Marine geophysical research in the first Ukrainian Antarctic expeditions: historical outline and some results

V. Solovyov, V. Bakhmutov
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Abstract

The article is devoted of the 25th anniversary of the First Ukrainian Marine Antarctic Expedition (1997). The short history of development the marine geophysical study of the deep structures of the World Ocean and Antarctica in the S. I. Subbotin Institute of Geophysics (National Academy of sciences of Ukraine) is presented. Main focus is on the results obtained during the implementation of the «State research programs in Antarctica». The main patterns of geophysical anomalies and their spatiotemporal distributions in West Antarctica were investigated. The lithosphere deep structured geophysical models well corresponds with the evolution processes of the continental margin of the West Antarctica. The built-depth sections record the large-scale processes of the formation of the Drake Passage and the western part of the Scotia Sea as a result of the primary crust fragments’ transformation and the geodynamic evolution of the region located between South America and West Antarctica. Some results for the assessment of mineral resources and hydrocarbon potential of the continental margin structures of the NW area of the Antarctic Peninsula are presented.
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乌克兰第一次南极考察中的海洋地球物理研究:历史概况和一些成果
这篇文章是献给第一次乌克兰海洋南极考察25周年(1997年)。介绍了苏博廷地球物理研究所(乌克兰国家科学院)对世界大洋和南极洲深部结构的海洋地球物理研究的简短发展历史。主要重点是在实施“南极洲国家研究方案”期间取得的成果。研究了西南极洲地球物理异常的主要模式及其时空分布。岩石圈深部构造地球物理模型与西南极洲大陆边缘的演化过程吻合较好。建成深度剖面记录了位于南美洲和西南极洲之间的区域由于地壳原始碎屑的转化和地球动力学演化而形成的德雷克海峡和斯科舍海西部的大规模过程。介绍了南极半岛西北地区大陆边缘构造的矿产资源和油气潜力评价的一些结果。
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审稿时长
6 weeks
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