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Journal articles on the topic 'South Caspian Basin'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

ZAREI, FATAH, HAMID REZA ESMAEILI, KEYVAN ABBASI, MARCELO KOVAČIĆ, ULRICH K. SCHLIEWEN, and CAROL A. STEPIEN. "Gobies (Teleostei: Gobiidae) of the oldest and deepest Caspian Sea sub-basin: an evidence-based annotated checklist and a key for species identification." Zootaxa 5190, no. 2 (2022): 151–93. http://dx.doi.org/10.11646/zootaxa.5190.2.1.

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An evidence-based annotated checklist of gobiid species (Teleostei: Gobiidae) inhabiting the South Caspian Sea and its catchment area (i.e., the South Caspian Sea sub-basin) is compiled. The South Caspian Sea sub-basin gobiofauna currently comprises 38 confirmed species in 11 genera (i.e., 88.4% of the Caspian gobiofauna); the most diverse genus is Benthophilus (16 species, 42.1%), followed by Ponticola (seven species, 18.4%), and Neogobius (four species, 10.5%). Ten species (26.3%) are endemic to the South Caspian Sea sub-basin, another 21 species (55.3%) are endemic in the Caspian Sea basin

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2

Ghassemi, Mohammad R., Mark B. Allen, and Hossein Motamedi. "A SYNTHESIS OF THE GEOLOGY AND PETROLEUM GEOLOGY OF THE IRANIAN PORTION OF THE SOUTH CASPIAN BASIN AND SURROUNDING AREAS." Journal of Petroleum Geology 46, no. 4 (2023): 487–512. http://dx.doi.org/10.1111/jpg.12848.

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The South Caspian Basin, the northern Alborz Mountains, the Gorgan plain and the Moghan plain constitute the northernmost and youngest petroleum system in Iran. This region was part of the Paratethys realm from Oligocene to Pliocene time. The Oligocene – Miocene Maikop/Diatom Total Petroleum System of the South Caspian Basin produces major volumes of hydrocarbons in Azerbaijan and Turkmenistan, and the Iranian sector of the basin has consequently undergone exploration due to its generally similar geology. The 20 km thick, dominantly Cenozoic sedimentary cover in the basin is reduced to less th

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Mammadov, P. Z., and R. Y. Ganiyevа. "CONDITIONS FOR THE FORMATION OF CLINOFORMS IN THE MIDDLE AND SOUTH CASPIAN MEGABASIN." Series of Geology and Technical Sciences 2, no. 446 (2021): 82–89. http://dx.doi.org/10.32014/2021.2518-170x.38.

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The paper considers sedimentation process and objects of lateral development in deep-water uncompensated and shallow-water – epicontinental paleobasins developed at various evolution stages of South- Caspian and Middle-Caspian basins. The South Caspian megabasin is a great tectonic crustal element and a highly prospective sedimentary basin in the central segment of the Alpine-Himalayan mobile belt. The role of boundary structures of Scythian-Turan platform in the Middle Caspian (such as South-Caspian land and Karaboghaz arc) and avalanche sedimentation on the continental shelf in development o

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Balykin, Pavel Aleksandrovich, and Raisa Pavlovna Khodorevskaya. "STATE OF FISHERIES IN SOUTH REGION OF VOLGO-CASPIAN FISHERIES BASIN." Vestnik of Astrakhan State Technical University. Series: Fishing industry 2021, no. 3 (2021): 7–17. http://dx.doi.org/10.24143/2073-5529-2021-3-7-16.

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The paper presents the generalized materials on the current state of fisheries in the Northern part of the Caspian Sea (southern region of the Volga-Caspian fisheries basin). It is shown that catches in the North-Western and Tersk-Caspian subdistricts varied in the opposite way: an increase in production in one subdistrict was accompanied by a decrease in the other. The decreasing or increasing catches is due to semi-anadromous (roach, brim, zander, carp) and freshwaterfish species (cat-fish, pike-perch, small size ordinary fish). There have been found the significant relationships between the

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5

Jackson, James, Keith Priestley, Mark Allen, and Manuel Berberian. "Active tectonics of the South Caspian Basin." Geophysical Journal International 148, no. 2 (2002): 214–45. http://dx.doi.org/10.1046/j.1365-246x.2002.01005.x.

