2020
DOI: 10.1080/1064119x.2019.1709585
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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

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Cited by 7 publications
(3 citation statements)
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“…The northern contourite feature is divided by the obvious fault into two segments which together form typical fault-controlled drift (Figure 13). The acoustical transparent anomalies indicative of gas escape are widely distributed in the Caspian Sea [44,61]. Similar weak acoustic anomalies are observed in this area (Figure 13B).…”
Section: Contourite Sedimentary Driftssupporting
confidence: 63%
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“…The northern contourite feature is divided by the obvious fault into two segments which together form typical fault-controlled drift (Figure 13). The acoustical transparent anomalies indicative of gas escape are widely distributed in the Caspian Sea [44,61]. Similar weak acoustic anomalies are observed in this area (Figure 13B).…”
Section: Contourite Sedimentary Driftssupporting
confidence: 63%
“…In the bottom relief, the drift is complicated by a channel-looking feature (Figure 11); however, this feature can be interpreted as a crater because canyons are normally V-shaped and have new sedimentation at the bottom, but the materials at the bottom of this structure seem to collapse down. Gerivani et al [44] interpret this structure as a crater formed by a mechanism such as that suggested and described by [45,46] for "hill-hole pairs". In this crater, it seems that the mixture of high-pressure gas, sediments and water were first emitted from probably weak zones in both sides of the crater, and then the upper beds collapsed down.…”
Section: Northern Slope (Mangyshlak Sill)mentioning
confidence: 92%
“…It is estimated that 97-99% of the discovered gas hydrate resources in the world are located in the ocean, and only 1-3% are distributed on land (Merey and Chen, 2022). Gas hydrate also exists in deep-water areas of some inland seas and lakes, such as the Black Sea and Lake Baikal (Gerivani et al, 2020;Yevgeny et al, 2021). Nevertheless, people are more concerned about the gas hydrate stability zone (GHSZ) with considerable thickness in the ocean because the thick layered hydrate-bearing sediments generally do not appear in the inland seas and lakes.…”
Section: Introductionmentioning
confidence: 99%