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Gas generation characteristics of the lower cambrian niutitang shale in qiannan depression, China

机译:中国黔南坳陷下寒武纪NIUTITANG页岩的气体生成特征

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摘要

Based on the thermal simulation experiments of shale and crude oil samples, the amount of gas generated from kerogen and oil cracking during each geological period was calculated based on the chemical kinetic method. The results showed that the total amount of gas generated from the Niutitang Shale in Hy1 well is 49.00 m(3)/t, including gas generated from kerogen (17.76 m(3)/t) and gas generated from oil cracking (31.24 m(3)/t). The period of gas generated from kerogen is from the Cambrian to the Carboniferous with amount of gas generated value of 14.77 m(3)/t, which is mainly from the Lower Ordovician to the Middle Ordovician (510-470 Ma). The period of gas generated from oil cracking is from the Ordovician to the Triassic, and the main period of gas generated from oil cracking is from the Lower Devonian to the Upper Permian (410-250 Ma). The amounts of gas generated from oil cracking are 13.30 m(3)/t, 9.44 m(3)/t, and 3.77 m(3)/t in the Devonian, Carboniferous, and Permian, respectively.
机译:基于页岩和原油样品的热仿真实验,基于化学动力学方法计算了每个地质时期的基因酮和油裂产生的气体量。结果表明,从麦克隆孔中的NiutITang页岩产生的气体总量为49.00米(3)/ t,包括从Kerogen产生的气体(17.76米(3)/ t)和油裂化产生的气体(31.24米( 3)/ t)。从角化根产生的气体时期是从寒武纪到石炭系,气体产生的值为14.77米(3)/ t,主要来自下奥陶诺维安(510-470 mA)。从油裂产生的气体时期是从奥陶语到三叠纪的,并且从油裂产生的气体的主要时期是从较低的牧师到上二叠纪(410-250 mA)。从油裂解产生的气体量分别为13.30米(3)/ t,9.44米(3)/ t,分别在德文郡,石炭系和二叠纪的3.77米(3)/ t。

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