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6

Jackson, J., K. Priestley, M. Allen, and M. Berberian. "Active tectonics of the South Caspian Basin." Geophysical Journal International 148, no. 2 (2002): 214–45. http://dx.doi.org/10.1046/j.1365-246x.2002.01588.x.

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7

Djevanshir, Rashid D., and G. Ali Mansoori. "Introduction to South Caspian Basin special issue." Journal of Petroleum Science and Engineering 28, no. 4 (2000): 153–55. http://dx.doi.org/10.1016/s0920-4105(00)00074-7.

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8

Rieke, Herman H. "Petroleum Geology of the South Caspian Basin." Journal of Petroleum Science and Engineering 34, no. 1-4 (2002): 137. http://dx.doi.org/10.1016/s0920-4105(01)00167-x.

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9

Bagirov, E., and I. Lerche. "Breccia Hazards in the South Caspian Basin." Energy Exploration & Exploitation 16, no. 2-3 (1998): 153–84. http://dx.doi.org/10.1177/0144598798016002-304.

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Ejection of breccia from mud volcanoes for the onshore and offshore South Caspian Basin provides hazards for rigs, pipeline, and subsea completion equipment. Here we investigate the lateral ranges of ejected rock fragments for aeolian and submarine conditions. In addition, the consequences are considered of emission from a raised or depressed crater, with or without a surrounding crater wall. Also investigated is aeolian transport to an ocean surface, and subsea motion thereafter. Rough rules of thumb for aeolian hazards from breccia would indicate that seconds to tens of seconds after breccia

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10

Bagirov, E., and I. Lerche. "Flame Hazards in the South Caspian Basin." Energy Exploration & Exploitation 16, no. 4 (1998): 373–97. http://dx.doi.org/10.1177/014459879801600406.

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Heating hazards caused by mud volcano flame eruptions are assessed for the South Caspian Basin. In general, it is found that winds of more than about 50 km/hr will cause serious heating hazard problems when directed partially downward onto flame columns of greater than a few hundred meters in length. Hazard distances from emergence points of flame columns at which the surface temperature is less than 60°C, stinging hot against human flesh, are typically in the 5–15 km range. Low angle emergent flames are more easily bent to lick the emergent surface than are high angle flames, providing a high

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11

Samedova, F. I., Yu A. Abdullaeva, and S. A. Zeinalova. "Crude oils of the South Caspian Basin." Chemistry and Technology of Fuels and Oils 27, no. 12 (1991): 666–69. http://dx.doi.org/10.1007/bf00725711.

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12

Yusifov, M. G. "The role of the Absheron facies in the formation of the productive strata in the South Caspian Basin." Oil and Gas Studies, no. 5 (December 4, 2022): 57–74. http://dx.doi.org/10.31660/0445-0108-2022-5-57-74.

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In oilfield practice, the lithofacies criterion is very often decisive for the formation of deposits of liquid and gaseous hydrocarbons. The Absheron lithofacies type of sediments (Absheron facies), enriched in quartz material, composes the reservoirs of the horizons of all large oil and gas fields in the South Caspian Basin. The genesis of the Absheron facies is closely related to the genesis of the productive stratum, there is no consensus on both issues to date. It is indisputable that the productive stratum and the Absheron facies were formed in the conditions of a closed continental basin

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Rachinskiy, M. Z., G. V. Chilingar, and M. V. Gorfunkel. "Oil and Gas Potential of South-Caspian Basin." Energy Sources, Part A: Recovery, Utilization, and Environmental Effects 29, no. 15 (2007): 1339–60. http://dx.doi.org/10.1080/15567030701545964.

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14

Kaz’min, V. G., and E. V. Verzhbitskii. "Age and origin of the South Caspian Basin." Oceanology 51, no. 1 (2011): 131–40. http://dx.doi.org/10.1134/s0001437011010073.

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15

Guliev, I., A. Geizullayev, and M. Tagiyev. "Isotopic-Geochemical Characteristics in the South Caspian Basin." Energy Exploration & Exploitation 15, no. 4-5 (1997): 311–68. http://dx.doi.org/10.1177/0144598797015004-503.

