Chunlei Jing, Yanpeng Zheng, Baohua Liu, Yingchun Cui
{"title":"海底热液硫化物矿床分布规律及控制因素:海底热液硫化物矿床分布规律及控制因素","authors":"Chunlei Jing, Yanpeng Zheng, Baohua Liu, Yingchun Cui","doi":"10.3724/SP.J.1140.2013.01057","DOIUrl":null,"url":null,"abstract":"The latest data on global hydrothermal vent sites are used in this paper to discuss the tectonic settings of submarine polymetallic sulfide deposits and other ore-controlling factors,such as the deep magmatic activity,fault structure and sediment cap.Results show that the submarine hydrothermal polymetallic sulfide vent sites are mainly located at the divergent and convergent plate boundaries;the deep magmatic activity and the fault structures are the most important factors controlling the distribution of the hydrothermal polymetallic sulfide on mid-ocean ridges;and the speed of sea floor spreading contributes to the size of polymetallic sulfide deposits.Conclusions of this study could be used as the reference in the exploration of submarine hydrothermal polymetallic resources.","PeriodicalId":18188,"journal":{"name":"海洋地质与第四纪地质","volume":"33 1","pages":"57-64"},"PeriodicalIF":0.0000,"publicationDate":"2014-03-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"DISTRIBUTION PATTERN OF SUBMARINE HYDROTHERMAL SULFIDE DEPOSITS AND CONTROLLING FACTORS: DISTRIBUTION PATTERN OF SUBMARINE HYDROTHERMAL SULFIDE DEPOSITS AND CONTROLLING FACTORS\",\"authors\":\"Chunlei Jing, Yanpeng Zheng, Baohua Liu, Yingchun Cui\",\"doi\":\"10.3724/SP.J.1140.2013.01057\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The latest data on global hydrothermal vent sites are used in this paper to discuss the tectonic settings of submarine polymetallic sulfide deposits and other ore-controlling factors,such as the deep magmatic activity,fault structure and sediment cap.Results show that the submarine hydrothermal polymetallic sulfide vent sites are mainly located at the divergent and convergent plate boundaries;the deep magmatic activity and the fault structures are the most important factors controlling the distribution of the hydrothermal polymetallic sulfide on mid-ocean ridges;and the speed of sea floor spreading contributes to the size of polymetallic sulfide deposits.Conclusions of this study could be used as the reference in the exploration of submarine hydrothermal polymetallic resources.\",\"PeriodicalId\":18188,\"journal\":{\"name\":\"海洋地质与第四纪地质\",\"volume\":\"33 1\",\"pages\":\"57-64\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2014-03-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"海洋地质与第四纪地质\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.3724/SP.J.1140.2013.01057\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"海洋地质与第四纪地质","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.3724/SP.J.1140.2013.01057","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
DISTRIBUTION PATTERN OF SUBMARINE HYDROTHERMAL SULFIDE DEPOSITS AND CONTROLLING FACTORS: DISTRIBUTION PATTERN OF SUBMARINE HYDROTHERMAL SULFIDE DEPOSITS AND CONTROLLING FACTORS
The latest data on global hydrothermal vent sites are used in this paper to discuss the tectonic settings of submarine polymetallic sulfide deposits and other ore-controlling factors,such as the deep magmatic activity,fault structure and sediment cap.Results show that the submarine hydrothermal polymetallic sulfide vent sites are mainly located at the divergent and convergent plate boundaries;the deep magmatic activity and the fault structures are the most important factors controlling the distribution of the hydrothermal polymetallic sulfide on mid-ocean ridges;and the speed of sea floor spreading contributes to the size of polymetallic sulfide deposits.Conclusions of this study could be used as the reference in the exploration of submarine hydrothermal polymetallic resources.
期刊介绍：
Marine Geology and Quaternary Geology launched in 1981 is a bimonthly academic journal sponsored by Qingdao Institute of Marine Geology, China Geological Survey, and published by the Science Press, China.The journal aims to publish original, cutting-edge, and explorative scientific results in the field of marine geology and sea-land Quaternary geology. The journal focus on reporting the latest research achievements supported by National Natural Science Foundation Project, National Key Project and International Cooperation Project, with priority to the results in China seas, global ocean and three poles, and the comparative study results between offshore and land, regional and global scientific issues.
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