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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2006-03
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The relativity between volcano activity and distribution of the bivalve-community in Late Triassic in Changtai,Western Sichuan,China

PANG Yan-chun,LIN Li,ZHU Li-dong, WANG Xin-li,MA Ye-qingInstitute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China  
Volcano activity took place frequently in Late Triassic in the Changtai area of Western Sichuan.After every volcano activity,a suit of fuscous sediments also appeared,including black limy slate,argillite,silt shale.Many bivalve-fossils were buried in the suit of sediments.The most abundant fossils were buried in the bottom of the suit of sediments,imbedded in the rocks with shell form and mineralized evidently.Based on the characters of the rock slices and geochemistry-analysis,a conclusion is made,that is the volcano activity was related to the community closely.The volcano activity offered a channel way for the benthic hydrothermal activity in Late Triassic in the Changtai area of Western Sichuan.In this term,the variation parameters of the environment including high temperature and high concentration etc.are favorable to the breeding of the bivalve-community.
【Fund】: 国家自然科学基金(40472013);; 教育部跨世纪优秀从才基金;; 四川省青年科技基金;; 四川省学术技术后备人选基金资助项目
【CateGory Index】: Q915
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