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现代地质 ›› 2016, Vol. 30 ›› Issue (1): 181-191.

• 能源地质学 • 上一篇    下一篇

滇黔桂盆地泥盆系页岩气成藏条件及资源潜力分析

孟江辉1,2,潘仁芳1,2,陈浩3,唐小玲1,2   

  1. (1. 长江大学油气资源与勘探技术教育部重点实验室,湖北 武汉 430100;2. 长江大学 非常规油气湖北省协同创新中心,
    湖北 武汉430100;3.中海石油(中国)有限公司上海分公司,上海200030)
  • 出版日期:2016-01-29 发布日期:2016-05-01
  • 作者简介:孟江辉,男,博士,副教授,1983年出生,地质资源与地质工程专业,主要从事非常规油气地质研究。 Email: mjhyzu@163.com。
  • 基金资助:

    国家自然科学基金项目“中扬子区下古生界页岩气关键评价指标限定值研究”(41402114);中国博士后科学基金项目“我国西南古生界高-过热演化条件下页岩气评价标准研究”(2013M530342)。

Shale Gas Accumulation Condition and Resource Potential Analysis of Devonian in Dian-Qian-Gui Basin

MENG Jiang-hui1,2, PAN Ren-fang1,2, CHEN Hao3, TANG Xiao-ling1,2   

  1. (1. Key Laboratory of Oil and Gas Resources and Exploration Technology of Ministry of Education, Yangtze University, Wuhan,Hubei
    430100, China; 2. Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan,Hubei 430100, China;
    3. Shanghai Branch of CNOOC Ltd., Shanghai 200030, China)
  • Online:2016-01-29 Published:2016-05-01

摘要:

通过野外露头观察、剖面测量和样品测试,分析了滇黔桂盆地泥盆系页岩气成藏条件。研究结果表明:滇黔桂盆地中、下泥盆统发育两套台盆相暗色泥页岩沉积,泥页岩单层厚度为10~55 m,累计厚度普遍在100~450 m之间;泥页岩TOC一般为1.0%~2.5%,有机质类型为Ⅰ型-Ⅱ1型,处于高-过成熟热演化阶段;储层物性接近于四川盆地威201井寒武系九老洞组页岩,发育多种储集空间类型,脆性矿物含量平均值为46%,具备储集条件;黔南坳陷西南部和桂中坳陷中西部地区地层相对平缓,断裂密度和剥蚀厚度小,且断裂性质以逆冲、压扭为主,页岩气保存条件相对较好。综合考虑暗色泥页岩厚度、埋藏深度、有机碳含量、热演化程度和保存条件等因素,预测滇黔桂盆地泥盆系页岩气有利层段为塘丁组和罗富组,有利区主要分布于天峨—南丹—河池一带以及桂中坳陷中部的鹿寨—来宾—合山—大化地区。利用地质资源丰度类比法计算出该区页岩气地质资源量为0.66×1012~1.09×1012 m3

关键词: 页岩气, 资源潜力, 泥盆系, 滇黔桂盆地

Abstract:

Based on the outcrop observation, profile survey and sample analysis of Devonian dark shale, this paper studied the accumulation condition of Devonian shale gas in Dian-Qian-Gui Basin. The results show that two sets of dark shales of intraplatform depression facies were deposited in Dian-Qian-Gui Basin during the Early to Middle Devonian, and the single layer thickness of Devonian shale is 10-55 m; the accumulative thickness is generally between 100 m and 450 m. The TOC values are mainly in the range of 1.0% to 2.5%, and the organic matter type is Ⅰ-Ⅱ1, and the vitrinite reflectance values indicate high to over mature thermal evolution stages. As an effective reservoir, the porosity and permeability of Devonian shale in Dian-Qian-Gui Basin are similar to those of Jiulaodong Formation in well Wei-201, and various reservoir space types well developed in the shale, and the content of brittle minerals is averagely up to 67%. The gas preservation conditions of southwestern Qiannan Depression and middle-west Guizhong Depression are relatively better because of the relative flat strata, low fault density and erosion thickness, and thrusting and transpressional faults. Overall considering of the dark shale thickness, buried depth, organic matter content, thermal evolution degree and preservation condition, it can be predicted that the favorable intervals of Devonian shale gas are Tangding Formation and Luofu Formation, and the favorable areas mainly distribute in Tian’e-Nandan-Hechi area and Luzhai-Laibin-Heshan-Dahua area of middle Guizhong Depression. By using the analogy method of geological resource abundance, it can be calculated that the geological resources of Devonian shale gas is 0.66×1012 m3 to 1.09×1012 m3 .

Key words: shale gas, resource potential, Devonian, Dian-Qian-Gui Basin

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