莺歌海盆地高温超压环境下储层物性影响因素

姜涛; 解习农

莺歌海盆地高温超压环境下储层物性影响因素

姜涛,
解习农

中国地质大学资源学院, 湖北武汉 430074

基金项目:

教育部科学技术研究重点项目“超压盆地流体系统及成藏动力学研究” 01038

详细信息

作者简介:
姜涛(1979 - ), 男, 在读博士生, 2000年毕业于中国地质大学(武汉)石油系, 现主要从事油气成藏动力学和储层沉积学方向的研究

中图分类号: P618
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出版历程
- 收稿日期: 2004-09-30
- 刊出日期: 2005-03-25

Effects of High Temperature and Overpressure on Reservoir Quality in the Yinggehai Basin, South China Sea

Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 莺歌海盆地由于独特的沉积地层和温压场特征, 使得盆地内的储层成岩演化也具有了与众不同的过程和特点.通过对莺歌海盆地内有钻井证实的两种超压体系类型(自源型和传导型) 的对比研究, 阐明了其成因差别及其石油地质意义, 并详细论述了高温超压环境下储层物性的影响因素: (1) 储层物性主要受沉积环境和成岩作用控制; (2) 高地温梯度使砂岩的孔隙度衰减较快; (3) 超压保存了一部分原生孔隙, 这是深部储层还具有高孔隙度的最主要原因; (4) 超压通过溶解等成岩作用产生了一些次生孔隙; (5) 流体压裂突破过程中产生了大量的裂缝, 有效地提高了储层渗透性.
- 异常压力 /
- 储层物性 /
- 超压类型 /
- 莺歌海盆地
Abstract: Research into hydrocarbon basins around the world has shown that overpressure is closely connected with hydrocarbon generation and distribution. Because of unique sedimentary sequences and temperature-pressure characteristics, reservoir diagenesis has larruping processes and traits. Through comparing two types of overpressure systems (self-source type and conduction type), confirmed by core and log, this paper illustrates their origin and hydrocarbon value, and sets forth the effects of high temperature and overpressure on reservoir qualities, which include: ① reservoir characteristics are mainly determined by sedimentary environment and diagenesis; ② high geotemperature gradient decreases sandstone porosity; ③ (overpressure) conserves parts of original porosity, which causes high porosity in a deep reservoir; ④ overpressure brings out much of secondary porosity in the processes of diagenesis; ⑤ fluid breakthrough causes cracks, which effectively increase reservoir permeability.
- anomalous pressure /
- reservoir characteristics /
- overpressure type /
- Yinggehai basin

HTML全文

图 1 莺歌海盆地分布及充填序列

Fig. 1. Distribution and filling sequences of the Yinggehai basin

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图 2 粒度、分选性与孔隙度、渗透率关系

Fig. 2. Correlation plot between granularity, divagation and porosity, permeability

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图 3 DF1-1构造区与Ya13-1构造区孔隙度演化对比

Fig. 3. Porosity evolution comparison between DF1-1 and Ya13-1 zones

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图 4 渗透率与孔隙度关系

Fig. 4. Porosity-permeability plot at different depths of LD15-1-1

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表 1 不同沉积环境下的碎屑岩物性

Table 1. Clast reservoir qualities in different sedimentary environments

表 2 LG20-1-1井沿岸砂坝岩石学特征

Table 2. Lithologic characteristics of shore sandstones in LG20-1-1 well

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