地学前缘 ›› 2016, Vol. 23 ›› Issue (2): 176-189.DOI: 10.13745/j.esf.2016.02.018

• 页岩储层特征与评价 • 上一篇    下一篇

滇东地区马龙区块筇竹寺组海相页岩储层特征及对比研究

李昂,丁文龙,张国良,张名泉,张宗羲,闫宝珍,周传迅   

  1. 1. 中国地质大学(北京) 能源学院, 北京 100083
    2. 中国地质大学(北京) 页岩气勘查与评价国土资源部重点实验室, 北京 100083
    3. 中国地质大学(北京) 海相储层演化与油气富集机理教育部重点实验室, 北京 100083
    4. 北京资丰域博能源投资管理有限公司, 北京 100195
    5. 云南省煤炭地质勘查院, 云南 昆明 650218
  • 收稿日期:2015-11-14 修回日期:2015-12-08 出版日期:2016-03-15 发布日期:2016-03-15
  • 通讯作者: 丁文龙(1965—),男,教授,博士生导师,石油地质学专业,长期从事石油构造分析与控油作用、非常规油气构造和裂缝及其与含气量关系等方面的教学与科研工作。E-mail:dingwenlong2006@126.com
  • 作者简介:李昂(1990—),男,博士研究生,矿产普查与勘探专业,主要从事石油构造分析、页岩气构造和裂缝及其与含气量关系研究。E-mail:1073286570@qq.com
  • 基金资助:

    国家自然科学基金项目(41372139,41072098);国家油气重大专项专题(2016ZX05046 - 003,2011ZX05033 - 004,2011ZX05018 - 001 - 002)

Reservoir characteristics of marine shale in the Malong block of eastern Yunnan Province and comparison analysis.

  • Received:2015-11-14 Revised:2015-12-08 Online:2016-03-15 Published:2016-03-15

摘要:

利用最新钻探的马页1井的井下资料和大量岩心样品的测试分析数据,并结合野外地质调查资料,从富有机质页岩的有机地化、矿物组分、储集特性和裂缝特征等方面,系统地研究了滇东地区马龙区块下寒武统筇竹寺组黑色页岩的储层特征。研究区筇竹寺组黑色页岩有机碳丰度较高,TOC含量普遍大于2%;由于筇竹寺组地层较老,黑色页岩的有机质均处于高成熟过成熟阶段;黑色页岩的矿物组分主要为碎屑矿物、碳酸盐矿物和黏土矿物。脆性矿物含量较高,脆性指数平均值为0.62。黏土矿物主要以伊利石为主,其次为伊蒙混层和绿泥石,高岭石含量较低;该区筇竹寺组页岩的孔、渗较低,孔隙类型复杂多样,主要包括“墨水瓶”孔、板状孔和狭缝型孔。页岩主要发育纳米级中孔,且比表面积和总孔体积偏小,平均值分别为9.18 m2/g和10.38×10-3cm3/g;储层裂缝以高角度缝为主,上部碳质页岩裂缝发育,下部粉砂质页岩裂缝不发育。有机碳含量和脆性矿物含量促进了页岩裂缝的发育;与国内外典型海相页岩储层对比,滇东地区马龙区块筇竹寺组页岩以粉砂质页岩为主,碳质页岩层较薄,而Fort Worth盆地Barnett页岩、焦石坝地区龙马溪组页岩和岑巩区块牛蹄塘组页岩主要为硅质页岩和碳质页岩,筇竹寺组页岩的岩相与这3组海相页岩相比较差;筇竹寺组页岩有机碳含量低于其他3组海相页岩,有机质丰度中等;筇竹寺组页岩脆性矿物含量与龙马溪组页岩相当,稍低于牛蹄塘组页岩,脆性较好;Barnett页岩和龙马溪组页岩无论在储集物性上还是有机质孔隙发育程度上都要优于筇竹寺组页岩和牛蹄塘组页岩,筇竹寺组页岩有机质孔隙主要发育于有机质与黏土的混合物中;筇竹寺组页岩裂缝发育程度低于Barnett页岩、龙马溪组页岩和牛蹄塘组页岩。此外,筇竹寺组页岩含气量低于其他3组海相页岩,但吸附能力较强。

关键词: 马龙区块, 马页1井, 筇竹寺组, 海相页岩, 储层特征, 对比分析

Abstract:

Based on the latest drilling data, the laboratory test results of shale core samples from Well Maye1 and combined with the geologic survey of field outcrops, this paper systematically studies the reservoir characteristics of the Lower Cambrian Qiongzhusi shale in the Malong block of eastern Yunnan Province from organic geochemical characteristics, mineral constituents, reservoir properties and fracture characteristics. The Qiongzhusi shale of study area is characterized by high organic content with TOC over 2%. The black shale was all highover mature because of the old Qiongzhusi Formation. The major mineralogical compositions of shale are detrital minerals, carbonatite minerals and clay minerals. The black shale has a high brittleness mineral content and the brittleness index averages at 0.62. Clay minerals are mainly composed of illite, followed by the I/S layers and chlorite, and the kaolinite content is low. Qiongzhusi shale is characterized by low porosity and permeability and various pore types dominated by inkbottleshaped pores, platelike pores and slitshaped pores. Nanoscale mesopores in shale play an important role. The specific surface area and total pore volume are low with an average of 9.18 m2/g and 10.38×10-3cm3/g, respectively. The fissures of shale reservoir are mainly of high angle crack. Carbonaceous shale in the upper part of target layer is characterized by welldeveloped fissures and silty shale in the lower part of target layer possesses undeveloped fissures. TOC and brittle minerals contents promote the development of fissures. Compared with typical marine shale from home and abroad, the shale from Qiongzhusi Formation in the Malong block of eastern Yunnan Province is mainly composed of silty shale with some thin carbonaceous shale. Barnett shale from Fort Worth, Longmaxi shale from Jiaoshiba area and Niutitang shale from Cengong block are mainly carbonaceous and siliceous shale. So the lithofacies of Qiongzhusi shale is poorer than that of the other three kinds of marine shale. The TOC content of Qiongzhusi shale is moderate, lower than that of the other three kinds of marine shale. The brittleness minerals content of Qiongzhusi shale is similar to that of Longmaxi shale and slightly lower than that of Niutitang shale. Qiongzhusi shale is characterized by good brittleness. The reservoir property and development of organic matter pores of Barnett shale and Longmaxi shale are better than those of Qiongzhusi shale and Niutitang shale. The organic matter pores in Qiongzhusi shale mainly develop in the mixture of organic matter and clay. The fissure development of Qiongzhusi shale is poorer than that of Barnett shale, Longmaxi shale and Niutitang shale. In addition, the gas content of Qiongzhusi shale is lower than that of other three kinds of marine shale, and Qiongzhusi shale has a strong adsorption ability.

Key words: Malong block, Maye1 well, Qiongzhusi Formation, marine shale, reservoir characteristics, comparison analysis

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