Surface structure, activity and microgravimetry modeling delineate contrasted mud chamber types below flat and conical mud volcanoes from Azerbaijan

Odonne, Francis; Imbert, Patrice; Rémy, Dominique; Gabalda, Germinal; Aliyev, A.; Abbasov, O. R.; Baloglanov, Elnur E.; Bichaud, Victoria; Juste, Remy; Dupuis, Matthieu; Bonvalot, Sylvain

doi:10.1016/j.marpetgeo.2021.105315

Cited by 9 publications

(4 citation statements)

References 67 publications

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“…The southern margin of the East European craton keeps relatively stable. Similar regimes set almost in the whole territory of the Scythian plate, except for its Caspian side [42][43][44][45][46][47][48], where the zone of varied regimes with the dominant extension and downwarping forms, and the southern margin, with inceptive submontane troughs.…”

Section: Resultsmentioning

confidence: 99%

Tectonic zonality of sedimentation cover in the Black Sea–Caspian Region

Senin¹,

Mustaev²,

Kerimov³

et al. 2022

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The article focuses on modeling tectonic zonality of the sedimentation cover in the Black Sea-Caspian Region, and addresses the identification and validation of the Late Paleozoic, Mesozoic, Alpine and recent-time geodynamically active structures. The modeling shows that the significant events, which governed the evolution features of the geodynamically active structures, correlate with the recent time. That is the time when such sedimentation basins as Terek-Caspian, Indol-Kuban, Eastern Kuban and Karkinit have finally set. The first three basins in this list occur in the zones of the reverse geodynamic regime, with dominant extension and downwarping within the limits of cratons, and belong to the Black Sea-Caspian geodynamically active structure. The Karkinit basis belongs to the Scythian geodynamically active structure with generally compressive tectonics, dominant upheaval or relative stabilization. The tectonic features have had the critical influence on both formation of the sedimentation cover of the basins and spatial distribution of minerals.

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Section: Resultsmentioning

confidence: 99%

Tectonic zonality of sedimentation cover in the Black Sea–Caspian Region

Senin¹,

Mustaev²,

Kerimov³

et al. 2022

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“…The maximum velocities were observed in the Indol-Kuban basin in the Maykopian period, in the Terek-Caspian basin in the Miocene and in the Indol-Kuban basin again in the Pliocene. Both basins are conventionally assumed to be the frontal foredeeps ahead of the Caucasus orogeny front, which is considered as a key control factor the genesis and evolution of the basins [33][34][35][36][37][38]. The accomplished analysis shows that a potential complimentary factor to control tectonic downwarping of the Indol-Kuban basin at some stages of its development is the indirect influence of rifting in the Eastern Black Sea depression, via a system of shearinduced dislocations.…”

Section: Erc Rc Er H H H H H H H H H H H H H H H H H H H H H H H H Cr...mentioning

confidence: 99%

Sedimentary basin analysis: Black Sea–Caspian Region

Mustaev¹,

Kerimov²,

Лавренова³

et al. 2023

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The accomplished analysis has found out that the study basins were the parts of the Black Sea-Caspian basin system in the Mesozoic era, partly participated in dislocation tectonics later on, and are the part of the Alpine folding zone from the viewpoint of the modern tectonic zoning. Furthermore, the analysis has set the main stages of the sedimentation cross-section formation with the specified sedimentary depocenters at each stage, which allows reconstructing the sedimentation evolution. The studies of the delineated area reveal four zones of stable downwarping within the period of the plate mantle formation: the Karkinit, Indol-Kuban, Eastern Kuban and Terek-Caspian basins. Each basin features unique evolution in terms of different tectonics modes and sedimentation velocities. These factors govern the geological structures of the basins-different thickness relationships of sedimentary units.

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“…As follows from the map, the areas of the sedimentation cross-section with the total thickness of more than 1.5 km occupy the largest part of the Black Sea-Caspian region. Sediments are absent or have the thickness smaller than 1.5 km in the areas of the Anatolian-Iran boundary of the Black Sea-Caspian region, at its Balkan and East Mysian (Dobrudzha) limits, in the areas of the Ukrainian shield, Folded Donbass and some parts of the Karpinsk ridge, which limit the region in the north, and at some inner and marginal uplifts in the region [35][36][37]. The latter are the orogenesis-Caucasus, Crimean and Mangyshlak, and some domelike and swell-like uplifts-the Arkhangelsk uplift in the Black Sea, Azov swell and Central Crimean and Karabogaz swells, as well as the smaller size structures.…”

Section: Han Han Ha H H Han Ha An Han Han Han An Han H Han Ha H Han A...mentioning

confidence: 99%

Formation conditions of sedimentary basins in the Black Sea–Caspian region

Mustaev¹,

Senin²,

Kerimov³

et al. 2022

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structures-Scythian-Turan and Black Sea-South Caspian [1][2][3][4][5][6][7]. The Paleogene-Neogene age of the sedimentary basins is connected with the formation of a foredeep ahead of the front of the Greater Caucasus folding. The pattern of the Cenozoic basinlike structures characterizes the contemporary age of this region. The east-west strike of the belt of the basin-like structures in the north of the study regions obeys the general strike of the zone of interaction between the orogenic folded structure of the Greater Caucasus and the Scythian Platform, which

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Surface structure, activity and microgravimetry modeling delineate contrasted mud chamber types below flat and conical mud volcanoes from Azerbaijan

Cited by 9 publications

References 67 publications

Tectonic zonality of sedimentation cover in the Black Sea–Caspian Region

Tectonic zonality of sedimentation cover in the Black Sea–Caspian Region

Sedimentary basin analysis: Black Sea–Caspian Region

Formation conditions of sedimentary basins in the Black Sea–Caspian region

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