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Characteristics and Geologic Implication of Fluid Inclusions of Carboniferous Huanglong Formation in well Paishen 1, Jianghan Plain
详细信息   
摘要

The Jianghan Plain is one of the under-explored regions in southern China. Fracture (vug) fillings and aplite dolomites in cores of Huanglong Formation in well Paishen 1 of the study area were analyzed systematically using polarizing microscope, fluorescence microscope and cooling-and-heating bench. Based on homogenization temperature distribution and the mineral types of host as well as the time of various veins(vugs), the inclusions were divided into 5 phases corresponding to homogenization temperature intervals 74.7~86.4, 94.6~106.5, 111.1~131.8, 141.3~152.9 and 158~162.6 ℃, respectively. Combined with the studies of burial and thermal histories, it was concluded that inclusions were formed from the late Triassic to Cretaceous, and were influenced by stages of tectonic movement.

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