地学前缘 ›› 2011, Vol. 18 ›› Issue (4): 201-211.

• 论文 • 上一篇    下一篇

川东北地区台地边缘礁、滩气藏沉积与储层特征

郭彤楼   

  1. 中国石化勘探南方分公司, 四川 成都 610041
  • 收稿日期:2011-03-10 修回日期:2011-05-29 出版日期:2011-07-18 发布日期:2011-07-20
  • 作者简介:郭彤楼(1965—),男,博士,教授级高级工程师,主要从事构造与石油地质综合研究和勘探管理工作。E-mail:guotl.ktnf@sinopec.com
  • 基金资助:

    国家油气重大专项(2008CX05005003)

The characteristics of sedimentation and reservoirs of reefbeach gas fields in carbonate platform margins, Northeastern Sichuan Basin.

  1. SINOPEC Exploration Southern Company, Chengdu  610041, China
  • Received:2011-03-10 Revised:2011-05-29 Online:2011-07-18 Published:2011-07-20

摘要:

普光、元坝和龙岗等多个大、中型天然气田的发现,揭示了川东北地区长兴组—飞仙关组环开江—梁平陆棚东西两侧和城口—鄂西陆棚西侧台缘礁、滩带具有巨大油气勘探潜力。勘探实践证实不同部位台缘带的气藏特点及相关礁、滩沉积和储层特征均具有明显差异性。文中在层序地层学、沉积学和储层评价等研究基础上对这些差异性开展了分析工作。川东北地区长兴组—飞仙关组识别出两个三级层序,它们均由海侵和高位体系域构成,总体表现为水体向上变浅序列。研究区内不同部位的台缘带沉积和储层具有明显的差异,长兴期环开江—梁平陆棚东西两侧台缘地貌相近,铁厂河—普光—高峰场台缘带具加积为主、台缘斜坡陡、滩薄、生物礁发育的特点,上部白云岩化强;元坝—龙岗台缘带具前积和侧积明显、斜坡略缓、礁和滩均发育的特点,礁滩上部白云岩化强,孔隙型储层发育且物性较好;飞仙关期台缘不对称性明显,铁厂河—普光—高峰场台缘带仍以加积型为主,飞二段鲕滩发育,白云岩化强,孔隙型储层发育,具有储层厚度大和物性好的特点;元坝—龙岗台缘带飞二段发育鲕滩,但滩厚度薄、白云岩化弱,以孔隙型储层为主,储层物性略差。宣汉盘龙洞—见天坝长兴组台缘生物礁滩相及飞二段台缘鲕滩发育,白云岩化强,易于形成较好的储层。通过综合分析研究认为不同部位台缘带沉积及储层分布明显受同沉积古地貌、白云岩化强度、断裂、埋藏期成岩作用和流体活动等综合因素控制。

关键词: 台地边缘礁、滩, 层序地层学, 沉积, 储层, 川东北

Abstract:

The discovery of several large to mediumscale gas fields, such as Puguang gas field, Yuanba gas field, Longgang field etc., reveals that carbonate reefbeach zones have great petroleum exploration potential in the platform margin of the east and west sides of KaijiangLiangping shelf and the west side of ChengkouExi shelf. Previous exploration has confirmed that the characteristics of gas fields, sedimentation and reservoirs of reefbeach are obviously different in different parts of platform margins. However the regularity of the differences needs to be disclosed by further studies. Based on the study of highresolution sequence stratigraphy, sedimentology and reservoir evaluation, the paper analyzes the differences. Two thirdorder sequences have been identified which are shoaling upward, and all of them are composed of transgressive and highstand system tracts. It reveals that the characteristics of sedimentary facies and reservoirs are obviously different in different parts of platform margin. During the period of Changxing, the palaeogeomorphology of platform margins was similar in west and east sides of KaijiangLiangping shelf. The strata with main aggradational stacking patterns were strongly dolomitized at the top of Changxing Formation in TiechanghePuguangGaofengchang platform margin, which was the characteristics of steep ramp, thin sedimentation of beach and developing reef. And the YuanbaLonggang platform margin was characterized by gentle slope, obvious forest and lateral accretion stacking pattern, development both reef and beach, and stronger dolomitization at the top of reef and beach; porosity reservoir with good physical property was developed. In the period of Feixianguan, the asymmetry of the platform margins was clear. In TiechanghePuguangGaofengchang platform margin, the stacking pattern of stratigraphy was still aggradational, and thick oolitic beach with strong dolomitization was developed, and its porefractured type reservoir with good physical properties was developed in the second member of Feixianguan Formation. The YuanbaLonggang platform margin was developed thin oolitic beach with weak dolomitization in the second member of Feixianguan Formation, and the reservoir was typical of pore reservoir with poor physical property. The PanlongdongJiantianba platform margin grew reef and beach in Changxing Formation, and developed oolitic beach in the second member of Feixianguan Formation, both of them were strongly dolomitized and were easy to form available reservoirs. Through the comprehensive study of the characteristics of sedimentation and reservoir, we conclude that the sedimentation and the distribution of reservoir are obviously controlled by the integrated factors of synsedimentary palaeogeomorphology, dolomitization, faults, and the diagenesis and fluids in the burial period.

Key words: reef and beach in platform margin, sequence stratigraphy, sedimentation, reservoir, Northeastern Sichuan Basin

中图分类号: