沙垒田凸起古近纪源-汇系统中有利储层评价与预测

李顺利; 朱筱敏; 刘强虎; 徐长贵; 杜晓峰; 李慧勇

doi:10.3799/dqkx.2017.127

沙垒田凸起古近纪源-汇系统中有利储层评价与预测

doi: 10.3799/dqkx.2017.127

李顺利^1,2,,
朱筱敏^1, ,,
刘强虎³,
徐长贵⁴,
杜晓峰⁴,
李慧勇⁴

1.
油气资源与工程国家重点实验室, 中国石油大学地球科学学院, 北京 102249
2.
中国地质大学能源学院, 北京 100083
3.
中国地质大学构造与油气资源教育部重点实验室, 湖北武汉 430074
4.
中海石油(中国)有限公司天津分公司渤海石油研究院, 天津 300452

基金项目:

国家自然科学基金项目 41272133

国家科技重大专项 2016ZX05024-002-002

博士后基金项目 2015M581269

详细信息

作者简介:
李顺利(1987-), 男, 讲师, 从事碎屑岩沉积学、储层地质学研究及相关教学工作

通讯作者:
朱筱敏

中图分类号: P624
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- 被引次数: 0
出版历程
- 收稿日期: 2017-05-17
- 刊出日期: 2017-11-15

Evaluation and Prediction of Favorable Reservoirs in Source-to-Sink Systems of the Palaeogene, Shaleitian Uplift

Li Shunli^{1,2
,},
Zhu Xiaomin^{1
, ,},
Liu Qianghu³,
Xu Changgui⁴,
Du Xiaofeng⁴,
Li Huiyong⁴

1.
State Key Laboratory of Petroleum Resource and Prospecting, College of Geosciences of China University of Petroleum, Beijing 102249, China
2.
School of Energy Resources, China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan 430074, China
4.
Tianjin Branch of China National Offshore Oil Corporation Limited, Tianjin 300452, China

摘要

摘要: 渤海湾盆地沙垒田凸起与围区凹陷形成了典型的陆相断陷湖盆源-汇系统.基于钻井、地震、岩心及储层分析资料，刻画了沙垒田凸起及围区源-汇系统要素特征，并将源-汇系统分为断裂陡坡型、断裂缓坡型、斜坡型及断槽型4大类.不同类型源-汇系统的物源供给控制相应的沉积体系发育，从而影响其储层的成岩作用与物性特征.研究表明，沙垒田凸起围区凹陷的储层发育受源-汇系统要素耦合与成岩作用的共同控制，其中断裂缓坡带由于源区高差与汇水面积大，沿断裂坡折带分布的沉积体系与砂体规模大、范围广，砂岩成分、结构成熟度较高，埋深浅、机械压实作用较弱，次生孔隙发育，为优质储层发育的有利区，而断裂陡坡型、斜坡型及断槽源-汇系统次之.
- 源-汇系统类型 /
- 成岩作用 /
- 储层分类 /
- 沙垒田凸起 /
- 石油地质 /
- 沉积
Abstract: The Shaleitian uplift and its surrounding areas in the Bohai bay basin constitute a typical Source-to-Sink (S2S) system in terrestrial rift basin. Based on the data of drilling, seismic, core, and reservoir analysis, this paper illustrates element characteristics of S2S systems in the Shaleitian uplift and its surrounding areas. The S2S systems are classified into four types, namely, faulted-steep-slope, faulted-gentle-slope, gentle-slope, and faulted-trough. Different S2S systems controlled various depositional systems, and subsequently influenced their reservoir diagenesis and properties. Research results indicate that reservoir development in sags around the Shaleitian uplift was influenced both by element coupling of the S2S systems and diagenesis. The faulted-gentle-slope was characterized by high elevation of source rocks and catchment area, which developed large scale of depositional systems and sandbodies along the fault break zones. The sandstone in this kind of S2S systems was high quality reservoirs with high maturity of component and texture, shallow buried depth, weak mechanical compaction, and abundant secondary porosity. However, other S2S systems including faulted-steep-slope, gentle-slope, and faulted-trough developed less high quality reservoirs.
- source-to-sink system /
- diagenesis /
- reservoir classification /
- Shaleitian uplift /
- petroleum geology /
- sedimentary

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图 1 渤海湾盆地沙垒田凸起及围区地质概况

Fig. 1. Geological settings of the Shaleitian uplift and surrounding area in the Bohai bay basin

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图 2 渤海湾盆地沙垒田凸起及围区古近系综合柱状图

Fig. 2. Integrated stratigraphic column of the Paleogene in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 3 渤海湾盆地沙垒田凸起古近纪汇水体系与搬运通道分布