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16

Mukhtarova, Khuraman Z., and Gulter J. Nasibova. "Geodynamic regime and prospects for oil and gas potential in the South Caspian Basin." Journal of Geology, Geography and Geoecology 32, no. 3 (2023): 550–59. http://dx.doi.org/10.15421/112349.

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   The article considers the geodynamic regime of the South Caspian depression, de- fines the directions of compressive stresses, the role of the latter in changing the thickness of sedimentary formation complexes, in the formation of local uplifts and their complication by faults and mud volcanism. The purpose of the study is to research the geodynamic regime and determine the oil and gas content of the South Caspian depression. The article reflects the features of studying the zone of pseudosub- duction in the South Caspian depression and the analysis of the obtained result

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17

Lahijani, H. A. K., H. Abbasian, A. Naderi Beni, et al. "Sediment distribution pattern of the South Caspian Sea: possible hydroclimatic implications." Canadian Journal of Earth Sciences 56, no. 6 (2019): 637–53. http://dx.doi.org/10.1139/cjes-2017-0239.

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The south Caspian subbasin extends from the foot of the Alborz Mountains to the deepest part of Caspian Sea. The lithological background and tectonic setting of the study area primarily control the deposition of thick sedimentary sequences of the basin, while hydroclimatic processes exert secondary impacts on the sediment distribution pattern. To evaluate past hydroclimatic changes, short sediment cores were retrieved from the continental shelf and upper slope of the south Caspian Sea and were treated for basic sedimentological properties and mineralogy. The results show that the sediments are

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18

Serikova, U. S., M. A. Allanazarova, and E. Z. Idiyatullina. "Hydrocarbon systems in the Turkmen sector of the South Caspian basin." Proceedings of higher educational establishments. Geology and Exploration, no. 5 (February 5, 2023): 24–40. http://dx.doi.org/10.32454/0016-7762-2022-64-5-24-40.

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Introduction. The paper considers conditions conductive to the formation and location of oil and gas accumulations in the Turkmen sector of the South Caspian Basin.Aim. Modeling of hydrocarbon systems of the Turkmen sector of the South Caspian Basin.Materials and methods. Statistical generalization and systematization of the data and materials presented in reference literature, field sources, and archive data, as well as published works of Sh.F. Mekhtiev, I.S. Guliev, M.Z. Rachinskii, S.S. Dzhibuti, S.A. Aliev, V.Yu. Kerimov, V.V. Kolodiya, etc. Data modeling was performed using the PetroMod s

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19

Mukhtarov, Abdulvahab Sharif. "Shallow and Deep Temperatures in the South-Caspian Basin." International Journal of Terrestrial Heat Flow and Applications 1, no. 1 (2018): 23–29. http://dx.doi.org/10.31214/ijthfa.v1i1.13.

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Distribution of shallow and deep temperatures in the sedimentary cover of the South Caspian Basin (SCB) is addressed. Analysis of soil temperature data recorded in meteostations of Azerbaijan and its neighboring regions provide clues as to the temperatures at near surface layers. Such layers, where seasonal variations of temperatures converge to near-stable values have been designated as the “neutral” layer. In many localities, the bottom parts of such layers extend to depths of around 20 m. In addition, temperature data of over 150 wells, obtained from depths varying from 100 to 6000 m in oil

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20

Green, Tim, Nazim Abdullayev, Jake Hossack, Greg Riley, and Alan M. Roberts. "Sedimentation and subsidence in the South Caspian Basin, Azerbaijan." Geological Society, London, Special Publications 312, no. 1 (2009): 241–60. http://dx.doi.org/10.1144/sp312.12.

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21

Gunduz, M., and E. Özsoy. "Modelling seasonal circulation and thermohaline structure of the Caspian Sea." Ocean Science 10, no. 3 (2014): 459–71. http://dx.doi.org/10.5194/os-10-459-2014.

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Abstract. The wind- and buoyancy-driven seasonal circulation of the Caspian Sea is investigated for a better understanding of its basin-wide and mesoscale dynamics, mixing and transport. The model successfully reproduces the following basic elements of the circulation: the southward-flowing current systems along the eastern and western coasts, the upwelling along the eastern coast, the cyclonic circulation in the Middle Caspian Sea (MCS), especially in winter, and the cyclonic and anticyclonic cells of circulation in the South Caspian Sea (SCS). The observed seasonal variability of sea level a

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Gunduz, M., and E. Özsoy. "Modelling Seasonal Circulation and Thermohaline Structure of the Caspian Sea." Ocean Science Discussions 11, no. 1 (2014): 259–92. http://dx.doi.org/10.5194/osd-11-259-2014.

