鄂尔多斯盆地典型夹层型页岩油地质特征及潜力评价：以宁228井长7段为例

辛红刚; 田杨; 冯胜斌; 岳贤和; 陈薪凯; 淡卫东; 罗顺社

doi:10.19509/j.cnki.dzkq.tb20220224

鄂尔多斯盆地典型夹层型页岩油地质特征及潜力评价：以宁228井长7段为例

doi: 10.19509/j.cnki.dzkq.tb20220224

辛红刚^1,,
田杨^{2a, 2b, ,},
冯胜斌¹,
岳贤和^{2a, 2b},
陈薪凯¹,
淡卫东¹,
罗顺社^{2a, 2b}

1.
长庆油田勘探开发研究院, 西安 710200
2a.
长江大学非常规油气省部共建协同创新中心, 武汉 430100
2b.
长江大学地球科学学院, 武汉 430100

基金项目:

湖北省教育厅科学研究计划资助项目 Q20221311

非常规油气省部共建协同创新中心开放基金项目 UOG2022-40

详细信息

作者简介:
辛红刚(1972—), 男, 高级工程师, 主要从事油藏评价研究。E-mail: xinhg_cq@petrochina.com.cn

通讯作者:
田杨(1989—), 男, 讲师, 主要从事成藏动力学和成藏机理研究。E-mail: ty@yangtzeu.edu.cn

中图分类号: P618.130.2
计量
- 文章访问数: 812
- PDF下载量: 78
- 被引次数: 0
出版历程
- 收稿日期: 2021-10-17

Geological characteristics and potential evaluation of typical interlayer shale oil in the Ordos Basin: A case study of the Chang 7 Member of Well Ning228

Xin Honggang^1
,,
Tian Yang^{2a, 2b
, ,},
Feng Shengbin¹,
Yue Xianhe^{2a, 2b},
Chen Xinkai¹,
Dan Weidong¹,
Luo Shunshe^{2a, 2b}

1.
The Exploration and Development Research Institute of Changqing Oilfield, Xi′an 710200, China
2a.
Cooperative Innovation Center of Unconventional Oil and Gas of Ministry of Education & Hubei Province, Yangtze University, Wuhan 430100, China
2b.
School of Geosciences, Yangtze University, Wuhan 430100, China

摘要

摘要:
鄂尔多斯盆地长7段具有较好的页岩油资源潜力。长7段砂岩夹层型页岩油的勘探开发已经取得了实质性突破, 泥页岩型页岩油的勘探开发潜力巨大, 是长庆油田未来重要的油气接替资源, 但其相关地质基础性研究相对薄弱。通过对宁228井长7段全取心段厘米级岩心观察描述及系统采样, 一系列实验测试分析及鉴定结果表明：长7段主要发育黑色页岩、暗色泥岩、粉细砂岩及凝灰岩4种岩石类型；长7段烃源岩整体条件优越, 泥页岩有机碳含量高, 生烃潜力大, 有机质类型以Ⅰ型、Ⅱ型为主, 均处于低成熟-成熟阶段, 其中黑色页岩具有更高的有机质丰度；长7段主要储集空间为原生孔隙和次生孔隙, 泥页岩主要发育有机孔和无机孔, 粉细砂岩主要发育残余粒间孔、粒内孔和粒间孔, 凝灰岩则以粒间孔、矿物粒内孔为主；长7段整体含油性较好, 但可动性差异性大, 砂岩、凝灰岩的流体可流动性较好, 泥页岩的可流动性较差。总之, 典型夹层型页岩油精细解剖分析可以为推动鄂尔多斯盆地页岩油规模性开发提供有利指导。
- 鄂尔多斯盆地长7段 /
- 夹层型页岩油 /
- 沉积学特征 /
- 潜力评价
Abstract:
The Chang 7 Member of the Ordos Basin has favorable shale oil resource potentiality. The exploration and development of sandstone interlayer shale oil in the Chang 7 Member has made substantial breakthroughs. The exploration and development potential of shale oil is huge, and will be a significant oil and gas alternative resource in the Changqing Oilfield in the future, but its related geological fundamental research is relatively weak. Based on the observation, description and systematic sampling of the centimeter-level core of the full core section of Chang 7 Member in Well Ning228, a series of experimental test analyses and identification outcomes indicated that Chang 7 Member primarily developed four rock types: Black shale, dark mudstone, siltstone and tuff. The overall conditions of source rocks in the Chang 7 member are superior, the organic carbon content of shale is high, and the hydrocarbon generation potential is large. The organic matter types are mainly type Ⅰ and type Ⅱ, which are in the low mature-mature stage, and the black shale has higher organic matter abundance. The main reservoir spaces of the Chang 7 Member are primary pores and secondary pores. Mud shale primarily develops organic pores and inorganic pores. Fine sandstone mainly develops residual intergranular pores, intragranular pores and intergranular pores. Tuff mainly develops intergranular pores and mineral intragranular pores. The overall oil-bearing property of the Chang 7 Member is good, but the mobility difference is large. The fluid mobility in sandstone and tuff is good, and the mobility inshale is poor. In short, fine anatomical analysis of typical interlayer shale oil provides favorable guidance for promoting the large-scale development of shale oil in the Ordos Basin.
- Chang 7 Member of the Ordos Basin /
- interlayer shale oil /
- sedimentological characteristics /
- potential evaluation

