, Guangzhou 510275, Guangdong, Peoples R China
3.Sun Yat Sen Univ, Dept Earth Sci, Guangzhou 510275, Guangdong, Peoples R China
推荐引用方式
GB/T 7714
Li, Hongzhong,Zhai, Mingguo,Zhang, Lianchang,et al. The Distribution and Composition Characteristics of Siliceous Rocks from Qinzhou Bay-Hangzhou Bay Joint Belt, South China: Constraint on the Tectonic Evolution of Plates in South China[J]. SCIENTIFIC WORLD JOURNAL,2013.
APA Li, Hongzhong.,Zhai, Mingguo.,Zhang, Lianchang.,Zhou, Yongzhang.,Yang, Zhijun.,...&Zhou, Liuyu.(2013).The Distribution and Composition Characteristics of Siliceous Rocks from Qinzhou Bay-Hangzhou Bay Joint Belt, South China: Constraint on the Tectonic Evolution of Plates in South China.SCIENTIFIC WORLD JOURNAL.
MLA Li, Hongzhong,et al."The Distribution and Composition Characteristics of Siliceous Rocks from Qinzhou Bay-Hangzhou Bay Joint Belt, South China: Constraint on the Tectonic Evolution of Plates in South China".SCIENTIFIC WORLD JOURNAL (2013).
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