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Abstract. The wind and buoyancy driven seasonal circulation of the Caspian Sea is investigated for a better understanding of its basin-wide and meso-scale dynamics, mixing and transport. The model successfully reproduces the following basic elements of the circulation: the southward flowing current systems along the eastern and western coasts, the upwelling along the eastern coast, the cyclonic circulation in the Middle Caspian Sea (MCS) especially in winter, and the cyclonic and anticyclonic cells of circulation in the South Caspian Sea (SCS). The observed seasonal variability of sea level an

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23

Medvedev, Igor P., Evgueni A. Kulikov, and Isaac V. Fine. "Numerical modelling of the Caspian Sea tides." Ocean Science 16, no. 1 (2020): 209–19. http://dx.doi.org/10.5194/os-16-209-2020.

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Abstract. The Caspian Sea is the largest enclosed basin on Earth and a unique subject for the analysis of tidal dynamics. Tides in the basin are produced directly by the tide-generating forces. Using the Princeton Ocean Model (POM), we examine details of the spatial and temporal features of the tidal dynamics in the Caspian Sea. We present tidal charts of the amplitudes and phase lags of the major tidal constituents, together with maps of the form factor, tidal range, and tidal current speed. Semi-diurnal tides in the Caspian Sea are determined by a Taylor amphidromic system with anticlockwise

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24

Pogorelova, E., and M. Abdulla-zada. "ANTI-CAUCASIAN FOLDING OF THE KURA-SOUTH CASPIAN HOLLOW (BY THE EXAMPLE OF SOUTH CASPIAN BASIN AND CIS-LESSER CAUCASIAN TROUGH)." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 1 (100) (2023): 23–29. http://dx.doi.org/10.17721/1728-2713.100.03.

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The South Caspian Basin (SCB) is the deepest submerged sedimentary basin in the World and occupies the entire southern deep-water part of the Caspian Sea and the Kura and West Turkmenian lowlands adjacent to it from the west and east. The SCB has the thinnest (6...8 km) consolidated oceanic-type crust and the thickest sedimentary cover (25...30 km). The thickness of the Pliocene-Quaternary deposits is 10...12 km. The thickness of the main oil and gas complex – Productive-Red-Colored Strata of the Lower Pliocene is 7 ... 8 km. More than 6 km of volcanic-sedimentary deposits accumulated within t

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URMANOVA, D., and D. D. HUMPHREY. "STRATIGRAPHIC DEVELOPMENT OF THE DEVONIAN-CARBONIFEROUS COMPLEX OF THE SOUTHERN SIDE OF THE CASPIAN DEEP." Neft i Gaz 131, no. 5 (2022): 77–93. http://dx.doi.org/10.37878/2708-0080/2022-5.05.

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This article presents a study of the stratigraphic development of the Devonian-carboniferous complex of the southern side of the Caspian basin, in which a comprehensive study of sedimentary formations of the subsalt complex and the creation of a stratigraphic model of the Late Paleozoic stage of evolution of the southern Caspian sedimentary basin was carried out based on a refined correlation scheme by Abilkhasimov (2015), with the inclusion of generalized data on the structures of Ansagan and Maksat. The basis for the development of a stratigraphic model in the Late Paleozoic of the Coastal z

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ABILKHASIMOV, H. B. "SEDIMENTATION MODEL OF CARBONATE UPLIFTS OF THE COASTAL ZONE OF THE SOUTH OF THE CASPIAN SEDIMENTARY BASIN IN THE LATE DEVONIAN-EARLY VISEAN TIME." Neft i Gaz 130, no. 4 (2022): 8–25. http://dx.doi.org/10.37878/2708-0080/2022-4.01.

