The first data on the eastern part of Taman Bay are based on an ultra-high-resolution seismic survey. The seismoacoustic complexes of a profile are compared with Novochernomorsk and Karangat sediments to Lower Chauda sediments of the Quaternary age. The fold structure of Quaternary sediments of this area is confirmed. An analysis of the bedding of the newest marine sediments of the bottom and the submergence of the ancient city of Phanagoria in the beginning of the 1st century AD indicate the Late Holocene tectonic activity of the Taman Bay depression. Two profile areas exhibit signal coherence gaps interpreted as areas of gas accumulations. The gas emissions are probably morphologically related to a wing of the adjacent Akhtaniz Anticline and are interpreted as a result of clay diapirism of the Maikop Group.

中文翻译：

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帕纳戈里亚古城地区塔曼湾近海超高分辨率地震声波测量结果

塔曼湾东部的第一批数据基于超高分辨率地震勘测。将剖面的地震声复合体与新切尔诺莫尔斯克和卡兰加特沉积物与第四纪下乔达沉积物进行比较。确认了该区第四纪沉积物的褶皱结构。对公元 1 世纪初最新海相沉积物的层理和帕纳哥里亚古城的淹没分析表明，塔曼湾洼地处于全新世晚期构造活动。两个剖面区域表现出信号相干间隙，解释为气体聚集区域。气体排放可能在形态上与相邻的 Akhtaniz 背斜的一个翼有关，并被解释为 Maikop 群粘土底辟作用的结果。