ORIGIN OF STRONG INTRAPLATE EARTHQUAKES

dc.contributor.author	Vinnik L.P.
dc.date.accessioned	2020-10-06T05:04:54Z
dc.date.available	2020-10-06T05:04:54Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31076327
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 6, 37-38
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17701
dc.description.abstract	The foci of strong tremors are generally confined to long-lived active faults. However, some earthquakes occur at great distances from the boundaries of lithospheric plates, and the seismic events which occur in the stable continental crust (SCC) constitute a special category. The purpose of the present article is to compare and logically connect certain properties of seismogenic zones of SCC regions, and to come up with a hypothesis (susceptible to experimental verification) that could serve as a starting point for the development of geophysical methods for identifying zones of high seismic risk in SCC regions.
dc.title	ORIGIN OF STRONG INTRAPLATE EARTHQUAKES
dc.type	Статья

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