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The results of lithological studies and paleogeographic reconstructions of the Late DevonianEarly Visean stage of development and features of the formation of the sedimentary complex of the Primorsky zone of uplifts in the south of the Caspian sedimentary basin are presented. The complex geological structure of the region is mainly due to the influence of tectonic, volcanic, and denudation processes on sedimentation. The results of drilling deep wells in recent years have made it possible to refine the internal structure, substantiate new objects in the Late Devonian complex, and reassess the

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Bagirov, E., R. Nadirov, and I. Lerche. "Hydrocarbon evolution for a north-south section of the South Caspian Basin." Marine and Petroleum Geology 14, no. 7-8 (1997): 773–854. http://dx.doi.org/10.1016/s0264-8172(97)00052-4.

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28

Naseka, A. M., and N. G. Bogutskaya. "Fishes of the Caspian Sea: zoogeography and updated check-list." Zoosystematica Rossica 18, no. 2 (2009): 295–317. http://dx.doi.org/10.31610/zsr/2009.18.2.295.

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Geographic distribution of some 350 taxa from the Caspian and Black Sea basins were analyzed with regard to recent taxonomy, phylogeny, endemicity and ecological classification. A check-list of the Caspian Sea fishes (taxa from families down to subspecies) is provided. Eighty species and subspecies permanently occur or occasionally recorded from the North Caspian while 33–35 species and subspecies being only distributed in the Middle and South Caspian. Forty-four species are common for the two ecoregions. A comparison of the Caspian and the Black Sea fish faunas and their historical evolution

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Abilkhasimov, Kh B., A. M. Ospanov, R. K. Madisheva, and R. Smabayeva. "Prospects for the allocation of Paleorousels in the subsalt complex of the south-east of the Caspian sedimentary basin." Neft i Gaz, no. 4 (August 30, 2024): 6–21. http://dx.doi.org/10.37878/2708-0080/2024-4.01.

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development and features of the formation of the sedimentary complex of the south of the Caspian sedimentary basin are presented. The complex geological structure of the region is mainly due to the influence of tectonic, volcanic and denudation processes on sedimentation. The introduction of terrigenous material deep into the sedimentary basin (Matken-Ushmolinsk, Biikzhal and South Embin zones) by paleorubic flows contributed to the emergence of accumulative shafts and interbranch uplifts composed mainly of clay rocks with alternating siltstone-sandstones. In the paleorusls themselves, coarser

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30

Aliyeva, E. H., and K. F. Mustafayev. "Geochemistry of Miocene sediments of the Middle and South Caspian basins (within Azerbaijan): climate, chemical maturity and provenance." SOCAR Proceedings, SI2 (December 30, 2023): 49–65. http://dx.doi.org/10.5510/ogp2023si200893.

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Geochemical and petrographic characteristics of the Miocene rocks of the Shamakhi-Gobustan trough (South Caspian basin) and the North Absheron uplift zone (Middle Caspian basin) indicate that these sediments contain products of erosion of the magmatic rocks of the Eurasian continent’s active margin - the volcanic arc of the Lesser Caucasus, as well as granitic basement of the Garabogaz High and Mesozoic-Eocene sedimentary strata of the Middle Caspian basin and the Greater Caucasus. The uplift of the Greater Caucasus, which began in the Middle Eocene as a result of the collision of the Afro-Ara

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Aslanov, B. S., S. M. Mammadova, I. I. Guliyev, and V. B. Jabrailzadeh. "Structural-tectonic criteria of oil-gas bearing capacity on the western coastal "land-sea" transition zone of South Caspian depression (in the order of discussion)." Azerbaijan Oil Industry, no. 2 (February 15, 2020): 10–15. http://dx.doi.org/10.37474/0365-8554/2020-2-10-15.

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South Caspian oil-gas bearing basin is the richest Caspian region for oil and gas production. The great majority of produced fields are located here. Therefore, coastal states consider it the prospective region. Briefly, the paper describes the geographic and tectonic location of South Caspian, as well as the structural-morphological features of Mezo-Cenozoic sediment layers. It is emphasized that ultra-deep South Caspian depression is the major oil-gas forming bolson, both in the paleo-geological evolution process and nowadays. However, there is no single opinion on its role in the formation

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Serikova, U. S., and M. A. Allanazarova. "Formation conditions of hydrocarbon systems in the Turkmen sector of the South Caspian basin." Proceedings of higher educational establishments. Geology and Exploration, no. 5 (December 13, 2023): 33–51. http://dx.doi.org/10.32454/0016-7762-2023-65-5-33-51.

