%0 Journal Article
%T Homogenization temperature and its significance for primary fluid inclusion in halite formed in Chaka salt lake, Qardam basin<br>内陆盐湖石盐流体包裹体均—温度指示意义的现代过程研究
%A LIU XingQi
%A NI Pei
%A DONG HaiLiang
%A WANG TianGang
%A <br>刘兴起
%A 倪培
%A 董海良
%A 王天刚
%J 中国科技期刊研究
%D 2007
%I 
%X Halite precipitation with water and air temperature was observed in detail, and homogenization temperature of fluid inclusions in halite formed in ancient and modem Chaka Salt Lake was studied. Halite precipitates mainly in August every year and largely precipitates between 13 and 15pm at one day when water temperatures reach 20℃ but can seldom reach 30℃. Homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake range from 14℃ to 38℃ with an average of 23.7℃. The number of inclusions appears an obvious peak value at homogenization temperatures between 18 - 25℃, which probably represent the water temperature in which halite mainly precipitates when water temperatures reach 20℃. Therefore, homogenization temperatures of fluid inclusions in halite formed in Chaka Salt Lake can wall reflect the water temperature.
%K Chaka Salt Lake
%K Fluid inclusion in halite
%K Homogenization temperature
%K Forming condition<br>内陆盐湖
%K 石盐流体包裹体
%K 均—温度
%K 指示意义
%K 现代过程
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=B5EDD921F3D863E289B22F36E70174A7007B5F5E43D63598017D41BB67247657&cid=B47B31F6349F979B&jid=5375BC8CB1300555FBA7BEFA534FF15F&aid=F0DD9B70527BE068BD8B0A29B2490FFC&yid=A732AF04DDA03BB3&vid=EA389574707BDED3&iid=CA4FD0336C81A37A&sid=A63576421B012172&eid=8477411EEDB08A86&journal_id=1001-7143&journal_name=中国科技期刊研究&referenced_num=0&reference_num=0