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Cited by 149 publications
(111 citation statements)
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References 19 publications
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“…During the Pliocene, the palaeo-Volga delta was situated about 500 km to the south of its present-day position Reynolds et al, 1998) in response to the initial subsidence of the south Caspian basin and uplift of the Caucasus and Kopet Dag ranges (Allen et al, 2002). The middle Caspian basin (Derbent Depression) subsided at a later time (Dumont, 1998) and is separated from the south Caspian basin by the Apsheron Sill, an area of tectonic uplift (Allen et al, 2002(Allen et al, , 2003 where present-day water depths vary between 80 and 200 m (Ferronsky et al, 1999;Kosarev and Yablonskaya, 1994).…”
Section: Structural and Geographical Settingmentioning
confidence: 99%
“…During the Pliocene, the palaeo-Volga delta was situated about 500 km to the south of its present-day position Reynolds et al, 1998) in response to the initial subsidence of the south Caspian basin and uplift of the Caucasus and Kopet Dag ranges (Allen et al, 2002). The middle Caspian basin (Derbent Depression) subsided at a later time (Dumont, 1998) and is separated from the south Caspian basin by the Apsheron Sill, an area of tectonic uplift (Allen et al, 2002(Allen et al, , 2003 where present-day water depths vary between 80 and 200 m (Ferronsky et al, 1999;Kosarev and Yablonskaya, 1994).…”
Section: Structural and Geographical Settingmentioning
confidence: 99%
“…2) that is not located above a subduction regime, but bordered east and west by super deep sedimentary basins that have their origin in the Mesozoic and are filled with Cenozoic-Quaternary sediments. To the north and south of the Greater Caucasus are the foreland basins of the Terek-Kuban and the Kura-Kakheti-Kartli-Rioni, respectively (Ershov et al 1999;Mikhailov et al 1999;Ulminshek 2001;Daukeev et al 2002;Ershov et al 2003); to the east and west are the Caspian Sea and the Black Sea, respectively (Shikalibeily & Grigoriants 1980;Berberian 1983;Ismail-Zade et al 1987;Narimanov 1992;Abrams & Narimanov 1997;Mangino & Priestley 1998;Nikishin et al 1998;Allen et al 2002;Brunet et al 2003;Nikishin et al 2003). The Lesser Caucasus is situated above an old, possibly detached subduction slab (Hafkenscheid et al 2006).…”
Section: Regional Tectonics and Geodynamicsmentioning
confidence: 99%
“…However, the northern boundary of the basin is characterized by deep earthquakes (30-76 km), interpreted by Jackson et al (2002) and Allen et al (2002) to indicate incipient subduction of the South Caspian Basin under the Central Caspian continental domain to the north. The basement of the South Caspian Basin remains rigid (aseismic) in this process, and the convergence is accommodated by the formation of an incipient accretionary prism with numerous anticlinal folds of the sedimentary cover detached on deeper mobile shales.…”
Section: Structurementioning
confidence: 99%