The dating and temperature measurement technologies for carbonate minerals and their application in hydrocarbon accumulation research in the paleo-uplift in central Sichuan Basin, SW China
SHEN Anjiang,ZHAO Wenzhi,HU Anping,WANG Hui,LIANG Feng,WANG Yongsheng
Fig. 3. Characteristics of inclusions in dolomite and quartz crystals of Dengying Formation in Central Sichuan paleo-uplift. (a) Well Moxi 22, Deng 2 Member, 5418.70 m; gas-liquid two-phase brine inclusions in foliated dolomite cement; (b) Well Gaoshi 6, Deng 2 Member, 5363.04 m; liquid hydrocarbon inclusions in fine-medium crystalline dolomite cement, colorless-light yellow; (c) Well Moxi 22, Deng 2 Member, 5418.70 m; liquid hydrocarbon inclusions in fine-medium crystalline dolomite cement, light yellow; (d) Well Moxi 22, Deng 2 Member, 5418.70 m; hydrocarbon inclusions in fine-medium crystalline dolomite cement, yellow green fluorescence under ultraviolet light; (e) Well Moxi 9, Deng 2 Member, 5422.10 m; liquid hydrocarbon inclusions in coarse crystalline dolomite cement, light yellow; (f) Well Moxi 9, Deng 2 Member, 5422.10 m; hydrocarbon inclusions in coarse crystalline dolomite, light yellow, and yellow green fluorescence under ultraviolet light; (g) Well Gaoshi 1, Deng 4 Member, 4985.00 m; gas-liquid two-phase hydrocarbon inclusions in saddle-shaped dolomite cement, black; (h) Well Moxi 9, Deng 2 Member, 5422.10 m; gaseous hydrocarbon inclusions in saddle-shaped dolomite cement, black; (i) Well Moxi 9, Deng 2 Member, 5422.10 m; gaseous hydrocarbon inclusions in quartz crystal, black.