摘要
渝东南及周边地区下寒武统黑色岩系稀土总量略低于北美页岩,∑LREE/∑HREE值为1.99~9.01,平均6.86,轻稀土相对富集;δEu值为0.69~7.33,平均2.79;δCe值为0.70~1.01,平均0.85。区内下寒武统黑色岩系为正常海水与热水沉积作用的混合产物,形成于缺氧还原环境逐渐向弱氧化环境过渡的外陆架。
The Lower Cambrian black rock series in southeastern Chongqing and its adjacent areas are characterized by less-enriched ΣREE,ΣLREE/ΣHREE ratios ranging between 1.99 and 9.01 with an average of 6.86,relatively Enriched LREE,δEu values ranging between 0.69 and 7.33 with an average of 2.79,and δCe values ranging between 0.70 and 1.01 with an average of 0.85.The results of research in the present paper show that the Lower Cambrian black rock series in the study area resulted from the mixing of the normal seawater and hot seawater deposition in the transitional conditions from the anoxic reducing environments to the weakly oxidized environments on the outer continental shelves.
出处
《沉积与特提斯地质》
CAS
CSCD
2011年第2期49-54,共6页
Sedimentary Geology and Tethyan Geology
基金
中国地质调查局<雪峰山西侧地区海相油气地质调查>项目资[2007]035-05资助
关键词
渝东南
黑色岩系
稀土元素
沉积环境
southeastern Chongqing
black rock series
REE
sedimentary environment