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柴西南区岩性油气藏地质特征及控制因素OA北大核心CSTPCD

Geological characteristics and controlling factors of lithologic reservoirs in southwestern Qaidam Basin

中文摘要英文摘要

近年来,柴达木盆地在咸化湖相滩坝砂中发现了多个"小而肥"的岩性油气藏.为了拓展岩性油气勘探规模、发现新的目标及区带,支撑油田规模增储上产,利用岩心、测井和地震资料,开展岩性油气藏成藏条件综合分析.通过解剖已发现岩性油气藏特征,明确控制因素,指出了岩性油气藏勘探接替领域.结果表明,柴西南区具备形成岩性油气藏的四大有利条件:一是发育继承性的七个泉—红柳泉、砂西—跃进、扎哈泉—乌南三大稳定的古斜坡,利于油气聚集成藏;二是临近红狮和扎哈泉两个生烃中心,油源条件优越;三是咸化湖盆发育大型辫状河三角洲、广覆式分布的滨浅湖滩坝砂及藻席—灰云坪沉积,形成碎屑岩和碳酸盐岩两种互补型的储集体;四是发育多种疏导体系,纵向上可以形成多套含油层系.受古构造、沉积、成岩等多因素控制,柴西南区发育砂岩上倾尖灭型、砂岩透镜体型、物性封堵型和白云石化成岩圈闭四种类型岩性油气藏.岩性油气藏受古构造、优质源岩和有效储层三因素控制.古构造决定岩性圈闭的类型和油气运移方向;优质烃源岩控制岩性油气藏的分布及规模;有效储层控制岩性油气藏的富集.综合评价指出,辫状河三角洲前缘砂体是古近系下干柴沟组下段岩性勘探的有利区,主要分布在砂西、尕斯、乌南向盆内的倾末端;白云石化成岩圈闭是古近系下干柴沟组上段岩性勘探的有利区,主要分布在环红狮凹陷周缘;广覆式分布滩坝是新近系上干柴沟组、下油砂山组岩性油气藏勘探的有利区,主要分布在英雄岭、尕斯、扎哈泉、乌南等地区.这一认识支撑了切探 2 井、尕斯新层系等岩性勘探获得一系列重大突破,可为柴西南区岩性油气藏的下一步勘探提供指导.

In recent years,several small and rich lithologic oil and gas reservoirs have been discovered in the saline lacustrine beach bar sand in the Qaidam Basin.In order to expand the exploration scale of lithologic oil and gas reservoirs,find new exploration targets and zones,and increase storage and production of oilfields,based on coring,logging and seismic data,the controlling factors of oil and gas accumulation in lithologic reservoirs are defined,and some exploration succeeding fields of lithologic reservoirs are pointed out.The results show that:The southwestern Qaidam Basin has four favorable conditions for the formation of lithologic reservoirs.The first is the development of three stable ancient slopes,namely,the Qigequan-Hongliuquan,Shaxi-Yuejin,and Zahaquan-Wunan,which are inherited and conducive to the accumulation of oil and gas.The second is the proximity of two hydrocarbon generation centers,Hongshi and Zahaquan,with superior oil source conditions.The third is that the salt lake basin developed large braided river delta,widely distributed shoal-bar sand and algal hill-gray cloud flat deposits,forming two complementary types of reservoirs of clastic rock and carbonate rock.The fourth is the development of a variety of drainage systems,which can form several sets of oil-bearing strata vertically.Controlled by paleo-structural,sedimentary and diagenetic factors,there are four types of lithologic reservoirs in the southwestern Qaidam Basin:updip pinching out,sandstone lens,physical sealing and dolomitization trap.Lithologic reservoirs are controlled by three factors:paleo-structure,high-quality source rock and effective reser-voir.Paleo-structure determines the type of lithologic traps and the direction of hydrocarbon migration.The high-quality source rock controls the distribution and scale of lithologic reservoirs and effective reservoir controls the accumulation of lithologic reservoirs.Comprehensive evaluation shows that the braided river delta front sand body is a favorable area for the exploration of lithologic reservoirs in the lower Ganchaigou Formation of the Lower Paleogene,mainly distributed in the basin dip end of Shaxi,Gasi,and Wunan.The dolomitization trap is a favorable area for exploration of lithologic reservoirs in the upper member of lower Ganchaigou Formation of Paleogene,mainly distributed around the Hongshi Sag.The widely distributed beach bar is a favorable area for lithologic oil exploration in the upper Ganchaigou Formation and lower Youshashan Formation of Neogene,mainly distributed in Yingxiongling,Gasi,Zhahaquan,Wunan,and other areas.This understanding supports a series of major breakthroughs in lithologic exploration,such as well Qietan 2 and the new series of Gasi,with important guiding significance for further exploration of lithologic reservoirs in the southwestern Qaidam Basin.

吴颜雄;薛建勤;施奇;杨芸;刘君林;马凤春;李翔;王艳清

青海省高原咸化湖盆油气地质重点实验室,甘肃 敦煌 736202||中国石油 青海油田分公司,甘肃 敦煌 736202中国石油 青海油田分公司,甘肃 敦煌 736202中国石油 勘探开发研究院 西北分院,兰州 730020中国石油 杭州地质研究院,杭州 310023

石油、天然气工程

成藏条件控制因素岩性油气藏勘探潜力柴达木盆地

reservoir formation conditioncontrolling factorlithologic reservoirexploration potentialQaidam Basin

《石油实验地质》 2024 (001)

22-31 / 10

国家科技重大专项(2016ZX05046-006)和中国石油天然气股份有限公司重大科技专项(2016E-01)联合资助.

10.11781/sysydz202401022

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