乌克兰喀尔巴阡山脉古新世矿床:地质和岩相特征、储层性质

Pub Date : 2020-12-28 DOI:10.5200/baltica.2020.2.1
H.Ya. Havryshkiv, N. Radkovets
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引用次数: 2

摘要

古新世亚姆纳组是喀尔巴阡山石油省乌克兰部分的主要含油序列之一。乌克兰喀尔巴阡山脉的Boryslav Pokuttya和Skyba单元有大量石油聚集。在研究区的大部分地区,Yamna组由厚的浊积砂岩层组成,起着油气藏的作用。根据测井数据、岩性和岩相调查对古新世复理石矿床的沉积环境进行的重建表明,陆源物质从两个来源供应到沉积盆地。其中一个位于研究区西北部,以粗粒砂质沉积物为主。来源于其中部的碎屑显示出粘土泥和细粒砂屑物质的优势。古新世序列中陆源物质分布的特殊性使我们能够挑选出砂岩、粉砂岩和泥岩发育最大(占总剖面的50%以上)的四个区域。在这四个地区进行的岩相学调查和对Yamna组岩石储层性质的估计,为研究区域内的碳氢化合物进一步勘探工作确定了优先方向。
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Paleocene deposits of the Ukrainian Carpathians: geological and petrographic characteristics, reservoir properties
The Paleocene Yamna Formation represents one of the main oil-bearing sequences in the Ukrainian part of the Carpathian petroleum province. Major oil accumulations occur in the Boryslav-Pokuttya and Skyba Units of the Ukrainian Carpathians. In the great part of the study area, the Yamna Formation is made up of thick turbiditic sandstone layers functioning as reservoir rocks for oil and gas. The reconstructions of depositional environments of the Paleocene flysch deposits performed based on well log data, lithological and petrographic investigations showed that the terrigenous material was supplied into the sedimentary basin from two sources. One of them was located in the northwest of the study area and was characterized by the predominance of coarse-grained sandy sediments. Debris coming from the source located in its central part showed the predominance of clay muds and fine-grained psammitic material. The peculiarities of the terrigenous material distribution in the Paleocene sequence allowed singling out four areas with the maximum development (> 50% of the total section) of sandstones, siltstones and mudstones. The performed petrographic investigations and the estimation of reservoir properties of the Yamna Formation rocks in these four areas allowed establishing priority directions of further exploration works for hydrocarbons in the study territory.
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