Fig. 3. Distribution of catchment area and transport pathways in the Paleogene on the Shaleitian uplift, Bohai bay basin

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图 4 渤海湾盆地沙垒田凸起及围区古近系沉积体系类型

SP单位为mV；GR单位为API；RS、RT、LLD、RILM、RMSFL单位均为Ω·m；深度单位为m

Fig. 4. Types of depositional systems of the Paleogene in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 5 渤海湾盆地沙垒田凸起及围区古近系沉积砂体类型与展布特征

Fig. 5. Types and distribution of Paleogene sedimentary sandbodies in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 6 渤海湾盆地沙垒田凸起及围区源-汇系统类型

地震剖面时深关系y=0.000 2x²+0.697 5x+105.4，R²=0.999 5

Fig. 6. Types of Source-to-Sink systems in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 7 沙垒田凸起围区沙河街组储层岩石学与物性特征

a.碎屑组分相对含量；b.储层孔隙类型及频率

Fig. 7. Petrology and physical property of Paleogene reservoir in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 8 沙垒田凸起围区沙河街组储层成岩作用特征

a.颗粒受机械压实作用呈线接触；SLT-3-1井，3 830.54 m；b.嵌晶状方解石胶结；SLT-2-1井，3 165.80 m；c.自生石英晶粒，SLT-2-1，3 281.30 m；d.绿泥石及伊/蒙混层粘土，SLT-3-1井，3 787.00 m；e.粒间溶孔，SLT-1-4D井，3 991.20 m；f.粒内溶蚀孔隙，SLT-1-1，3 673.80 m

Fig. 8. Reservoir diagenetic characteristics of the Shahejie Formation in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 9 渤海湾盆地沙南凹陷沙河街组储层成岩序列

Fig. 9. Diagenetic sequence of reservoir in the Shahejie Formation in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 10 渤海湾盆地沙垒田凸起围区沙河街组储层类型分布

颜色区域为沙河街组发育深度

Fig. 10. Distribution of reservoir type in the Shaleitian uplift and surrounding area, Bohai bay basin

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图 11 渤海湾盆地沙垒田凸起及围区沙河街组有利储层分布

Fig. 11. Distribution of the favorable reservoirs in the Shaleitian uplift and surrounding area, Bohai bay basin

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表 1 渤海湾盆地沙垒田凸起围区沙河街组储层分类评价参数标准

Table 1. Reservoir classification and evaluation parameters of the Shahejie Formation in the Shaleitian uplift and surrounding area, Bohai bay basin

分类参数		物源位置
分类参数		Ⅰ	Ⅱ	Ⅲ	Ⅳ
沉积特征	粒度(mm)	粗砂岩、中砂岩、细砂岩		细砂岩粉细砂岩	细粉砂岩
沉积特征	沉积微相	辫状河三角洲内前缘扇三角洲前缘滨岸滩坝		三角洲外前缘	前三角洲滨浅湖
物性特征	φ(%)	＞20	10~20	6~10	＜6
物性特征	K(mD)	＞100	1-100	0.1 ~1.0	＜0.1
	成岩相	长石溶蚀相剩余粒间孔相	长石溶蚀相碳酸盐胶结物溶蚀相	碳酸盐胶结相	机械压实相碳酸盐胶结相
孔隙结构	排驱压力(MPa)	＜0.1	0.1~0.5	0.5 ~1.5	＞1.5
	孔隙结构类型	大孔粗喉型	中孔中喉型	小孔微喉型	小孔微喉型
	平均喉道半径(μm)	＞5.5	1.0-5.5	0.6-1.0	＜0.6
	退汞效率(%)	＞40	45-40	40-35	＜35
	储层评价	好	较好	一般	差

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表 2 源-汇系统类型与储层差异对比

Table 2. Type of Source-to-Sink systems and their reservoir difference

源-汇系统	断裂活动	沉积体系	成岩作用	储层类型
断裂陡坡型	强烈 (生长指数＞2)	扇三角洲	压实作用与胶结作用强烈，少量次生孔隙	Ⅱ、Ⅲ类储层为主
断裂缓坡型	中等 (生长指数＜2)	扇三角洲/ 辫状河三角洲	压实作用中等，次生孔隙发育	Ⅰ类储层为主，同时发育Ⅱ、Ⅲ类储层
斜坡型	无	辫状河三角洲	胶结作用强烈，次生孔隙较少	Ⅱ、Ⅲ类储层为主，少量Ⅳ类储层
断槽型	走滑	扇三角洲	成岩作用差异较大，次生孔隙较为发育	Ⅰ类储层较少， Ⅱ、Ⅲ、Ⅳ类储层较多

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