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Background. The formation and placement conditions of hydrocarbon systems and their accumulation in the Turkmen sector of the South Caspian basin are considered.Aim. To model the existing hydrocarbon systems in the Turkmen sector of the Caspian Sea based on available data.Materials and methods. Statistical generalization and systematization of available data was carried out. Research materials included fund and reference sources, fieldwork data, and publications by Sh.F. Mehdiyev, I.S. Guliyev, M.Z. Rachinsky, S.S. Djibouti, S.A. Aliyev, V.Y. Kerimov, V.V. Kolodiya, etc.Data modeling was perfo

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Ganiyeva, R. Y. "LATERAL GROWTH OBJECTS IN SEDIMENTARY COVER OF SOUTH CASPIAN BASIN." Petroleum Engineering 17, no. 6 (2019): 15. http://dx.doi.org/10.17122/ngdelo-2019-6-15-22.

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Gahramanov, G., M. Babayev, S. Shpyrko, and Kh Mukhtarova. "SUBSIDENCE HISTORY AND HYDROCARBON MIGRATION MODELING IN SOUTH CASPIAN BASIN." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 1 (88) (2020): 82–91. http://dx.doi.org/10.17721/1728-2713.88.12.

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We study the mechanisms of migration and spacial distribution of hydrocarbon deposits along a regional 1000 km long SW - NE seismic cross section of the South Caspian Basin. A retrospective 2D geological simulation of basin subsidence and sediment filling history is performed taking into account accompanying processes of thermal and catagenetic transformations of organic matter, and subsequent migration and accumulation of hydrocarbons. The start of the basin opening with accumulation of considerable sedimentary mass can be dated as middle Mesozoic (Triassic or Jurassic), and hydrocarbon prone

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35

Kagramanov, G. N., and R. V. Veliyev. "PROSPECTIVE DEEP OIL-GAS FEATURES IN THE SOUTH CASPIAN BASIN." Geology and Mineral Resources of World Ocean 12, no. 3 (2016): 76–88. http://dx.doi.org/10.15407/gpimo2016.03.076.

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36

Ghafarian, Parvin, and Sahar Tajbakhsh. "SIGNATURE OF THE CLIMATE CHANGE IN THE SOUTH CASPIAN BASIN AND COASTAL AREA." Journal of Oceanological Research 47, no. 5 (2019): 12–25. http://dx.doi.org/10.29006/1564-2291.jor-2019.47(5).2.

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The climate change is the main issue in recent decades. Marine and coastal areas are deeply affected by climate change. To investigate the effect of climate change in the southern coast of the Caspian Sea, the variations of main meteorological parameters such as anomaly of minimum and maximum temperature, precipitation, sea surface temperature and, also the frequency of foggy, hazy and dusty days are examined in a 40-year period from 1979 to 2018 (anomalies with respect to the 1981–2010 baseline). The results of the study showed that the significant increasing trend in temperature in all stati

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37

Aliyeva, S., and A. Nasibov. "GEOLOGICAL CONDITIONS AND FEATURES OF MUD VOLCANOES IN THE SOUTH CASPIAN BASIN." Scientific heritage, no. 90 (June 6, 2022): 11–13. https://doi.org/10.5281/zenodo.6616126.

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The article deals with the development and spatial distribution of mud volcanoes in the waters of the South Caspian (in particular, the Baku archipelago), the characteristic features of the mud volcanic process, the main differences and similarities between marine and terrestrial mud volcanoes. It was found that by analyzing the products of mud volcanism it is possible to determine the age of deposits and the geological structure of the deep layers of the Earth. The geodynamic regime also affects the accumulation of hydrocarbons and the formation of traps. The system of anticlines of the Baku

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Yazmyradova, Gulbahar, Maman Hermana, and Hassan Soleimani. "Estimation of porosity from well logs and seismic using artificial neural network." IOP Conference Series: Earth and Environmental Science 1003, no. 1 (2022): 012017. http://dx.doi.org/10.1088/1755-1315/1003/1/012017.