HTML全文

图 1 鄂尔多斯盆地区域构造图(a)与延长组岩性柱状图(b)

Figure 1. Regional tectonic unit map of the Ordos Basin (a) and the comprehensive stratigraphic columnar map of the stratigraphy of the Yanchang Formation (b)

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图 2 宁228井长7段不同岩石类型岩石学特征

a.宁228井, 长7₃, 1 763.75 m, 页岩；b.宁228井, 长7₃, 1 762.30 m, 页岩；c.宁228井, 长7₃, 1 764.55 m, 油页岩具硅质纹层, 单偏光；d.宁228井, 长7₁, 1 672.75 m, 泥岩；e.宁228井, 长7₁, 1 672.50 m, 泥岩；f.宁228井, 长7₁, 1 672.50 m, 粉砂岩中具有机质纹层, 单偏光；g.宁228井, 长7₂, 1 720.60 m, 块状层理细砂岩；h.宁228井, 长7₂, 1 720.25 m, 由长石、石英颗粒、黏土杂基和少量碳酸盐矿物组成, 单偏光；i.宁228井, 长7₂, 1 728.40 m, 鲍马序列层理粉细砂岩, 具明显的火焰构造, 粉砂岩单层厚度较小, 单层厚度1~10 cm；j.宁228井, 长7₂, 1 728.35 m, 具明显火焰构造, 单偏光；k.宁228井, 长7₂, 1 697.75 m, 灰黄色凝灰岩中具有机质纹层；l.宁228井, 长7₂, 1 697.50 m, 蚀变凝灰岩中发育富有机质纹层状构造, 单偏光

Figure 2. Sedimentary petrology characteristics of different rock types in the Chang 7 Member of Well Ning228

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图 3 鄂尔多斯盆地宁228井长7段沉积与地球化学综合分析图

Figure 3. Comprehensive graphics for sedimentary and geochemical analysis of Chang 7 Member of Well Ning228 in Ordos Basin

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图 4 鄂尔多斯盆地宁228井长7段烃源岩有机质丰度判别图(a)和有机质类型图(b)

Figure 4. Organic matter abundance discrimination (a) and organic matter type diagram (b) of source rock in the Chang 7 Member of Well Ning28 in the Ordos Basin

