Neogene-Eopleistocene shelly limestones in the North Caucasus and Ciscaucasia regions
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  • 作者：E. V. Beluzhenko (1)
  • 关键词：shell ; detrital limestones ; Neogene ; Middle ; Upper Miocene ; Pliocene ; Eopleistocene ; North Caucasus ; Ciscaucasia
  • 刊名：Stratigraphy and Geological Correlation
  • 出版年：2014
  • 出版时间：July 2014
  • 年：2014
  • 卷：22
  • 期：4
  • 页码：406-425
  • 全文大小：1,394 KB
  • 参考文献：1. Beluzhenko, E.V., Kovalenko, E.I., and Pis鈥檓ennaya, N.S., Stratigraphy of Oligocene-Eopleistocene deposits of Northern Osetia (sheet: K-37-IX), in / Problemy Geologii, geoekologii i mineragenii Yuga Rossii i Kavkaza. Materialy V Mezhdunarodnoi nauchnoi konferentsii, Novocherkassk, 28 aprelya 2006 g. (Proc. V Int. Sci. Conf. 鈥淧roblems of Geology, Geoecology, and Minerageny of South Russia and Caucasus鈥?, Novocherkassk: Temp, 2006, pp. 40鈥?5.
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  • 作者单位：E. V. Beluzhenko (1)

    1. Open Joint-Stock Company Kabardino-Balkarskaya Geologo-Razvedochnaya Ekspeditsiya, ul. Kalinina 262, Nalchik, 360000, Russia
  • ISSN：1555-6263
文摘
In the North Caucasus and Ciscaucasia, seven distribution zones of Middle-Upper Miocene, Pliocene, and Eopleistocene shell-detrital limestones are defined: Lower Don, Tsimlyansk-Manych, Western Ciscaucasia, Western Caucasus, Central Ciscaucasia, Kabarda-Chechen, and Eastern Dagestan. The shell-detrital limestones are present among sandy-clayey sediments in the form of intercalations of variable thickness traceable over different distances (up to a few kilometers). The maximum thicknesses of such limestones are characteristic of the Neogene sections in the northwestern pericline of the Greater Caucasus: Taman-Adagum area, where their distribution comprises the stratigraphic interval from the Chokrakian to early Cimmerian regional stages (approximately 10 m.y. long). Their most spacious distribution area is confined to the Central Ciscaucasia zone. The shell-detrital limestones in the Neogene sections mark shallowwater shelf areas (ancient coastal bars, banks, and shoals) with intermittently forming environments favorable for accumulation of significant volumes of shelly detritus. In such paleogeographic settings, the sediments were subjected to repeated erosion with subsequent formation of limestones. Now, they represent building material widely used in the region for different purposes.

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