RADIOPROBING OF UNDERGROUND STRUCTURE OF THE FAILURE GULF, FORMED AS A RESULT OF THE M7.5 TSAGAN EARTHQUAKE

Bashkuev Yu.B.; Khaptanov V.B.; Dembelov M.G.; Angarkhaeva L.Kh.; Boloev V.P.; Hayakawa M.

dc.contributor.author	Bashkuev Yu.B.
dc.contributor.author	Khaptanov V.B.
dc.contributor.author	Dembelov M.G.
dc.contributor.author	Angarkhaeva L.Kh.
dc.contributor.author	Boloev V.P.
dc.contributor.author	Hayakawa M.
dc.date.accessioned	2025-05-19T06:46:14Z
dc.date.available	2025-05-19T06:46:14Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=13523327
dc.identifier.citation	Physics and Chemistry of the Earth, Parts A/B/C, 2006, 31, 4-9, 210-214
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/49307
dc.description.abstract	The Failure Gulf of the Baikal Lake was formed after a strong earthquake when dry land was lowered under the Baikal Lake water. Geoelectric characteristics of the seismotectonic structures of the studied region are described. Now the foundation of the gulf continues to depress. A border between modern bottom sediments and “paleo-soil” was revealed by means of method of radioimpedance sounding. Underground structure and electrophysical properties of the Failure Gulf of the Baikal Lake are defined.
dc.title	RADIOPROBING OF UNDERGROUND STRUCTURE OF THE FAILURE GULF, FORMED AS A RESULT OF THE M7.5 TSAGAN EARTHQUAKE
dc.type	Статья