SEDIMENTARY CHARACTERISTICS OF A NEAR-SOURCE STEEP SLOPE DELTA AND THEIR CONTROL OVER OIL ACCUMULATION: AN EXAMPLE FROM SHA-4 FORMATION, KL OIL FIELD IN LAIZHOU BAY DEPRESSION
-
摘要:
针对KL油田沙四段扇三角洲巨厚砂砾沉积体优势储层认识不清的问题,利用丰富的井壁取心、薄片、扫描电镜等资料,系统研究莱州湾凹陷南斜坡KL油田沙四段扇三角洲沉积特征,并对形成储层控制因素及储集空间类型进行了探讨。结果表明:沙四段为暖温带干旱背景下的退积型扇三角洲沉积,发育平原和前缘亚相,岩性自下向上发育棕褐色砂砾岩、凝灰质含砾砂岩、杂色含砾砂岩、灰色粗砂岩,局部夹薄层凝灰岩;岩石成分主要为石英、长石以及火山岩碎屑,填隙物以泥质、凝灰质为主,可见白云石。同时发现沉积作用和成岩作用共同控制该套沉积体有效储层形成,扇三角洲前缘沉积的含砾砂岩和粗砂岩分选较好,粒间孔发育,成岩期溶蚀作用改善储集空间效果明显,孔隙类型主要为粒间孔,其次是溶蚀孔;扇三角洲平原沉积的砂砾岩分选极差,粒间孔不发育,溶蚀作用效果差,又受压实作用、胶结交代作用等影响,储集空间变差。指出了南斜坡带沉积体优势储层的分布规律,认为扇三角洲前缘沉积的杂色含砾砂岩为有效储层的主体,是今后勘探评价的重点。
Abstract:Sedimentary characteristics of a fan delta in the 4th Member of the Shahejie Formation located on the south slope of the Laizhou Bay Depression are studied, aiming at finding out the major reservoir of the fan-delta sand of the KL Oilfield. Data of wall sample, thin slice and scanning electron microscope are used for the purpose. Reservoir controlling factors and reservoir space types are also discussed. Results suggest that the fan delta was a retrogressive one developed in a warm and dry climate, consisting of brown conglomerate, green gray tuffaceous gravel sandstone, colored gravel sandstone, and gray coarse sandstone from the bottom up, with thin layers of tuffs locally. Clastic components including quartz, feldspar and volcanic rock debris are cemented by muddy, tuffaceous, and dolomitic interstitial materials. Both the deposition and diagenesis control the formation of reservoir. Gravel sandstone and coarse sandstone deposited in the fan delta front are well sorted, and their pores are dominated by the type of intergranular, followed by dissolution pores. The diagenetic dissolution can improve the reservoir space obviously. The fan-delta plain sediments, however, are poorly sorted with less intergranular pores. The dissolution effect is not well developed under heavy compaction, instead, the accumulation space is further deteriorated. Based upon the distribution pattern of the deposits on the southern slope, it is concluded that the gravel sandstone deposited in front of the fan delta is the most effective reservoir and exploration target.
-
Key words:
- Laizhou Bay /
- near-source steep slop /
- fan delta /
- sandstone /
- controlling factor
-
-
表 1 KL油田沙四段岩性命名原则
Table 1. Lithology classification and nomenclature
岩石类别 命名原则(粒度+特殊成分) 岩石名称 粒度 特殊成分 粒径/mm 含量 成分 含量 砂岩 0.5~1.0 >50% - 粗砂岩 0.25~2.0 25%~50%且C0.5~1.0 mm > C0.25~0.5 mm - 含砾砂岩 2.0~4.0 10%~25% 0.25~2.0 >50% 凝灰质 25%~50% 凝灰质含砾砂岩 2.0~10.0 10%~25% 砾岩 0.25~2.0 25%~50%且C2.0~30.0 mm > C0.25~2.0 mm - 砂砾岩 2.0~30.0 -
[1] Holmes A. Principle of physical geology[M]. London: Thomas Nelson and Sons, 1965: 288.
[2] 张昌民, 朱锐, 尹太举, 等.扇三角洲沉积学研究进展[J].新疆石油地质, 2015, 36(3):362-367. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjsydz201503023
[3] 张春生, 刘忠保, 施冬, 等.扇三角洲形成过程及演变规律[J].沉积学报, 2000, 18(4):522-525. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb200004007
[4] 邹妞妞, 史基安, 张大权, 等.准噶尔盆地西北缘玛北地区百口泉组扇三角洲沉积模式[J].沉积学报, 2015, 33(3):607-614. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201503019
[5] 孙龙德.东营凹陷北部斜坡带沙三—四段砂砾岩体与油气聚集[J].沉积学报, 2003, 21(2):278-282. doi: 10.3969/j.issn.1000-0550.2003.02.014
[6] 陈全红, 李可永, 张道锋, 等.鄂尔多斯盆地本溪组—太原组扇三角洲沉积与油气聚集的关系[J].中国地质, 2010, 37(2):421-428. doi: 10.3969/j.issn.1000-3657.2010.02.015
[7] 管红, 朱筱敏.南堡凹陷东营组层序地层格架与沉积体系[J].沉积学报, 2008, 26(5):731-735. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb200805003
[8] 刘志飞, 王成善.西藏日喀则地区早白垩世恰布林组辫状河—扇三角洲沉积[J].沉积学报, 1998, 16(3):6-12. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800006543
[9] 李文厚.塔西南坳陷侏罗系的扇三角洲沉积[J].沉积学报, 1998, 16(2):150-153. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800006539
[10] 史基安, 何周, 丁超, 等.准噶尔盆地西北缘克百地区二叠系沉积特征及沉积模式[J].沉积学报, 2010, 28(5):962-967. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cjxb201005013
[11] 黄雷, 王应斌, 武强, 等.渤海湾盆地莱州湾凹陷新生代盆地演化[J].地质学报, 2012, 86(6):867-875. doi: 10.3969/j.issn.0001-5717.2012.06.002
[12] 刘志刚, 杜晓峰, 王清斌, 等.渤海海域旅大21_A构造沙四段储集层特征及控制因素[J].海洋石油, 2012, 32(2):26-29. doi: 10.3969/j.issn.1008-2336.2012.02.026
[13] 刘志刚, 周心怀, 李建平, 等.渤海海域石臼坨凸起东段36- 3构造古近系沙二段储集层特征及控制因素[J].石油与天然气地质, 2011, 32(54):832-838. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=syytrqdz201106004
[14] 孟元林, 李亚光, 牛嘉玉, 等.渤海湾盆地北部深层碎屑岩储层孔隙度影响因素探讨[J].中国海上油气, 2007, 19(3):154-156. doi: 10.3969/j.issn.1673-1506.2007.03.003
[15] 张友, 侯加根, 李娜, 等.黄骅坳陷塘34断块古近系沙河街组一段下部储集层特征及控制因素[J].古地理学报, 2012, 14(3):383-392. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201203012
[16] 斯春松, 寿建峰, 王少依, 等.鄂尔多斯盆地中部上古生界砂(砾)岩储集层孔隙成因及控制因素[J].古地理学报, 2012, 14(4):533-542. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gdlxb201204011
[17] 蒋凌志, 牛嘉玉, 张庆昌, 等.渤海湾盆地深部有利储层发育的主控因素[J].地质评论, 2009, 55(1):75-78. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200901008
[18] 沈卫兵, 庞雄奇, 张宝收, 等.塔中地区碳酸盐岩与碎屑岩储层物性差异及主控因素[J].高校地质学报, 2015, 21(1):138-146. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb201501014
-