ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979

HomeAbout UsEditorialAuthorGuide DownloadContentsB B SChinese

黑色页岩的 Re－Os 同位素定年

关键词:Re－Os isotope method dating black shales

基金项目:国家自然科学基金项目（编号：40372059）资助

作者	单位	E-mail
杨競红	南京大学地球科学系成矿作用国家重点实验室南京大学海洋地球化学研究中心，江苏南京，210093	yangjh@icpms.nju.edu.cn
蒋少涌	南京大学地球科学系成矿作用国家重点实验室南京大学海洋地球化学研究中心，江苏南京，210093
凌洪飞	南京大学地球科学系成矿作用国家重点实验室南京大学海洋地球化学研究中心，江苏南京，210093
陈永权	南京大学地球科学系成矿作用国家重点实验室南京大学海洋地球化学研究中心，江苏南京，210093
冯洪真	南京大学地球科学系成矿作用国家重点实验室南京大学海洋地球化学研究中心，江苏南京，210093

摘要点击次数: 2916

全文下载次数: 2789

摘要:

Re－Os Isotope Dating of Black Shales

As one of the recently-developed new geochemical techniques,the Re-Osisotope system can not only serve the precise dating but also provide information on environmental changes, The organism-rich black shales are very suitable for Re-Os dating,and hence precise ages can be obtained. In South China, several periods of oceanic anoxic events occurred from Neoproterozoic to Cambrian,resulting in the deposition of huge theickness of black shales. Using the Re-Os isotope method,we can not only estimate the time of such events, but also effectively trace the paleo-oceanic environment. The results obtained by the authors show that the black shales of Lower Cambrian Niutitang Formation yield a Re-Os isochron age of 537±10Ma.

YANG Jinghong,JIANG Shaoyong,LING Hongfei,CHEN Yongquan,FENG Hongzhen.2005.Re－Os Isotope Dating of Black Shales[J].Acta Geoscientica Sinica,26(z1):180-181.

查看全文查看/发表评论下载PDF阅读器