期刊
DOKLADY EARTH SCIENCES
卷 430, 期 2, 页码 155-157出版社
MAIK NAUKA/INTERPERIODICA/SPRINGER
DOI: 10.1134/S1028334X10020017
关键词
-
资金
- Russian Foundation [08-05-00588a]
Using seismic evidence and other geological data, a balanced section has been built for the Tuapse foredeep-Western Caucasus-Western Kuban foredeep tectonic system. This section enabled us to restore the history of the region, from the Callovian time. It was suggested that, in the Callovian-Eocene, the western Caucasian basin existed in the form of a rift. The principal phase of rift inversion occurred in the Oligocene-Miocene, and in the Pliocene-Quaternary, it evolved into the orogeny phase. The extent of the Caucasus compression within the section area was more than 30 km.
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