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图 5 鄂尔多斯盆地宁228井长7段泥页岩与砂岩主要储集空间

a.宁228井, 长7₃, 1 758.85 m, 有机孔呈斑点状；b.宁228井, 长7₃, 1 751.10 m, 黑色有机质呈不规则的条状分布；c.宁228井, 长7₃, 1 741.75 m, 长英质矿物颗粒间发育的微孔隙；d.宁228井, 长7₂, 1 719.00 m, 黏土和杂基中发育大量微孔隙；e.宁228井, 长7₁, 1 693.70 m, 自形晶黄铁矿粒间充填有机质；f.宁228井, 长7₂, 1 723.00 m, 长石溶蚀孔隙发育；g.宁228井, 长7₂, 1 669.80 m, 残余粒间孔发育；h.宁228井, 长7₂, 1 707.80 m, 片丝状伊利石附着于颗粒表面发育伊利石晶间孔；i.宁228井, 长7₂, 1 767.35 m, 高岭石晶间孔

Figure 5. Main reservoir space of shale and sandstone in the Chang 7 Member of Well Ning228 in the Ordos Basin

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图 6 鄂尔多斯盆地宁228井长7段凝灰岩主要储集空间

a.宁228井, 长7₃, 1 761.20 m, 黏土矿物粒间孔发育；b.宁228井, 长7₃, 1 751.10 m, 粒间孔发育；c.宁228井, 长7₃, 1 742.75 m, 长石颗粒边缘发育溶蚀孔；d.宁228井, 长7₂, 1 719.00 m, 黄铁矿边缘发育微裂缝；e.宁228井, 长7₃, 1 764.15 m, 孔隙联通缝；f.宁228井, 长7₁, 1 751.7 m, 孔隙联通缝

Figure 6. Main reservoir space of tuff in the Chang 7 Member of Well Ning228, Ordos Basin

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图 7 鄂尔多斯盆地宁228井长7段典型样品页岩油含油性评价

Figure 7. Oiliness evaluation of typical shale oil samples from the Chang 7 Member of Well Ning228 in the Ordos Basin

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图 8 鄂尔多斯盆地宁228井长7段不同岩石类型可动流体对比分析

a.井深1 751.00 m, 页岩；b.井深1 718.90 m, 泥岩；c.井深1 722.55 m, 细砂岩；d.井深1 767.45 m, 凝灰岩

Figure 8. Comparative analysis of movable fluids for different types of rocks in the Chang 7 Member of Well Ning228, Ordos Basin

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图 9 鄂尔多斯盆地宁228井长7段页岩、砂岩抽提物族组分特征分布图

Figure 9. Distribution map of the group composition characteristics of shale and sandstone extracts in the Chang 7 Member of Well Ning228, Ordos Basin

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参考文献(28)

