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HYDROCARBON SYSTEMS OF THE BLACKSEA REGION

机译:黑海地区的油气系统

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Hydrocarbon systems of the Black Sea region are represented by oil and gas fields, gasaccumulation in the sea water, huge gas outburst from the sea bottom, gas hydrate shows andwide distribution of mud volcanoes in the deep parts of the sea. New data on gas-bearing ofthe Black Sea area and correlation with results of geological exploration of gas hydratedeposits of different regions permit to revise gas hydrate reserves and consider the Black Seaas one of the richest gas hydrate region of the world. According to the latest calculation thereserves of hydrate methane of the Black Sea area are appreciated up to 1,330 trilllion m3The first commercial oil in the Black Sea region was discovered in the eighties byRomanian geologists in the fields Lebada West, Lebada East and Sinoe. In the Ukrainian partof the Black Sea no oil fields have been found in the meanwhile. Slight oil shows wereencountered in 2001 in the well Olimpiyska 400 during the testing of the Lower Paleocenearenaceous limestone. Main discoveries of commercial gas in the Black Sea were made byUkrainian geologists detected 8 fields (Golitsyne, Southern Golitsyne, Shmidt, Stormove,Crimean, Arkhangelske, Odessa, Bezimenne on the northern shelf. By ones gas field wereascertained on the Romanian (Doina) and Bulgarian shelf (Galata) [Fig. 1]Till present exploration for gas and oil in the Black Sea was concentrated at shallow depthnot more than 90 m. All gas fields in the Ukrainian part of sea have been discovered on thenorth-western shelf; whereas deep part of the sea remains unexplored. The latest geologicaland geophysical data indicate that the deep part of the Black Sea is of great possibilities.Therefore much attention must be concentrated on abyssal part of the Black Seas. Especiallyas the sea is comparatively shallow with maximum depth of 2200 m.The Black Sea is the most gas-polluted sea in the world. Its waters contain hydrogensulphide beginning from the depth of 110-130m in the central part and 150-170 m along itsperiphery up to the bottom. Concentration of hydrogen sulphide in the Black Sea watersamounts 420 μM or 2 billion tons of sulphur. The presence of hydrogen sulphide in theBlack Sea makes its water toxic, lifeless. There are no living creatures in these waters and thiszone is dead.
机译:黑海地区的油气系统以油气田,天然气为代表 积聚在海水中,海底有巨大的瓦斯突出物,天然气水合物显示出 海深处的泥火山分布广泛。关于含气量的新数据 黑海地区天然气水合物的地质勘探结果及其相关性 不同地区的矿床允许修改天然气水合物储量并考虑黑海 作为世界上最丰富的天然气水合物地区之一。根据最新计算 黑海地区的水合物甲烷储量最高可升至1,330 trilllion m3 黑海地区的第一批商业石油是在80年代被发现的 西部的Lebada,东部的Lebada和Sinoe领域的罗马尼亚地质学家。在乌克兰部分 在此期间,没有发现黑海油田。稍有油展 在下古新世的测试中,于2001年在Olimpiyska 400井中遇到 砂质石灰石。黑海的主要商业天然气发现是由 乌克兰地质学家发现了8个油田(Golitsyne,South Golitsyne,Shmidt,Stormove, 北部架子上的克里米亚半岛,阿尔汉格尔斯克群岛,敖德萨,贝济明讷。气场被 确定在罗马尼亚(多伊纳)和保加利亚架子(加拉塔)上[图。 1] 直到目前,黑海的天然气和石油勘探都集中在浅层深度 不超过90 m。乌克兰海上部分的所有气田均已在该地区发现。 西北大陆架;而深海尚未开发。最新地质 地球物理数据表明,黑海深处的可能性很大。 因此,必须将大量注意力集中在黑海的深渊部分。尤其 由于海洋相对较浅,最大深度为2200 m。 黑海是世界上污染最严重的海洋。它的水含有氢 硫化物从中部110-130m的深度开始,沿中部150-170 m的深度开始 外围直到底部。黑海水域中的硫化氢浓度 排放量为420μM或20亿吨硫。硫化氢的存在 黑海使水有毒,无生气。这些水域中没有活物,而这 区域已死。

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