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Abstract The Artificial Neural Network (ANN) is widely used to map and estimate reservoir properties. Since ANN has the ability of non-linear computing and self-error correction, it serves as an alternative method to enhance reservoir characterization by improving reservoir properties' prediction. This study employed an integrated approach where seismic, and well log data are used alongside ANN to evaluate petrophysical properties in Field X, South Caspian Basin. The study field is situated in the South Caspian Basin, which developed during Tertiary-Quaternary. The South Caspian Basin covers t

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Bagirov, E. B. "The characteristics and geodynamic mechanisms of formation of traps in Middle Caspian basin." Azerbaijan Oil Industry, no. 01 (January 15, 2023): 10–14. http://dx.doi.org/10.37474/0365-8554/2023-1-10-14.

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The structures of Middle Caspian basin differ from folded ones of South Caspian. The paper presents the researches of geodynamic processes in Middle Caspian basin and the types of traps formed due to them. Five structural types characteristic for the Middle Caspian basin, which can play a role of traps for hydrocarbons, are described. The significance of concept of formation process of each structure type for the specification of direction of exploration surveys in this region is shown as well. The most interesting of them in the context of geodynamic development are the inversion structures a

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Maloney, Richard F., Albert L. Rebergen, Ron J. Nilsson, and Nicky J. Wells. "Bird density and diversity in braided river beds in the Upper Waitaki: Basin, South Island, New Zealand." Notornis 44, no. 4 (1997): 219. https://doi.org/10.63172/250985aevuag.

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Wetland birds on 11 rivers of the Upper Waitaki Basin, South Island, New Zealand were surveyed annually between 1991 – 1994. Diversity, minimum abundance and density of birds were compared. In total 26 species of wetland birds were recorded. Minimum estimated river bird numbers were: 3566 Black-backed Gulls (Larus dominicanus), 3302 Black-fronted Terns (Sterna albostriata), 3260 Banded Dotterels (Charadrius bicinctus), 793 Black-billed Gulls (Larus bulleri), 789 Wrybills (Anarhynchus frontalis), 788 South Island Pied Oystercatchers (Haematopus ostralegus), 421 Pied Stilts (Himantopus himantopu

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Yusubov, N. P., I. S. Guliyev, and Juan I. Soto. "Time and mechanism of formation of mud volcanoes in the South Caspian basin according to seismic data." Azerbaijan Oil Industry, no. 04 (April 15, 2024): 4–14. http://dx.doi.org/10.37474/0365-8554/2024-04-4-14.

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There are 277 mud volcanoes located in the South Caspian basin and the Apsheron-Gobustan periclinal trough and the Lower Kura depression that open to it. On land there are 177 mud volcanic structures, from which steam, water, mud, gas and oil are constantly erupting at approximately 500 points. Mud volcanoes located in the Caspian Sea (about 100) also play an important role in the degassing (mainly methane) of the sedimentary layer of the earth’s crust. Based on the results of geological and geophysical research, it has been established that almost all mud volcanoes discovered on the territory

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Vetlugina, Tatiana. "RETROSPECTIVE ANALYSIS OF CATCHES AND STOCK DYNAMICS OF RUDD IN VOLGA-CASPIAN AND NORTHERN CASPIAN SUBAREAS." Fisheries 2020, no. 1 (2020): 52–56. http://dx.doi.org/10.37663/0131-6184-2020-1-52-56.

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Rudd is one of the most abundant species in the large group of minnow in the Volga-Caspian and Northern-Caspian fishery subareas of the Volga–Caspian fishery basin south. The article contains the data on its catches and usable stocks during ХХ – ХХI centuries. A long term analysis of the rudd catches and the runoff volume during the spring high water showed no substantial connection between these processes due to the rudd’s ecological peculiarities. The dynamics of the rudd catches and the level of the Caspian Sea are connected in inverse ratio. Inverse correlations with high determination coe

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Gurban Yetirmishli, Afag Samadzade, Gurban Yetirmishli, Afag Samadzade. "THE ROLE OF MUD VOLCANOES IN THE FORMATION OF OIL AND GAS STRUCTURES OF THE SOUTHERN CASPIAN BASIN." PAHTEI-Procedings of Azerbaijan High Technical Educational Institutions 48, no. 01 (2025): 18–26. https://doi.org/10.36962/pahtei48012025-18.

