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- W2023930034 abstract "By analogy with the extremely rich Mexican petroliferous barrier-reef La Reforma trend, and on the basis of a paleogeomorphic analysis of geologic-geophysical data, the reefal edge of the South Caspian Basin of Neocomian age has been recognized in Southwestern Turkmenia; this is promising with respect to oil and gas exploration in combined (structural-reefal) traps. The extent of the reefal scarp is about 400 km in the terrestrial part, with an amplitude of up to 1500-2000 m, the width of the crest is about 5 km, and the depth of occurrence is 3000-4500 m. In its sublatitudinal part, the reef coincides with the Near-Balkhan zone of structures, productive in the Pliocene sequence. In its submeridional part, it corresponds to the so-called Shordzha-Gekcha fault and has been built over by a Cretaceous diapiric clay swell. The paleogeomorphic plan in the South Caspian petroliferous basin, apart from Southwestern Turkmenia, suggests the distribution of the marginal barrier-reef scarp beyond the water area of the Caspian Sea and the Kura Basin." @default.
- W2023930034 created "2016-06-24" @default.
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- W2023930034 date "1982-07-01" @default.
- W2023930034 modified "2023-09-25" @default.
- W2023930034 title "The reefal margin of the South Caspian Basin and its petroleum prospects (Southwestern Turkmenia)" @default.
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- W2023930034 doi "https://doi.org/10.1080/00206818209449619" @default.
- W2023930034 hasPublicationYear "1982" @default.
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