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山东东营凹陷新近系为揭示中国东部新生代浅部地层水化学场响应
陈中红 2014-1-4 18:12
陈中红 , 等 . 东营凹陷新近系地层水化学场及油气意义 . 古地理学报 ,2012,14(5):685-693 为揭示中国东部新生代浅部地层水化学场响应及油气意义,在东营凹陷新近系试油资料统计分析的基础上,对东营凹陷新近系的水化学场特征进行了研究。结果表明,与东营凹陷古近系沙河街组三段与四段封闭性滞留型水化学场特征明显不同,东营凹陷新近系馆陶组和明化镇组总体以低矿化度的 NaHCO 3 型地层水为主体(矿化度小于 5g /L )。其 水化学剖面宏观上具有一定的分带性 , 大致可以划分为 3 种水文环境 : 以强开放性水文流畅带 ( 地表到 0.7 km ) 、弱开放性水文阻滞过渡带 (0.7~1.1 km) 和相对封闭性水文迟缓带 (1.1 km 以下 ) ,在不同的水化学作用带,水岩作用和地层水矿化度、离子和离子参数具有不同的响应。东营凹陷新近系 Ca 相对海水富集 (Ca excess ) 和 Na 相对海水亏损 (Na deficient ) 的定量关系 Ca excess ≤0.2367Na deficient -0.6261 ,显示出明显的钠亏损特征,钙富集量也远低于世界盆地 流体线 (Basin Fluid Line, BFL 所代表的富集量,与同凹陷古近系沙三、沙四段封闭性水文地质系统中钠相对富集特征也明显不同,反映了地层水蒸发浓缩作用弱及与地表水交替活动强烈的水文地质作用特征。地层水化学场的分布影响了原油密度和天然气的分布规律,使得东营凹陷新近系原油密度、与天然气相对密度在剖面上的分布规律与地层水分带性有良好的一致性。
个人分类: 科研成果|4252 次阅读|0 个评论
断陷湖盆超压分布与油气成藏(石油学报)
陈中红 2009-2-11 16:56
详文见:石油学报, 2008 , 29 ( 4 ): 509-515 断陷湖盆超压分布与油气成藏 陈中红  等  渤海湾盆地沾化凹陷古近系的超压在渤南洼陷和五号桩洼陷的沙三段中下亚段大套泥岩和沙四段灰色膏盐岩段中分布 , 但在不同层位超压分布略有差别 ; 常压低压系统发育于上部层段 , 剖面上形成二元结构。从埋深上看 , 2 500 m 以上地层基本为常压或低压 , 2 500 m 以下地层开始出现较明显的压力异常。沾化凹陷超压系统对应主力烃源岩系沙三中、下亚段及沙四上亚段 , 生烃作用是超压的重要成因 , 但超压对生烃的抑制作用不明显。超压体系构成了准封闭的超压封存箱型自源油气成藏动力学系统 , 同时也通过幕式排放为浅层的新近系及古近系的沙三段上亚段东营组常压开放性它源油气成藏动力学系统提供油源及成藏动力。 断裂是超压体系泻压的重要渠道 , 也是油气幕式排放的主要途径 , 与断裂沟通的砂岩体及背斜构造是有利的勘探目标 , 超压泥岩体 周围的透镜状砂体是潜在的目标。 关键词 : 沾化凹陷 ; 断陷湖盆 ; 超压系统 ; 流体流动机制 ; 断裂 ; 油气成藏 Distribution characteristics of overpressure and its controll ing to hydrocarbon accumulation in terrigenous faulted basin CHEN Zhonghong   et al ( Facul t y of Geo - Resources and I nf ormation , China Uni veristy of Pe roleum , Dongying 257061 , China) The overpressure in Zhanhua Sag of Bohai Bay Basin was dist ributed in the large series of mud in the middle and lower part s of the third member of Shahejie Formation and gypsum - salt rock in the forth member of Shahejie Formation. The dist ribution of overpressure in the various formations was different . There formed the binary st ructure on the section. The normal - compaction or normal - pressured (low pressured) system was formed at the formation above 2 500 m in depth, and the over - pressured system was formed at the formation below 2 500 m. The over - pressured system corresponds to the main source rocks. Hydrocarbon generation was an important mechanism for genesis of the overpressure system , but the suppression of overpressure on the hydrocarbon generation was not obvious. There are two kinds of fluid dynamics systems in Zhanhua Sag, including the normal - pressured opening fluid-dynamics system and over - pressured fluid - dynamics system , which result in two types of accumulation dynamic mechanisms. One is the self - sourced and sealed dynamic mechanism, and the other is the outward - sourced and opened mechanism. The former provided the oil - gas source and reservoir - forming driver for hydrocarbon accumulation. Fault s and ruptures are important pathways for episodic hydrocarbon - expulsion. So the sandstone - bodies communicated by faults and anticlines are the favorable prospect s for exploration, and the sand lens reservoirs around the over - pressured source rocks are the latent target s for the exploration of subtle t rap reservoirs. Key words : Zhanhua Sag ; faulted basin ; overpressure system; fluid flow mechanism; fault ; hydrocarbon accumulation Chen Zhonghong, Zha Ming. Distribution characteristics of overpressure and its controlling to hydrocarbon accumulation in terrigenous faulted basin. Acta Petrolei Sinica , 2008,29(4):509-515 (in Chinese)
个人分类: 科研成果|3989 次阅读|0 个评论

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