DEPOSITIONAL AND TECTONIC FRAMEWORK OF THE RIFT BASINS OF LAKE BAIKAL FROM MULTICHANNEL SEISMIC DATA

dc.contributor.author	Hutchinson D.R.
dc.contributor.author	Golmshtok A.J.
dc.contributor.author	Zonenshain L.P.
dc.contributor.author	Moore T.C.
dc.contributor.author	Scholtz C.A.
dc.contributor.author	Klitgord K.D.
dc.date.accessioned	2020-11-07T08:52:20Z
dc.date.available	2020-11-07T08:52:20Z
dc.date.issued	1992
dc.identifier	https://elibrary.ru/item.asp?id=29052639
dc.identifier.citation	Geology, 1992, , 7, 589-592
dc.identifier.issn	0091-7613
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18664
dc.description.abstract	Recent multichannel seismic reflection data from Lake Baikal, located in a large, active, continental rift in central Asia, image three major stratigraphic units totaling 3.5 to 7.5 km thick in four subbasins. A major change in rift deposition and faulting between the oldest and middle-rift units probably corresponds to the change from slow to fast rifting in early Pliocene time inferred from on-land studies. A minor modification of fault patterns characterizes the youngest unit. A brief comparison of the basins of Lake Baikal with those of the East African rift system highlights differences in structural style that can be explained by differences in age and evolution of the surrounding basement rocks.
dc.subject	Pliocene	en
dc.title	DEPOSITIONAL AND TECTONIC FRAMEWORK OF THE RIFT BASINS OF LAKE BAIKAL FROM MULTICHANNEL SEISMIC DATA
dc.type	Статья
dc.subject.age	Cenozoic::Neogene::Pliocene	en
dc.subject.age	Кайнозой::Неоген::Плиоцен	ru

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