《Table 3 Rare earth elements of different dolomite fabrics for Dengying Fm.in the study area (2)》

《Table 3 Rare earth elements of different dolomite fabrics for Dengying Fm.in the study area (2)》   提示：宽带有限、当前游客访问压缩模式
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《"A Model of Hydrothermal Dolomite Reservoir Facies in Precambrian Dolomite, Central Sichuan Basin, SW China and its Geochemical Characteristics"》


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Generally，the concentration of trace elements in sedimentary fluid and diagenetic fluid is the main factor contributing to the trace elements enrichment in rocks.As previous reports，the diagenetic fluid that affected the micritic dolomite in the Dengying Formation is normal or evaporated seawater.On the contrary，formation of saddle dolomite is attributed to the hydrothermal fluid which comes from deep-burial storage.This difference is directly reflected in the Fe and Mn concentrations of the two different fabrics dolomite mentioned above（Fig.7a）（Table 1） .

图表编号XD0030681700    严禁用于非法目的
绘制时间2019.02.01
作者GU Yifan、ZHOU Lu、JIANG Yuqiang、JIANG Chan、LUO Mingsheng、ZHU Xun
绘制单位School of Geosciences & Technology, Southwest Petroleum University、School of Geosciences & Technology, Southwest Petroleum University、School of Geosciences & Technology, Southwest Petroleum University、Exploration Division, PetroChina Southwest Oil & Gas F
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