%0 Journal Article
%T Homogenization temperature of fluid inclusions in laboratory grown halite and its implication for paleotemperature reconstruction.<br>实验室合成石盐包裹体的均一温度以及古气候意义
%A MENG FanWei
%A NI Pei
%A GE ChenDong
%A WANG TianGang
%A WANG GuoGuang
%A LIU JiQiang
%A ZHAO Chao
%A <br>孟凡巍
%A 倪培
%A 葛晨东
%A 王天刚
%A 王国光
%A 刘吉强
%A 赵超
%J 岩石学报
%D 2011
%I 
%X Halite is a major evaporate mineral in the surface environment,and it contains abundant fluid inclusions formed during crystal formation,which can record the brine temperatures of crystal growth in ancient oceanic salt ponds and salt lakes in geological history.Using the cooling nucleation method,homogenization temperature of fluid inclusions in halite can be measured.However,the interpretation and application of the homogenization temperature in palaeotemperature reconstruction is not straightforward.Fluid...
%K Halite
%K Fluid inclusion
%K Cooling nucleation method
%K Maximum homogenization temperature<br>石盐
%K 流体包裹体
%K 低温冷冻测温法
%K 最大均一温度
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=6DE5BEF27B522E6E2B32CB1003663B9C&yid=9377ED8094509821&vid=DB817633AA4F79B9&iid=94C357A881DFC066&sid=815F249353800F81&eid=D9E4B4338A9AF29A&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=28