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Nonproducing Carboniferous may have potential in Qaidam basin, NW China

机译:中国西北部柴达木盆地非生产石炭系可能具有潜力

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The Qaidam basin is one of three main oil and gas basins in Northwestern China, but its Carboniferous, formerly thought as a part of the metamorphic base of the basin, is a frontier formation without any oil and gas reserves or production.A large number of geological surveys have indicated most Carboniferous rocks to be sedimentary rocks with medium thermal evolution and hydrocarbon generation potential.More than 10 oil sands (bitumen deposits) were firstly discovered in Carboniferous outcrops in 2008-10. Geo-chemical evidence shows that these oil sands originate from Carboniferous source rocks. Using geochemical and analog methods, Carboniferous petroleum resources in place were calculated to be 4.5-5.3 billion bbl in the Qaidam basin. Its oil and gas resource richness is moderate compared with that of Carboniferous formations of other basins in the world. Hence, it is probable for the Carboniferous to become a successor of oil and gas productive formations in the Qaidam basin in the future.
机译:柴达木盆地是中国西北地区三大油气盆地之一,但其石炭纪曾被认为是该盆地变质基础的一部分,是一个边境地层,没有任何油气储量或产量。地质调查表明,大多数石炭系岩石是具有中等热演化和生烃潜力的沉积岩。2008-10年,石炭系露头首次发现了10多个油砂(沥青沉积物)。地球化学证据表明,这些油砂起源于石炭系烃源岩。使用地球化学和模拟方法,柴达木盆地的石炭纪石油资源估计为4.5-53亿桶。与世界上其他盆地的石炭系地层相比,其油气资源丰富度中等。因此,石炭纪很有可能在将来成为柴达木盆地油气生产地层的后继者。

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