[1]	邹才能, 赵群, 王红岩, 等. 非常规油气勘探开发理论技术助力我国油气增储上产[J]. 石油科技论坛, 2021, 40(3): 72-79. https://www.cnki.com.cn/Article/CJFDTOTAL-SYKT202103008.htm Zou C N, Zhao Q, Wang H Y, et al. Theory and technology of unconventional oil and gas exploration and development helps China increase oil and gas reserves and production[J]. Petroleum Science and Technology Forum, 2021, 40(3): 72-79(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYKT202103008.htm
[2]	杜金虎, 胡素云, 庞正炼, 等. 中国陆相页岩油类型、潜力及前景[J]. 中国石油勘探, 2019, 24(5): 560-568. doi: 10.3969/j.issn.1672-7703.2019.05.003 Du J H, Hu S Y, Pang Z L, et al. The types, potentials and prospects of continental shale oil in China[J]. China Petroleum Exploration, 2019, 24(5): 560-568(in Chinese with English abstract). doi: 10.3969/j.issn.1672-7703.2019.05.003
[3]	金之钧, 朱如凯, 梁新平, 等. 当前陆相页岩油勘探开发值得关注的几个问题[J]. 石油勘探与开发, 2021, 48(6): 1276-1287. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202106021.htm Jin Z J, Zhu R K, Liang X P, et al. Several issues worthy of attention in current lacustrine shale oil exploration and development[J]. Petroleum Exploration and Development, 2021, 48(6): 1276-1287(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202106021.htm
[4]	柳波, 孙嘉慧, 张永清, 等. 松辽盆地长岭凹陷白垩系青山口组一段页岩油储集空间类型与富集模式[J]. 石油勘探与开发, 2021, 48(3): 521-535. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202103009.htm Liu B, Sun J H, Zhang Y Q, et al. Reservoir space and enrichment model of shale oil in the First Member of Cretaceous Qingshankou Formation in the Changling Sag, southern Songliao Basin, NE China[J]. Petroleum Exploration and Development, 2021, 48(3): 521-535(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202103009.htm
[5]	陈扬, 胡钦红, 赵建华, 等. 渤海湾盆地东营凹陷湖相富有机质页岩纹层特征和储集性能[J]. 石油与天然气地质, 2022, 43(2): 307-324. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202202006.htm Chen Y, Hu Q H, Zhao J H, et al. Lamina characteristics and their influence on reservoir property of lacustrine organic-rich shale in the Dongying Sag, Bohai Bay Basin[J]. Oil & Gas Geology, 2022, 43(2): 307-324(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202202006.htm
[6]	李继宏, 侯景涛, 杨艳宁, 等. 鄂尔多斯盆地志丹地区长7₃亚段泥页岩地球化学特征及页岩油地质意义[J]. 天然气地球科学, 2021, 32(12): 1839-1848. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112009.htm Li J H, Hou J T, Yang Y N, et al. Geochemical characteristics and geological significance of Chang 7₃ sub-member mud shale in Zhidan area, Ordos Basin[J]. Natural Gas Geoscience, 2021, 32(12): 1839-1848(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112009.htm
[7]	刘金, 王剑, 张宝真, 等. 准噶尔盆地吉木萨尔凹陷二叠系芦草沟组微-纳米孔隙页岩油原位赋存特征[J]. 石油实验地质, 2022, 44(2): 270-278. https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD202202008.htm Liu J, Wang J, Zhang B Z, et al. In situ occurrence of shale oil in micro-nano pores in Permian Lucaogou Formation in Jimsar Sag, Junggar Basin[J]. Petroleum Geology & Experiment, 2022, 44(2): 270-278(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYSD202202008.htm
[8]	周新平, 何青, 刘江艳, 等. 鄂尔多斯盆地三叠系延长组7段深水碎屑流沉积特征及成因[J]. 石油与天然气地质, 2021, 42(5): 1063-1077. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202105006.htm Zhou X P, He Q, Liu J Y, et al. Features and origin of deep-water debris flow deposits in the Triassic Chang 7 Member, Ordos Basin[J]. Oil & Gas Geology, 2021, 42(5): 1063-1077(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202105006.htm
[9]	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. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201604003.htm Yang H, Niu X B, Xu L M, et al. Exploration potential of shale oil in Chang 7 Member, Upper Triassic Yanchang Formation, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2016, 43(4): 511-520(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201604003.htm
