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

Author:

Gerivani H.1,Putans V.A.2,Merklin L.R.2,Modarres M.H.1

Affiliation:

1. Iranian National Institute for Oceanography and Atmospheric Science, Tehran, Iran;

2. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia

Publisher

Informa UK Limited

Subject

Ocean Engineering,Geotechnical Engineering and Engineering Geology,Oceanography

Reference68 articles.

1. Massive blow-out craters formed by hydrate-controlled methane expulsion from the Arctic seafloor

2. On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods

3. Badhani, S., J. Bialas, C. Berndt, I. Klaucke, and T. Zander. 2016. Possible evidence for a relationship between gas hydrate dissociation and submarine slope failure in the Danube deep-sea fan, Black Sea. In 76. Jahrestagung der Deutschen Geophysikalischen Gesellschaft, 14.17.03.2016, Münster, Germany.

4. Subsea gas emissions from the Barbados Accretionary Complex

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