NEW DATA ON THE STRUCTURE OF SEDIMENTARY COVER AT THE CAPE VERDE SEAMOUNT AND THE CAPE VERDE BASIN (CENTRAL ATLANTIC) BASED ON CONTINUOUS SEISMIC PROFILING DATA

Efimov V.N.; Skolotnev S.G.

dc.contributor.author	Efimov V.N.
dc.contributor.author	Skolotnev S.G.
dc.date.accessioned	2024-11-02T11:07:52Z
dc.date.available	2024-11-02T11:07:52Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520501
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 3, 376-380
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46361
dc.description.abstract	he transition zones between oceanic and continental lithospheres at Atlantic-type margins remain poorly studied. The data available indicate that these regions are distinguished by specific tectonic and igneous activity. The results of several expeditions conducted by the Geological Institute near the rise of the African continental slope south of Cape Verde Islands support this statement. The systems of transform fracture zones (TFZ) that extend to the south of the Fifteen Twenty TFZ pinch out in this area.
dc.title	NEW DATA ON THE STRUCTURE OF SEDIMENTARY COVER AT THE CAPE VERDE SEAMOUNT AND THE CAPE VERDE BASIN (CENTRAL ATLANTIC) BASED ON CONTINUOUS SEISMIC PROFILING DATA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0603007X