深圳大学学报理工版

与依靠水平井体积压裂技术的页岩气、致密油开发相比,原位转化/改质技术更适合规模效益开发中国陆相大面积分布、成熟度介于0.5%～1.0%、总有机碳质量分数大于6%的页岩层系液态烃资源.本研究基于原位转化/改质技术具有不受地质条件限制、地下转化轻质油、高采出程度、较低污染等技术优势的特点,综合考虑鄂尔多斯盆地延长组7段页岩厚度、页岩有机质丰度、热演化程度和现今埋深等地质参数,评价优选试验有利区主要分布在盆地东南部,其中埋深小于1 500 m的分布面积大于6 000 km2.页岩选区评价结果表明,鄂尔多斯盆地陆相页岩是原位转化/改质技术工业试验的有利页岩分布区.

Compared with the multi-stage horizontal well fracturing technology facilitating development of shale gas and tight oil, in-situ conversion/upgrading processing is more suitable for development of liquid hydrocarbons in broad continental shale formations with the maturity of 0.5%-1.0% and total organic carbon of over 6% in China. This technology has several unique advantages including wide applicability to various geologic conditions, underground conversion to light oil, high oil recovery, and lower environmental pollution. Based on the requirements of this technology, together with key geologic parameters of Yanchang-7 shale, including thickness, organic matter abundance, thermal evolution degree, and burial depth, the pilot areas are selected in the southeastern part of the basin, with area of over 6 000 km2 and buried depth less than 1 500 m. The selection result of the pilot areas indicates that, the lacustrine shales in the Ordos Basin will be favourable shale areas for the industrial test of in-situ conversion/upgrading processing.

引言
1 原位转化/改质技术现状
2 鄂尔多斯盆地页岩地质特征
3 基于原位转化/改质技术的页岩有利区评价
4 结论

图1 鄂尔多斯盆地延长组地质地理概况图
Fig.1 Geologic and geographic profile of Yanchang Formation in Ordos Basin

图2 鄂尔多斯盆地延长组7段页岩厚度图(单位:m.151个控制点)<br/>Fig.2 Shale thickness isoline map of the 7th member of Yanchang Formation in Ordos Basin(unit: m. 151 control points)

图2 鄂尔多斯盆地延长组7段页岩厚度图(单位:m.151个控制点)
Fig.2 Shale thickness isoline map of the 7th member of Yanchang Formation in Ordos Basin(unit: m. 151 control points)

图3 鄂尔多斯盆地延长组7段页岩扫描电镜微观照片<br/>Fig.3 The scanning electronic microscope microphotograph of the 7th member of Yanchang Formation in Ordos Basin

图3 鄂尔多斯盆地延长组7段页岩扫描电镜微观照片
Fig.3 The scanning electronic microscope microphotograph of the 7th member of Yanchang Formation in Ordos Basin

图4 鄂尔多斯盆地延长组7段页岩有机质丰度(357个数据点)<br/>Fig.4 Shale organic matter abundance of the 7th member of Yanchang Formation in Ordos Basin(357 data points)

图4 鄂尔多斯盆地延长组7段页岩有机质丰度(357个数据点)
Fig.4 Shale organic matter abundance of the 7th member of Yanchang Formation in Ordos Basin(357 data points)

图5 鄂尔多斯盆地长7段页岩有机质成熟度与类型(425个数据点)<br/>Fig.5 Shale organic maturity and type of the 7th member of Yanchang Formation in Ordos Basin(425 data points)

图5 鄂尔多斯盆地长7段页岩有机质成熟度与类型(425个数据点)
Fig.5 Shale organic maturity and type of the 7th member of Yanchang Formation in Ordos Basin(425 data points)

图6 鄂尔多斯盆地延长组7段页岩厚度×w(TOC)(113个控制点)<br/>Fig.6 Shale thickness×w(TOC)isoline map of 7th member of Yanchang Formation in Ordos Basin(113 control points)

图6 鄂尔多斯盆地延长组7段页岩厚度×w(TOC)(113个控制点)
Fig.6 Shale thickness×w(TOC)isoline map of 7th member of Yanchang Formation in Ordos Basin(113 control points)

图7 鄂尔多斯盆地延长组7段页岩地史时期最大埋深等值线图(单位:m. 152个控制点)<br/>Fig.7 The deepest burial depth isoline map of the 7th member of Yanchang Formation shalein geohistory in Ordos Basin(unit: m. 152 control points)

图7 鄂尔多斯盆地延长组7段页岩地史时期最大埋深等值线图(单位:m. 152个控制点)
Fig.7 The deepest burial depth isoline map of the 7th member of Yanchang Formation shalein geohistory in Ordos Basin(unit: m. 152 control points)

图8 鄂尔多斯盆地延长组7段页岩ICP/IUP技术试验有利区综合评价图<br/>Fig.8 The favorable zone evaluation map for industry test of the 7th member of Yanchang Formation shale in Ordos Basin using ICP/IUP technology, Ordos Basin

图8 鄂尔多斯盆地延长组7段页岩ICP/IUP技术试验有利区综合评价图
Fig.8 The favorable zone evaluation map for industry test of the 7th member of Yanchang Formation shale in Ordos Basin using ICP/IUP technology, Ordos Basin

