GAS CHIMNEYS IN THE NW BLACK SEA NEAR THE KALANCHAK PALEOBRIVER

Y. Shnyukov, Y. Inozemtsev, O. Rybak, O. Parishev, L. Stupina
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Abstract

The publication is based on a large body of data on gas outcrops in the northwest of the Black Sea, and in particular, the paleo-Kalanchak area. The material was obtained during the voyages carried out on the R/V of the Department of Marine Geology and Sedimentary Ore Formation of the National Academy of Sciences of Ukraine, as well as data from literary sources. More than 3000 methane sips were identified in the study area. The vast majority of gas emissions in the area of paleo-river Kalanchak, as well as in other areas of the northwestern sector of the Black Sea, is confined to the upper part of the continental slope and the adjacent area of the shelf. Practically it is a band 45 km wide on both sides of the shelf edge. Seismic and acoustic profiles were studied in this article. Their analysis indicates that gas chimneys are not distributed randomly but concentrated in specific locations. A certain relationship between the spatial distribution of methane outcrops on the seafloor and geomorphological structures, as well as tectonic structure, primarily faults is traced. Gas chimneys are associated with various forms of seafloor topography, but their greatest number is located at the mouths of paleo-river canyons. The article provides more detailed geomorphological information of the paleo-river network of the NW Black Sea. In the estuarine canyon, gas emissions form along the sedimentary ridges, gas chimneys appear at the bottoms of canyons, their peripheries, or near the dumps of submarine landslides, where the sedimentary cover is disturbed by mass transport. On the shelf, the greatest concentration of gas chimneys is found in circular and elongated depressions (pockmarks). Based on the study of acoustic profiles, gas chimneys of the Paleo-Kalanchak part of the Black Sea were classified according to a few features: the depth of location, height of gas release, gas flow capacity, form of gas release, mode of operation. The results of the research are also presented in graphical materials (histograms of gas chimneys distribution by depth and height of gas discharge, map of sip location by the Paleo-Kalanchak River area).
卡兰恰克古河流附近新黑海的天然气烟囱
该出版物基于大量关于黑海西北部,特别是古卡兰恰克地区天然气露头的数据。这些材料是在乌克兰国家科学院海洋地质和沉积矿石形成部的R/V上进行的航行期间获得的,以及文献资料。在研究区域发现了3000多个甲烷小口。古河Kalanchak地区以及黑海西北部其他地区的绝大多数气体排放都局限于大陆斜坡的上部和大陆架的邻近地区。实际上,它是大陆架边缘两侧45公里宽的带状地带。本文对地震剖面和声学剖面进行了研究。他们的分析表明,烟囱不是随机分布的,而是集中在特定的位置。指出海底甲烷露头的空间分布与地貌构造以及以断裂为主的构造构造有一定的关系。气烟囱与各种形式的海底地形有关,但它们最多的是位于古河流峡谷的入口处。本文提供了黑海西北部古河网的较为详细的地貌信息。在河口峡谷,气体排放沿着沉积脊形成,气体烟囱出现在峡谷底部、边缘或海底滑坡堆积点附近,那里的沉积覆盖物受到物质运输的干扰。在大陆架上,气体烟囱最集中的地方是圆形和细长的洼地(凹痕)。在声学剖面研究的基础上,对黑海古卡兰恰克部分天然气烟囱进行了分类,根据其位置深度、气体释放高度、气体流量、气体释放形式、运行方式等特征进行了分类。研究结果还以图形材料的形式呈现(气体烟囱按排放深度和高度分布的直方图,古卡兰恰克河地区的sip位置图)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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