Ordovician Seawater Composition:Evidence from Fluid Inclusions in Halite  

作　　者：MENG Fanwei ZHANG Yongsheng Galamy A.R. XING Enyuan NI Pei JI Limin 

机构地区：[1]State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences [2]Guangzhou Institute of Geochemistry, Chinese Academy of Sciences [3]Chinese Academy of Geological Sciences [4]Institute of Geology and Geochemistry of Combustible Minerals,NAS of Ukraine [5]State Key Laboratory for Mineral Deposits Research, Institute of Geo-Fluid Research, Department of Earth Science,Nanjing University [6]Lanzhou Institute of Geology, Chinese Academy of Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2014年第S1期23-23,共1页地质学报（英文版）

基　　金：supported by Major State Basic Research Development Program(973 Program,no. 2011CB403000);National Natural Science Foundation of China (Nos: 40703018; 41173051; 41172131)

摘　　要：Fluid inclusions in halite can directly record the major composition of seawater,however Ordovician halite is very rare.Ordovician is a key time during the evolution history.However there are no Ordovician seawater data reported except from the data from the halite from theFluid inclusions in halite can directly record the major composition of seawater,however Ordovician halite is very rare.Ordovician is a key time during the evolution history.However there are no Ordovician seawater data reported except from the data from the halite from the

关 键 词：ORDOVICIAN seawater composition fluid inclusion HALITE 

分 类 号：P619.211[天文地球—矿床学] P534.42[天文地球—地质学]