[10]	刘全有, 李鹏, 金之钧, 等. 湖相泥页岩层系富有机质形成与烃类富集: 以长7为例[J]. 中国科学: 地球科学, 2022, 52(2): 270-290. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK202202006.htm Liu Q Y, Li P, Jin Z J, et al. Organic-rich formation and hydrocarbon enrichment of lacustrine shale strata: A case study of Chang 7 Member[J]. Science China: Earth Sciences, 2022, 52(2): 270-290(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK202202006.htm
[11]	付金华, 郭雯, 李士祥, 等. 鄂尔多斯盆地长7段多类型页岩油特征及勘探潜力[J]. 天然气地球科学, 2021, 32(12): 1749-1761. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112001.htm Fu J H, Guo W, Li S X, et al. Characteristics and exploration potential of muti-type shale oil in the 7th Member of Yanchang Formation, Ordos Basin[J]. Natural Gas Geoscience, 2021, 32(12): 1749-1761(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112001.htm
[12]	张斌, 毛治国, 张忠义, 等. 鄂尔多斯盆地三叠系长7段黑色页岩形成环境及其对页岩油富集段的控制作用[J]. 石油勘探与开发, 2021, 48(6): 1127-1136. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202106006.htm Zhang B, Mao Z G, Zhang Z Y, et al. Black shale formation environment and its control on shale oil enrichment in Triassic Chang 7 Member, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2021, 48(6): 1127-1136(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202106006.htm
[13]	李树同, 李士祥, 刘江艳, 等. 鄂尔多斯盆地长7段纯泥页岩型页岩油研究中的若干问题与思考[J]. 天然气地球科学, 2021, 32(12): 1785-1796. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112004.htm Li S T, Li S X, Liu J Y, et al. Some problems and thoughts on the study of pure shale-type shale oil in the 7th Member of Yanchang Formation in Ordos Basin[J]. Natural Gas Geoscience, 2021, 32(12): 1785-1796(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112004.htm
[14]	葸克来, 李克, 操应长, 等. 鄂尔多斯盆地三叠系延长组长7₃亚段富有机质页岩纹层组合与页岩油富集模式[J]. 石油勘探与开发, 2020, 47(6): 1244-1255. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202006020.htm Xi K L, Li K, Cao Y C, et al. Laminae combination and shale oil enrichment patterns of Chang 7₃ submember organic-rich shales in the Triassic Yanchang Formation, Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2020, 47(6): 1244-1255(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202006020.htm
[15]	杨智, 付金华, 郭秋麟, 等. 鄂尔多斯盆地三叠系延长组陆相致密油发现、特征及潜力[J]. 中国石油勘探, 2017, 22(6): 9-15. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201706002.htm Yang Z, Fu J H, Guo Q L, et al. Discovery, characteristics and resource potential of continental tight oil in Triassic Yanchang Formation, Ordos Basin[J]. China Petroleum Exploration, 2017, 22(6): 9-15(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201706002.htm
[16]	付金华, 牛小兵, 淡卫东, 等. 鄂尔多斯盆地中生界延长组长7段页岩油地质特征及勘探开发进展[J]. 中国石油勘探, 2019, 24(5): 601-614. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201905007.htm Fu J H, Niu X B, Dan W D, et al. The geological characteristics and the progress on exploration and development of shale oil in Chang 7 Member of Mesozoic Yanchang Formation, Ordos Basin[J]. China Petroleum Exploration, 2019, 24(5): 601-614(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201905007.htm
[17]	杨智, 邹才能, 付金华, 等. 大面积连续分布是页岩层系油气的标志特征: 以鄂尔多斯盆地为例[J]. 地球科学与环境学报, 2019, 41(4): 459-474. https://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201904007.htm Yang Z, Zhou C N, Fu J H, et al. Characteristics and "sweet area(section)" evaluation of continuous tight & shale oil and gas in Ordos Basin, north-central China[J]. Journal of Earth Sciences and Environment, 2019, 41(4): 459-474(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-XAGX201904007.htm
[18]	邓秀芹, 蔺昉晓, 刘显阳, 等. 鄂尔多斯盆地三叠系延长组沉积演化及其与早印支运动关系的探讨[J]. 古地理学报, 2008, 10(2): 159-166. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200802007.htm Deng X Q, Lin F X, Liu X Y, et al. Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the Early Indosinian Movement in Ordos Basin[J]. Journal of Palaeogeography, 2008, 10(2): 159-166(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200802007.htm
