三门峡盆地灵宝凹陷古近系小安组油气成藏条件及勘探方向
Hydrocarbon accumulation conditions and exploration direction of Paleogene Xiao''an formation in Lingbao sag, Sanmenxia basin
投稿时间:2026-04-09  修订日期:2026-05-31
DOI:
中文关键词:  古近系小安组  烃源岩  储集层  油气成藏条件  勘探方向  三门峡盆地
英文关键词:Paleogene Xiao''an Formation  hydrocarbon source rock  reservoir bed  hydrocarbon accumulation condition  exploration direction  Sanmenxia Basin
基金项目:河南省地质勘查“三门峡盆地油气资源接续基地调查评价(河南部分)”、河南省自然资源厅2025年度省自然资源科技创新“揭榜挂帅”项目“河南省中小盆地油气成藏条件潜力研究”(项目编号:豫自然资函〔2025〕456号-6)、河南省地质局局管地质科研项目“三门峡盆地油气成藏条件及勘探潜力分析”(任务书编号:豫地科研〔2025〕1号)联合资助。
作者单位邮编
刘俊 河南省地质局矿产资源勘查中心 450000
沈阳* 河南省地质局矿产资源勘查中心 450000
郭大伟 河南省地质局矿产资源勘查中心 
赵民 河南省地质局矿产资源勘查中心 
陈畅然 河南省地质局矿产资源勘查中心 
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中文摘要:
      三门峡盆地隶属于南华北盆地豫西隆起区,是一个以新生界为主的小型断陷盆地。早期研究认为,该盆地不具备烃源岩发育的地质条件,一直未取得油气勘探突破,整体勘探程度较低。近期,古近系油气勘探取得重要突破,多口探井试获高产工业油流,展现出良好的油气勘探前景。研究以野外露头、地震、钻井及分析测试资料为基础,系统分析油气成藏条件,总结成藏主控因素与成藏模式,评价勘探潜力。研究结果表明,盆地古近系坡底组与小安组下部发育咸化湖相优质烃源岩,整体处于生烃演化有利阶段;小安组三角洲成因砂体为优势储集体,以中孔中渗储层为主,储集物性优良。油气主要沿断裂-砂体复合输导体系向构造高部位运移聚集,以下生上储成藏组合为核心,成藏过程受控于烃源岩品质、储层发育规模及圈闭有效性三大关键因素。研究建立了“咸化湖相深凹多源供烃,断层–砂体复式输导,构造–岩性复合聚集成藏”的成藏模式。古近系小安组为盆地常规油气主力勘探层系,柳林河组具备接替勘探价值,深层同时具备页岩油气、致密砂岩油气非常规勘探潜力;灵宝凹陷生储盖及圈闭配置条件最优,为当前重点勘探层系,阳平凹陷、潼关凹陷与灵宝凹陷地质成藏条件相似,外延勘探空间广阔。强化地震勘探与钻井工程部署、深化成藏规律研究,可推动盆地常规与非常规油气勘探实现战略性突破。
英文摘要:
      The Sanmenxia Basin, which is subordinate to the Western Henan Uplift of the Southern North China Basin, is a small fault-depression basin dominated by the Cenozoic erathem. Early studies indicated that this basin lacks the necessary geological conditions for source rock development, leading to no breakthroughs in petroleum exploration and an overall low exploration intensity. Recently,important breakthroughs have been made in the Paleogene oil and gas exploration of the basin. Multiple exploration wells have obtained high-yield industrial oil flows, showing promising oil and gas exploration prospects. Based on field outcrop data, seismic data, drilling data and laboratory test results, this study systematically analyzes the hydrocarbon accumulation conditions, summarizes the main controlling factors and accumulation models of oil and gas, and evaluates the exploration potential.The research results show that high-quality saline lacustrine hydrocarbon source rocks are developed in the Podi Formation and the lower part of the Xiao’an Formation of the Paleogene in the basin, which are generally in a favorable stage of hydrocarbon generation and evolution. Deltaic sand bodies of the Xiao’an Formation serve as the dominant reservoir bodies, which are mainly medium-porosity and medium-permeability reservoirs with favorable reservoir physical properties. Oil and gas migrate and accumulate towards structural highs mainly along the composite fault-sandbody migration system. The hydrocarbon accumulation is dominated by the lower-generation and upper-accumulation assemblage, and the accumulation process is controlled by three key factors: source rock quality, reservoir development scale and trap effectiveness.This study establishes a hydrocarbon accumulation model summarized as multi-source hydrocarbon supply in deep sags of saline lacustrine facies, compound migration controlled by faults and sandbodies, and composite hydrocarbon accumulation of structural-lithologic traps. The Paleogene Xiao’an Formation is the main exploration interval for conventional oil and gas in the basin, and the Liulinhe Formation has important replacement exploration value. The deep strata also hold great exploration potential for unconventional shale oil and gas as well as tight sandstone oil and gas. The Lingbao Basin possesses the optimal matching conditions of source-reservoir-cap assemblages and traps, and is the key exploration area at present. The Yangping Sag and Tongguan Sag have similar geological and hydrocarbon accumulation conditions to the Lingbao Sag, with broad space for expanded exploration. Strengthening seismic exploration and drilling engineering deployment and deepening the research on hydrocarbon accumulation laws can promote strategic breakthroughs in conventional and unconventional oil and gas exploration in the Sanmenxia Basin.
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