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《Acta Sedimentologica Sinica》 2010-04
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Paleolake Evolution of Eocene in Fushun Basin

LIU Rong1,2 LIU Zhao-jun1,2 MENG Qing-tao1 SUN Ping-chang1ZHOU Ren-jie1 LIU Dong-qing1 YANG Dong1(1.College of Earth Sciences,Jilin University,Changchun 130061;2.Key-Lab for Evolution of Past Life and Environment in Northeast Asia,Ministry of Education,China,Changchun 130026)  
In order to interpret continental responses to globally climatic cooling in the Eocene-Oligocene,we have studied the paleolake features of Fushun Basin,an Eocene fault-depression basin in NE China,through measuring actual strata profiles in the fields and indoor sample testing.The analysis of rock facies,facies indicators and rock thinsections suggests the evolution history of sedimentary facies in Eocene,Fushun Basin.Sedimentary subfacies vary as: lake and marshland-shallow lacustrine-half deep lacustrine-deep lacustrine-half deep lacustrine-shallow lacustrine,with the water depth varying as: shallow-deep-shallow.On the basis of contents of trace elements(B,Mn,Ti,Co,Cr,Ni,V),element contents ratios(Sr/Ba,V/(V + Ni),Ni/ Co,ωFe2O3 /ωFeO) and ratios of oxides,we point out that there was an abrupt climatic change from early Eocene to late Eocene in Fushun Basin.In the early Eocene,climate was moisture and good for coral forming.While,in the middle-late Eocene,climate changed into drier and made contribution into the interbedding between marlite forming in saline and half-saline water and clay shale.In general,our study shows that the climate changed from moisture to dry in Eocene-Oligocene.
【Fund】: 高等学校博士学科点专项科研基金(新教师基金课题)(编号:200801831098);; 国家自然科学基金(批准号:40972076);; 吉林省科技发展计划(青年科研基金)(编号:20090167);; 国土资源部公益性行业科研专项(编号:200811013);国土资源部"十一五"重大科技创新项目(编号:20080106-1);; 国家科技重大专项(编号:2008ZX05018-001-004)联合资助
【CateGory Index】: P532
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