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陆相咸化湖泊沉积中锶/钡比值及其地质意义
引用本文:彭立才,韩德馨,濮人龙,高嵩.陆相咸化湖泊沉积中锶/钡比值及其地质意义[J].中国矿业大学学报,1999,28(1):50-52.
作者姓名:彭立才  韩德馨  濮人龙  高嵩
作者单位:1. 中国矿业大学资源开发工程系,北京,100083
2. 青海石油管理局,敦煌,736200
摘    要:陆相咸化湖泊水体与同矿化度的海水相比,大部分具有较高的ρ(SO42-).陆相咸化湖泊沉积物同海洋沉积物中的w(Sr)/w(Ba)比值相似.w(Sr)/w(Ba)比值在沉积物中没有碳酸岩盐存在时,可以作为古盐度标志,但作为海陆相沉积区分标志是不全面的,它不能区分海洋和陆相咸化湖泊沉积物.

关 键 词:陆相咸化湖泊,锶/钡比值,海相沉积,陆相沉积
修稿时间:1998-05-29

w(Sr)/w(Ba) Value of Continental Brackish Lake Deposit and Its Geological Significance
Peng Licai,Han Dexin,Pu Renlong,Gao Song.w(Sr)/w(Ba) Value of Continental Brackish Lake Deposit and Its Geological Significance[J].Journal of China University of Mining & Technology,1999,28(1):50-52.
Authors:Peng Licai  Han Dexin  Pu Renlong  Gao Song
Abstract:Being compared with the sea water of the same mineralization intensity, most of continental brackish waters show high values of w (SO 2- 4). While w (Sr)/ w (Ba) values of both continental brackish lake deposit and marine deposit are very alike. w (Sr)/ w (Ba) value can be used as a criterion of palaeosalinity without carbonate in the deposit. But when it is used as the criterion of discriminating continental deposit from the marine one, it is not correct.
Keywords:continental brackish lake    w  (Sr)/  w  (Ba) value    marine deposit  continental deposit
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