SEDIMENTARY CHARACTERISTICS AND GEOLOGICAL SIGNIFICANCE OF SHALLOW SEA GRAVITY FLOW DEPOSITS IN THE GAS FIELD D, YINGGEHAI BASIN
-
摘要:
莺歌海盆地D气田发育浅海重力流沉积,目前对于其沉积微相组成及特征存在较大争议。通过总结研究区岩石相、测井相、地震相综合特征,结合国内外海底扇沉积单元划分,考虑靶区实际情况,建立了适合D区的浅海重力流沉积微相划分方案,识别出侵蚀水道、水道侧缘、分流水道、朵叶体等多种沉积微相;总结不同沉积微相特征,建立了浅海重力流沉积微相识别图版;并在浅海重力流沉积模式的控制下,精细刻画沉积微相,识别沉积微相平面展布,为气田开发实施奠定基础。
Abstract:Shallow sea gravity flow deposits are well developed in the Gas Field D of the Yinggehai Basin. So far the composition and characteristics of the sedimentary microfacies of the shallow sea gravity flow deposits have remained controversial. In this study, we summarized the characteristics of the lithofacies, logging facies and seismic facies of the field. A schematic classification of shallow-gravity flow microfacies suitable for the Gas Field D is established upon the known classifications of marine fan depositional systems both domestic and abroad in addition to the geological background of the target area. Sedimentary microfacies of erosional channel, channel side, distributary channel and depositional lobe are identified. Based on the above researches, this paper proposed an identification plate for shallow sea gravity flow deposits. According to the sedimentation model of the shallow submarine fan, the spatial distribution pattern of microfacies of the Gas Field D is confirmed.
-
-
图 6 D气田海底扇沉积模式(据文献[20]修改)
Figure 6.
-
[1] Catuneanu O,Abreu V,Bhattacharya J P,et al. Towards the stand-ardization of sequence stratigraphy[J]. Earth Science Reviews,2009,92(1):1-33.
[2] Weimer P, Statt R M.Introduction to the petroleum geology of deepwater settings[M].Tulsa: AAPG, 2007.
[3] 刘喜玲,刘君荣. 深水沉积及海底扇相模式研究进展[J]. 长江大学学报(自然科学版),2013,10(14):30-32,5.
[4] 孙国桐. 深水重力流沉积研究进展[J]. 地质科技情报,2015,34(3):30-36.
[5] Cummings J P,Hodgson D M. Assessing controls on the distribution of ichnotaxa in submarine fan environments, the Basque Basin, Northern Spain[J]. Sedimentary Geology,2011,239(3/4):162-187.
[6] 李胜利,于兴河,刘玉梅, 等. 水道加朵体型深水扇形成机制与模式:以白云凹陷荔湾3-1地区珠江组为例[J]. 地学前缘,2012,19(2):32-40.
[7] Picot M,Droz L,Marsset T,et al. Controls on turbidite sedimentation: Insights from a quantitative approach of submarine channel and lobe architecture (Late Quaternary Congo Fan)[J]. Marine and Petroleum Geology,2016,72:423-446. doi: 10.1016/j.marpetgeo.2016.02.004
[8] 陈 杨,张道军,黄 灿,等. 莺歌海盆地莺东斜坡南段梅山组大型海底扇沉积特征及控制因素[J]. 东北石油大学学报,2019,43(4):40-49, 7. doi: 10.3969/j.issn.2095-4107.2019.04.004
[9] 王 华,陈 思,甘华军,等. 浅海背景下大型浊积扇研究进展及堆积机制探讨:以莺歌海盆地黄流组重力流为例[J]. 地学前缘,2015,22(1):21-34.
[10] 黄银涛,姚光庆,周锋德,等. 莺歌海盆地黄流组浅海重力流砂体物源分析及油气地质意义[J]. 地球科学,2016,41(9):1526-1538.
[11] 钟泽红, 刘景环, 张道军, 等. 莺歌海盆地东方区大型海底扇成因及沉积储层特征[J]. 石油学报,2013,34(S2):102-111. doi: 10.7623/syxb2013S2012
[12] 裴健翔,陈 杨,郝德峰,等. 莺歌海盆地中央坳陷中新世海底扇识别及其形成控制因素[J]. 东北石油大学学报,2016,40(5):46-54, 7. doi: 10.3969/j.issn.2095-4107.2016.05.006
[13] 郇金来,漆 智,杨朝强,等. 莺歌海盆地东方区黄流组一段储层成岩作用机理及孔隙演化[J]. 地质科技情报,2016,35(1):87-93.
[14] 漆 智, 吴 倩, 郇金来. 东方1-1气田黄流组一段储层沉积相研究[R]. 湛江: 中海石油(中国)有限公司湛江分公司, 2011.
[15] 周世明, 张建营, 曹 明, 等. 致密砂岩气藏沉积微相识别方法与划分标志的探讨[J]. 科技创新与应用,2016(7):165.
[16] 刘秀明,罗 祎. 粒度分析在沉积物研究中的应用[J]. 实验技术与管理,2013,30(8):20-23. doi: 10.3969/j.issn.1002-4956.2013.08.007
[17] 宋子齐,潘 艇,程 英,等. 利用测井曲线研究沉积微相及其含油有利区展布[J]. 中国石油勘探,2007,12(4):37-41, 7. doi: 10.3969/j.issn.1672-7703.2007.04.008
[18] 陈方鸿,王树平,李志政. 三维可视化地震相分析在沉积相研究中的应用[J]. 石油勘探与开发,2005,32(3):73-75. doi: 10.3321/j.issn:1000-0747.2005.03.018
[19] 杨玉峰. 利用测井和三维地震资料综合进行沉积相研究——以迈陈凹陷徐闻地区涠洲组为例[D].武汉: 长江大学, 2015.
[20] 王 玉,漆 智,杨朝强,等. 浅海重力流储层沉积模式新认识[J]. 地质科技情报,2019,38(4):16-22.
-