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Sedimentary environment of Late Carboniferous Tangjiatun Formation in Acheng of Heilongjiang
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作者 WANG Fukui WU Jianan +3 位作者 LV Shicong ZHAO Dalin QU Xiyu WANG Dehai 《Global Geology》 2014年第4期206-211,共6页
According to the lithological assemblages and elemental geochemistry of the measured profile,the authors studied the sedimentary and tectonic environment of the Late Carboniferous Tangjiatun Formation in Acheng. The r... According to the lithological assemblages and elemental geochemistry of the measured profile,the authors studied the sedimentary and tectonic environment of the Late Carboniferous Tangjiatun Formation in Acheng. The results show that the trace elements of mudstone samples from Tangjiatun Formation have the characteristics of high Th,V and Cu,but low Ba,Nb and Sr. The rare earth elements are characterized by significantly light and heavy rare earth elements differentiation,relative enrichment of light rare earth elements,and a negative anomaly of δEu. The Tangjiatun Formation belongs to a marine and delta sedimentary environment,and its tectonic setting is considered as a continental island arc environment. 展开更多
关键词 沉积环境 晚石炭世 黑龙江 重稀土元素 元素地球化学 轻稀土元素 构造环境 微量元素
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