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The research work considered the issue of the formation of oil and gas structures of mud volcanoes, and also analyzed the geological structure of the South Caspian Basin. In addition, the presented article characterized the South Caspian depression as being covered by a sedimentary cover with a thickness of more than 30 km, along with the widespread manifestation of mud volcanism. Therefore, the issue of studying the area, taking into account the regularity of the distribution, number and activity of mud volcanoes within the framework of the research, is considered relevant. Based on the resea

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Lazarev, Sergei, Elisabeth L. Jorissen, de Velde Sabrina van, et al. "Magneto-biostratigraphic age constraints on the palaeoenvironmental evolution of the South Caspian basin during the Early-Middle Pleistocene (Kura basin, Azerbaijan)." Quaternary Science Reviews 222 (October 31, 2019): 1–26. https://doi.org/10.1016/j.quascirev.2019.105895.

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Lazarev, Sergei, Jorissen, Elisabeth L., van de Velde, Sabrina, Rausch, Lea, Stoica, Marius, Wesselingh, Frank P., Van Baak, Christiaan G.C., Yanina, Tamara A., Aliyeva, Elmira, Krijgsman, Wout (2019): Magneto-biostratigraphic age constraints on the palaeoenvironmental evolution of the South Caspian basin during the Early-Middle Pleistocene (Kura basin, Azerbaijan). Quaternary Science Reviews (e105895) 222: 1-26, DOI: 10.1016/j.quascirev.2019.105895, URL: http://dx.doi.org/10.1016/j.quascirev.2019.105895

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Abbasi, Keyvan, Atta Mouludi-Saleh, and Soheil Eagderi. "Morphological diversity of the Caspian Asp, Leuciscus aspius, in the South Caspian Sea basin (Osteichthyes: Cyprinidae)." Zoology in the Middle East 67, no. 1 (2021): 25–31. http://dx.doi.org/10.1080/09397140.2021.1879439.

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Ahmadov, E. H. "The study of regularities of distribution of reservoir parameters." Azerbaijan Oil Industry, no. 12 (December 15, 2022): 4–9. http://dx.doi.org/10.37474/0365-8554/2022-12-4-9.

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The parameters of reservoir should be specified in order to calculate hydrocarbon reserves. In particular, the uncertainty of reservoir parameters occurs mostly in the new areas. Thus, for the geological substantiation of reservoir parameters in these areas an analogy method is used. However, in the geological substantiation of reservoir parameters with analogical approach, it is essential to use the data on the field development in adjacent territories not in numerical order, but considering the distribution regularity. Such an approach allows specifying the uncertainty degree of reservoir pa

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Kerimov, N. "US POLICY TOWARDS DETERMINING TRANSPORT ROUTES OF CASPIAN BASIN OIL AND GAS RESOURCES." Scientific heritage, no. 155 (February 23, 2025): 23–26. https://doi.org/10.5281/zenodo.14914536.

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One of the factors that increases the geopolitical importance of the Caspian basin is its location at the intersection of energy transmission lines and east-west and north-south transport corridors. In the article, the interests of the United States, which is considered the world's superpower, in determining the export routes of the energy resources of the Caspian Sea are extensively analyzed. In the first sub-heading, the policy followed by the USA in the field of defining energy transport routes within the scope of its geo-economic interests in the Caspian Basin is analyzed. In the second su

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Piip, V. B., A. G. Rodnikov, and N. A. Buvaev. "The deep structure of the lithosphere along the Caucasus-South Caspian Basin-Apsheron Threshold-Middle-Caspian Basin-Turan plate seismic profile." Moscow University Geology Bulletin 67, no. 2 (2012): 125–32. http://dx.doi.org/10.3103/s0145875212020068.

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Katz, Barry J., Akif Narimanov, and Rafiga Huseinzadeh. "Significance of microbial processes in gases of the South Caspian basin." Marine and Petroleum Geology 19, no. 6 (2002): 783–96. http://dx.doi.org/10.1016/s0264-8172(02)00086-7.

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Yusifov, Mehdi, and Philip D. Rabinowitz. "Classification of mud volcanoes in the South Caspian Basin, offshore Azerbaijan." Marine and Petroleum Geology 21, no. 8 (2004): 965–75. http://dx.doi.org/10.1016/j.marpetgeo.2004.06.002.

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