[19]	范柏江, 晋月, 师良, 等. 鄂尔多斯盆地中部三叠系延长组7段湖相页岩油勘探潜力[J]. 石油与天然气地质, 2021, 42(5): 1078-1088. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202105007.htm Fan B J, Jin Y, Shi L, et al. Shale oil exploration potential in central Ordos Basin: A case study of Chang 7 lacustrine shale[J]. Oil & Gas Geology, 2021, 42(5): 1078-1088(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202105007.htm
[20]	Jarvie D M. Shale resource systems for oil and gas: Part 2. Shale-oil resource systems[J]. AAPG Memoir, 2012, 97: 89-119. http://www.researchgate.net/publication/284338010_Shale_resource_systems_for_oil_and_gas_Part_2_Shale-oil_resource_systems
[21]	Jarvie D M. Components and processes affecting producibility and commerciality of shale resource systems[J]. Geol. Acta, 2014, 12: 307-325. http://www.barnettshalenews.com/documents/2012/pres/Components%20&%20Processes%20Affecting%20Producibility%20&%20Commerciality%20of%20Shale%20Resource%20Systems%20by%20Dan%20Jarvie%2C%20Shale%20Oil%20Symposium%2C%20China%2C%20April16-17%202012.pdf
[22]	黄振凯, 刘全有, 黎茂稳, 等. 鄂尔多斯盆地长7段泥页岩层系排烃效率及其含油性[J]. 石油与天然气地质, 2018, 39(3): 513-521, 600. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201803009.htm Huang Z K, Liu Q Y, Li M W, et al. Hydrocarbon expulsion efficiency and oil-bearing property of the shale system in Chang 7 Member, Ordos Basin[J]. Oil & Gas Geology, 2018, 39(3): 513-521, 600(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201803009.htm
[23]	孙中良, 王芙蓉, 韩元佳, 等. 潜江凹陷盐间页岩油储层孔隙结构分形表征与评价[J]. 地质科技通报, 2022, 41(4): 125-137. doi: 10.19509/j.cnki.dzkq.2021.0063 Sun Z L, Wang F R, Han Y J, et al. Characterization and evaluation of fractal dimension of intersalt shale oil reservoirs in Qianjiang Depression[J]. Bulletin of Geological Science and Technology, 2022, 41(4): 125-137(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2021.0063
[24]	时建超, 屈雪峰, 雷启鸿, 等. 致密油储层可动流体分布特征及主控因素分析: 以鄂尔多斯盆地长7储层为例[J]. 天然气地球科学, 2016, 27(5): 827-834, 850. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201605009.htm Shi J C, Qu X F, Lei Q H, et al. The distribution characteristics and main control factors of movable fluid in tight oil reservoirs: Taking Chang 7 reservoir in Ordos Basin as an example[J]. Natural Gas Geoscience, 2016, 27(5): 827-834, 850(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201605009.htm
[25]	孙照通, 辛红刚, 吕成福, 等. 鄂尔多斯盆地长7₃亚段泥页岩型页岩油的赋存状态与有机地球化学特征[J]. 天然气地球科学, 2022, 33(8): 1304-1318 https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202208009.htm Sun Z T, Xin H G, Lü C F, et al. Occurrence states and organic geochemical characteristics of shale-type shale oil from Chang 7₃ sub-member in the Ordos Basin[J]. Natural Gas Geoscience, 2022, 33(8): 1304-1318(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202208009.htm
[26]	王川, 董田, 蒋恕, 等. 中扬子地区上奥陶-下志留统五峰组-龙马溪组页岩纵向非均质性及主控因素[J]. 地质科技通报, 2022, 41(3): 108-121. doi: 10.19509/j.cnki.dzkq.2021.0053 Wang C, Dong T, Jiang S, et al. Vertical heterogeneity and the main controlling factors of the Upper Ordovician-Lower Silurian Wufeng-Longmaxi shales in the Middle Yangtzc region[J]. Bulletin of Geological Science and Technology, 2022, 41(3): 108-121(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2021.0053
[27]	李士祥, 周新平, 郭芪恒, 等. 鄂尔多斯盆地长7₃亚段页岩油可动烃资源量评价方法[J]. 天然气地球科学, 2021, 32(12): 1771-1784. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112003.htm Li S X, Zhou X P, Guo Q H, et al. Research on evaluation method of movable hydrocarbon resources of shale oil in the Chang 7₃ sub-member in the Ordos Basin[J]. Natural Gas Geoscience, 2021, 32(12): 1771-1784(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202112003.htm
[28]	关平, 徐永昌, 刘文汇. 烃源岩有机质的不同赋存状态及定量估算[J]. 科学通报, 1998, 43(14): 1556-1559. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199814025.htm Guan P, Xu Y C, Liu W H. Quantitative estimates of different existing state of organic matter in source rocks[J]. Chinese Science Bulletin, 1998, 43(14): 1556-1559(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199814025.htm