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Characteristics of features formed by gas hydrate and free gas in the continental slope and abyssal plain of the Middle Caspian Sea

机译:中里海大陆坡和深海平原天然气水合物和游离气体形成的特征

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摘要

Physicochemical conditions are proper to form gas hydrate and free gas in the Caspian Sea which are considered both for geohazard assessment and future possible source of energy. Gas migration, hydrate formation and decomposition cause different types of features to form in the seabed and sediments which can be affected by geological and physical conditions of sea. In this study, high-resolution marine seismoacoustic profiles were interpreted to investigate features formed by gas hydrate and free gas and assess their characteristics in the continental slope and abyssal plain of the middle Caspian Sea. A mud volcano, gas chimneys, pockmarks, gas pipes, sediment disturbances, a crater, a giant landslide and a big gentle diapir were investigated and reported in the present study. The geological and physical conditions including bathymetry, tectonic activity, sediments supply and water depth are different in the continental slope and abyssal plain, thereby the features of these two environments were compared to understand the effect of different conditions.
机译:里海的物理化学条件适合形成天然气、水合物和游离气体,这既可以用于地质灾害评估,也可用于未来可能的能源。气体迁移、水合物形成和分解导致海床和沉积物形成不同类型的特征,这些特征可能受到海洋地质和物理条件的影响。本研究通过高分辨率海洋地震声剖面研究天然气水合物和游离气体形成的特征,并评估了中里海大陆坡和深海平原的特征。本研究调查并报道了泥火山、煤气烟囱、麻点、煤气管道、泥沙扰动、火山口、巨型滑坡和大平缓底辟。大陆坡和深海平原的测深、构造活动、沉积物供应和水深等地质物理条件不同,因此比较了这两种环境的特征,了解不同条件的影响。

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