Citation: | XIONG Jinhong, LIANG Mingliang, CAO Zhanyuan, WANG Zongxiu, ZHENG Jianjing, WANG Zuodong. THE GEOCHEMICAL AND MINERALOGICAL CHARACTERISTICS OF SHALES IN CHAIWOBU DEPRESSION, SOUTHERN MARGIN OF JUNGGAR BASIN[J]. Journal of Geomechanics, 2017, 23(4): 585-593. |
Using XRD, Rock-eval and GC-MS, kerogen type, organic geochemical characteristics and inorganic mineralogy features of shales in upper Carboniferous, upper Permian, and lower Jurassi from the Chaiwobu depression at southern margin of Junggar Basin were analyzed. The organic geochemical index shows that from Carboniferous to Permian, it has been a long period of fresh-brackish water sedimentary environment in Chaiwobu depression. The sources of organic matter shared the similar source input characteristics, and kerogen type were mainly featured by type Ⅱ. The thermal evolution of organic matter indicates that shales in lower Jurassic were in low mature stage while shales in upper Carboniferous and upper Permian showed the features of high abundance, rich in types and mature-high mature stage in the thermal evolution. The mineralogical characteristics show that the content of brittle minerals feldspar and quartz in upper Permian shales is 73%, followed by clay mineral, indicating a high brittleness index and good property of fracturing and adsorption. Combined with the previous studies, it is predicted that a certain scale of shale gas resources may be contained in shales of this member with a good prospect and potential for exploration.
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Structural unit division and sample collection sites in Chaiwobu Depression
Crossplot of Pr/C17 and Ph/C18 of shale samples
Total ion current of saturated hydrocarbon of shale samples
Characteristics of terpane parameters in source rock
Triangular chart of the distribution of sterane of shale samples
Composition and distribution of the minerals in shales in Carboniferous-Jurassic of the study area