[1] Jarvie D M. Shale resource systems for oil and gas: part 2: shale-oil resource systems[J]. AAPG Memoir, 2012, 97:89-119.
[2] Cander H. What is unconventional resources? A simple definition using viscosity and permeability[J]. AAPG Annual Convention and Exhibition, 2012, 80217: 1-3
[3] Sarg J F. The Bakken: an unconventional petroleum and reservoir system[R]. Golden: Office of Scientific & Technical Information Technical Reports, 2012.
[4] 邱中建,邓松涛.中国油气勘探的新思维[J].石油学报,2012, 33(z1):1-5.
[5] 贾承造,邹才能,李建忠,等.中国致密油评价标准、主要类型、基本特征及资源前景[J].石油学报,2012, 33(3):343-350.
[6] 赵文智,胡素云,李建忠,等.我国陆上油气勘探领域变化与启示[J].中国石油勘探,2013, 18(4):1-10.
[7] 邹才能,张国生,杨智,等.非常规油气概念、特征、潜力及技术——兼论非常规油气地质学[J].石油勘探与开发,2013, 40(4):385-399.
[8] 国家能源局.致密油地质评价方法(SY/T6943—2013)[M]. 北京:石油工业出版社,2014.
[9] Zou Caineng. Unconventional petroleum geology[M]. Beijing: Geological Press, 2014.
[10] Zou Caineng, Yang Zhi, Zhu Rukai,et al. Progress in China's unconventional oil & gas exploration and development and theoretical technologies[J]. Acta Geologica Sinica English Edition,2015,89(3):938-971.
[11] 杨智,邹才能,吴松涛,等.含油气致密储层纳米级孔喉特征及意义[J].深圳大学学报理工版,2015, 32(3):257-265.
[12] 杨华, 李士祥, 刘显阳, 等. 鄂尔多斯盆地致密油、页岩油特征及资源潜力[J]. 石油学报, 2012, 34(1): 1-11.
[13] 姚泾利, 邓秀芹, 赵彦德, 等. 鄂尔多斯盆地延长组致密油特征[J]. 石油勘探与开发, 2013, 40(2): 150-158.
[14] 邹才能, 杨智, 崔景伟, 等. 页岩油形成机制、地质特征及发展对策[J]. 石油勘探与开发, 2013, 40(1): 14-26.
[15] 杨智,侯连华,陶士振,等. 致密油与页岩油形成条件与“甜点区”评价[J]. 石油勘探与开发,2015,42(5):555-565.
[16] 杨华,牛小兵,徐黎明,等. 鄂尔多斯盆地三叠系长 7 段页岩油勘探潜力[J]. 石油勘探与开发, 2016, 43(4): 511-520.
[17] Alpak F O, Vink J C, Gao Guohua, et al. Techniques for effective simulation, optimization, and uncertainty quantification of the in-situ upgrading process[J]. Journal of Unconventional Oil & Gas Resources, 2013, 3/4:1-14.
[18] 汪友平,王益维,孟祥龙,等. 美国油页岩原位开采技术与启示[J]. 石油钻采工艺,2013,35(6):55-59.
[19] Zhao Mengwei, Behr H J, Ahrendt H,et al. Thermal and tectonic history of the Ordos Basin, China: evidence from apatite fission track analysis, vitrinite reflectance, and K-Ar dating[J].AAPG Bulletin,1996,80(7):1110-1133.
[20] 杨智,付金华,刘新社,等. 苏里格上古生界连续型致密气形成过程[J]. 深圳大学学报理工版,2016,33(3):221-233.
[21] Dai Jinxing, Zou Caineng, Dong Dazhong, et al. Geochemical characteristics of marine and terrestrial shale gas in China[J]. Marine and Petroleum Geology, 2016, 76: 444- 463.
[22] Yang Zhi, He Sheng, Guo Xiaowen, et al. Formation of low permeability reservoirs and gas accumulation process in the Daniudi Gas Field, Northeast Ordos Basin, China[J]. Marine and Petroleum Geology, 2016, 70: 222-236.
[23] 陈瑞银,罗晓容,陈占坤,等. 鄂尔多斯盆地中生代地层剥蚀量估算及其地质意义[J]. 地质学报,2006,80(5):685- 693.
[24] Ren Zhanli, Zhang Sheng, Gao Shengli, et al. Tectonic thermal evolution history of the Ordos basin and its hydrocarbon accumulation significance[J]. Science in China Series D: Earth Sciences, 2007, 37(s2): 23-32.
[25] Zou Caineng, Yang Zhi, Tao Shizhen, et al. Continuous hydrocarbon accumulation over a large area as a distinguishing characteristic of unconventional petroleum: The Ordos Basin, North-Central China[J]. Earth-Science Reviews, 2013, 126: 358-369.
[26] 付金华, 邓秀芹, 楚美娟, 等. 鄂尔多斯盆地延长组深水岩相发育特征及其石油地质意义[J]. 沉积学报, 2013, 31(5): 928-938.
[27] 袁选俊, 林森虎, 刘群, 等. 湖盆细粒沉积特征与富有机质页岩分布模式: 以鄂尔多斯盆地延长组长7油层组为例[J]. 石油勘探与开发, 2015, 42(1): 34- 43.

备注

引言

1 原位转化/改质技术现状

2 鄂尔多斯盆地页岩地质特征

3 基于原位转化/改质技术的页岩有利区评价

4 结论

期刊信息

备注

引言

1 原位转化/改质技术现状

2 鄂尔多斯盆地页岩地质特征

3 基于原位转化/改质技术的页岩有利区评价

4 结 论

期刊信息

4 结论