Nature of the North Caspian gravity anomaly

With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12...

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Published in:Geotectonics 2007-05, Vol.41 (3), p.195-209
Main Authors: Segalovich, V. I., Volozh, Yu. A., Antipov, M. P., Vasil’ev, O. A.
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Language:English
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Paleozoic
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description With the use of the method of complete geological reduction, it has been shown that the unique gravity anomaly that frames the Near-Caspian petroliferous basin in the south is related to the Lower Paleozoic volcanic-terrigenous complex that occurs at the base of sedimentary cover at a depth of 8-12 km. This complex was formed contemporaneously with spreading of the Ural-Turkistan ocean and mark a rift zone in the south of passive margin of the East European continent. The rift was conjugated with an ancient triple junction on the floor of the Ural-Turkistan paleocean.[PUBLICATION ABSTRACT]
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subjects Geology
Paleozoic
title Nature of the North Caspian gravity anomaly
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