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- W2020161292 abstract "172 The territory of the Kerch Taman mud volcano zone is distinct for high neotectonic activity. Mud vol canoes erupt here both on land and in the Sea of Azov. In the latter case, islands of hundreds of meters in diameter and up to several meters high are formed from eruption products [1]. These islands are short lived though: active water erosion destroys them in the course of several months. Mud volcanoes are located in cryptodiapiric folds in Cenozoic deposits. Folds are grouped into long narrow subparallel anticline arrays divided by wider flat synclines. Anticlines are situated in the frontal parts of thrusts formed under tangential compression, and these structures are genetically interrelated [2, 3]. On land, anticlines are usually directly manifested in relief as topographic highs." @default.
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- W2020161292 date "2013-02-01" @default.
- W2020161292 modified "2023-10-10" @default.
- W2020161292 title "A Catastrophic tectonic event in summer 2011 in the Taman Peninsula" @default.
- W2020161292 doi "https://doi.org/10.1134/s1028334x13020207" @default.
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