THE RELATION OF EARTHQUAKE FOCI TO FAULTS AND THE MOST RECENT MOVEMENTS OF SOUTHERN ASIA

dc.contributor.author	Khromovskikh V.S.
dc.date.accessioned	2020-04-08T08:53:51Z
dc.date.available	2020-04-08T08:53:51Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30947380
dc.identifier.citation	JOURNAL OF GEODYNAMICS, 1988, 10, 2-4, 233-241
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16426
dc.description.abstract	This study presents an analysis of the interrelations between 700 earthquake foci (with M = 6-8 and M > 8) for the period from 1900 to 1980 and fault tectonics and neotectonic deformations in the territory of new folded belts and platforms in Southern Asia rejuvenated in the Cenozoic. The study shows that the seismic activity of ancient faults, that were tectonically passive in the Cenozoic, is nearly the same as that of the Cenozoic counterparts. Besides, it is established that the majority of earthquake foci are related to uplift regions, in which amounts of neotectonic deformation reach intermediate and minimum values, rather than to regions of maximum crustal deformations.
dc.subject	Cenozoic	en
dc.title	THE RELATION OF EARTHQUAKE FOCI TO FAULTS AND THE MOST RECENT MOVEMENTS OF SOUTHERN ASIA
dc.type	Статья
dc.subject.age	Cenozoic	en
dc.subject.age	Кайнозой	ru

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