Source-Reservoir-Cap Rock Association within Sequence Framework and Its Exploration Significance
-
摘要: 在层序地层研究基础上,结合右江盆地油气勘探成果,建立了右江盆地层序地层格架与油气生储盖组合之间的关系模型。具体是以南盘江凹陷及十万大山地区为重点,通过泥盆纪—中三叠世层序地层中生储盖组合的研究,阐述相应的不同级别层序格架 (二级及三级 )中储集体的成因类型及时空分布规律,进而探讨不同成因层序中有利储集体的发育模式。Abstract: Based on the sequence stratigraphy, in conjunction with the res ult of petroleum exploration, the correlation model of sequence stratigraphic framewor k and oil & gas source-reservoir-cap rock association has been established. Em phasi zed on Nanpanjiang depression and Shiwandashan basin, this paper deals with the genetic type and distribution pattern of source-reservoir-cap rock strata with in different hierarchies of sequence stratigraphic frameworks in the Youjiang Basin, and then discusses on their genesis and development model. Various sequence frameworks in different genetic basins contain different hydr ocarbon prospects. In general, transgressive system tracts (TST), condensed sec t ion (CS), highstand system tracts (HST) and lowstand system tracts (LST) of inte rplatform basin, deep-water basin are generally impo rtant source rocks and significant cap rocks, and coal-bearing carbonate formations of hi ghstand system tract in cratonic basin and carbonate platform. Highstand system tracts and lowstand system tracts in cratonic basin and carbon ate platform are important reservoins,and karst reservoir is developped along s equence boundary.Reservoirs maimly include all kinds of favoura ble sandbodies within different system tracts:①basin floor and slope fans, del ta front, alluvial fan, channel sandbodies, progradation complex, shoal-bioher m -reef complex, calcareous and mixed clastic turbidites within lowstand system tract; ②sandbodies of barrier beach, shoal, estuary, tide-controlled delta, fandelt a, turbidity fan, lag sediment, bioherm-reef complex, pyroclast turbidite withi n transgressiue system tract; ③river and wave dominated deltatic sandbodies, a lluvial-fan-channel sandbodies, fandelta, turbidity fan, terrigenous and car bonate shales, bioherm-reef complex, calcareous-clastic beach-bioherm-reef complex, calcareous clastic turbidite and dolostone within highstand system tra ct; and ④paleokarst reservoir dominated by sequence boundary.
-
Key words:
- petroleum exploration /
- sequence stratigraphy /
- You jiang Basin
-
[1] Chen Hongde, Qin Jianxiong,Tian Jingchun.Perm ian sequence stratigraphy of Sichuan-Yunnan-Guizhou-Guangxi Region[J] . Scie ntia Geologica Sinica. 1997,6(3): 241~261 [2] Chen Hongde, Qin Jianxiong,Tian Jingchun.Permian sed imentary basins and regional sedimentary models the Sichuan-Yunnan-Guizhou-Gu angxi region and correlation of sea level changes[J] . Scientia Geologica sinic a.1997,6(3): 283~292 [3] Tian Jingchun, Chen Hongde, Qin Jianxiong. Sequencce-based lithofaci es paleogeography of Permian in Sichuan-Yunnan-Guizhon-Guangxi Region[J] . Scientia Geologica Sinica.1997,6(3): 262~282 [4] 覃建雄,曾允孚,陈洪德,田景春. 西南地区二叠纪层序地层与海平面变化[J ] . 岩相古地理.1998,18(1):19~35 [5] Qin Jianxiong, Chen Hongde, Tian Jingchun. Reef and gravity flow sedi ments on Permian slopes in the Sichuan-Yunnan-Guizhon-Guangxi Region[J] . S cientia Geologica Sinica. 1997,6(3): 203~298 [6] 覃建雄. 四川西昌盆地早二叠世层序地层研究[A] . 见:油气地质学进展[C] . 成都:四川科技出版社.1996.15~21
计量
- 文章访问数: 560
- HTML全文浏览量: 5
- PDF下载量: 396
- 被引次数: 0