中国石油勘探 ›› 2019, Vol. 24 ›› Issue (4): 498-508.DOI: 10.3969/j.issn.1672-7703.2019.04.010

• 石油地质 • 上一篇    下一篇

柴西地区天然气成因、类型及成藏规律

张永庶1, ,周飞1, ,王波1, ,曾旭2, ,张静1, ,张小波1,   

  1. 1 中国石油青海油田公司勘探开发研究院;2 中国石油勘探开发研究院
  • 出版日期:2019-07-15 发布日期:2019-07-15
  • 作者简介:张永庶(1974-),男,四川南部人,1998 年毕业于石油大学(华东),高级工程师,现从事油气地质综合研究及勘探生产工作。 地址:甘肃省敦煌市七里镇青海油田公司勘探开发研究院,邮政编码:736202。E-mail: zysqh@petrochina.com.cn
  • 基金资助:
    国家科技重大专项“柴达木复杂构造区油气成藏、关键勘探技术与新领域目标优选”(2016ZX05003-006);中国石油 天然气股份有限公司重大科技专项“柴达木盆地建设高原大油气田勘探开发关键技术研究与应用”(2016E-0102)。

Genesis, type and reservoir formation law of natural gas in western Qaidam Basin

Zhang Yongshu1,, Zhou Fei1,, Wang Bo1,, Zeng Xu2,, Zhang Jing1,, Zhang Xiaobo1,,   

  1. 1 Research Institute of Exploration and Development, PetroChina Qinghai Oilfield Company; 2PetroChina Research Institute of Petroleum Exploration & Development
  • Online:2019-07-15 Published:2019-07-15
  • Supported by:
     

摘要: 柴达木盆地西部凹陷区是重要的油气勘探领域,发育独特的古近系—新近系高原咸化湖相烃源岩。近年 来,天然气勘探在南翼山、黄瓜峁、开特米里克、英中和扎哈泉等中深层获得了重要发现,发现多个天然气藏。但是 该区的天然气来源存在较大争议,是否存在深层侏罗系煤型气的混入影响着对该地区天然气、成藏模式的认识以及下 一步的勘探方向。在综合分析大量天然气样品地球化学特征的基础上,研究柴西地区古近系—新近系与柴北缘侏罗系 天然气地球化学特征差异性,以及伴生原油地球化学特征和区域地质条件,取得以下3 点认识:(1) 与其他地区不同, 乙烷碳同位素不能作为鉴别柴西地区高成熟咸化湖相天然气类型的主要指标;(2) 柴西地区的天然气主要来源于自 身发育的下干柴沟组上段(E3 2)和上干柴沟组(N1)咸化湖相烃源岩,主要为油型气,几乎不存在侏罗系煤型气 的混入;(3) 柴西地区天然气成藏具有就近成藏的特点,横向短距离运移,垂向晚期调整。并指出烃源岩埋深大、成 熟度高的区域,如英东、黄瓜峁—开特米里克和南翼山—油墩子地区,是今后重要的勘探领域。

 

关键词: 油型气, 煤型气, 天然气碳同位素, 天然气类型, 柴西地区

Abstract: The western depressed area of the Qaidam Basin is an important zone for oil and gas exploration, with unique Paleogene-Neogene source rocks in plateau saline lake facies. In recent years, important discoveries have been made in the middle-deep layers of Nanyishan, Huangguayao, Kaitemilike, Yingzhong and Zahaquan, etc., and many natural gas reservoirs have been discovered. However, the source of natural gas in this area is controversial. Whether there is mixed deep Jurassic coal-type gas affects the understanding of natural gas and reservoir-forming model in this area and the next exploration direction. On the basis of comprehensive analysis of geochemical characteristics of a large number of natural gas samples, the geochemical differences of natural gas between Paleogene-Neogene in western Qaidam Basin and Jurassic in the northern margin of the Qaidam Basin, and the geochemical characteristics of associated crude oil and regional geological conditions were studied, and the following three cognitions were obtained: (1) Unlike other regions, carbon isotope of ethane cannot be used as the main index to identify the type of high mature saline lacustrine natural gas in western Qaidam Basin. (2) The natural gas in western Qaidam Basin mainly comes from the saline lacustrine source rocks of the upper member of the Lower Ganchaigou Formation (E3 2) and the Upper Ganchaigou Formation (N1). They are mainly oil-type gas, and there is almost no mixed Jurassic coal-type gas. (3) Gas accumulation in western Qaidam Basin is characterized by near source, with short transverse migration distance and late vertical adjustment. The areas with deep burial and high maturity of source rocks, such as Yingdong, Huangguayao-Kaitemilike and Youdunzi, are important exploration areas in the future.

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