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Two accumulation modes of marine-origin natural gas in the Tarim Basin

机译:塔里木盆地海相天然气的两种聚集模式

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摘要

Hetianhe gas field, Lungudong gas field and Tazhong gas field are marine marine-origin natural gas reservoirs in the craton area in the Tarim Basin. The natural gas is generated from Cambrian source rocks. The simulation experiment indicated that the cracking of the dispersedly dissoluble organic matter remaining in the source rocks is the main origin of marine natural gas. There are two modes to form gas reservoirs, one is the dry gas reservoir such as Hetianhe gas field, in which gas accumulated on the fault belt with violent tectonic movement, the other is condensate gas reservoir formed on the inheriting uplift such as Lunnan and Tazhong gas fields. The hybrid simulation experiment of cracking gas and crude oil indicated that crude oil accumulated on a large scale in those uplift belts at the early stage, and natural gas filled the ancient oil reservoir at the late stage, and the gas reservoirs were formed after the gas mixed with the crude oil.
机译:和田河气田,area沽洞气田和塔中气田是塔里木盆地克拉通地区海相陆源天然气藏。天然气是由寒武纪烃源岩产生的。模拟实验表明,烃源岩中残留的分散可溶性有机物的裂解是海洋天然气的主要来源。形成气藏的方式有两种,一种是干田气藏,例如和田河气田,其中天然气以强烈的构造运动聚集在断层带上,另一种是在继承隆起形成的凝析气藏,例如轮南和塔中。气田。裂解气与原油的混合模拟实验表明,原油在早期隆起带大量聚集,后期天然气充填古油藏,天然气成藏后形成气藏。与原油混合。

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