COMPLEXES FILLING STRIKE-SLIP FAULT ZONES

dc.contributor.author	Kuteynikov Ye.S.
dc.contributor.author	Kuteynikova N.S.
dc.date.accessioned	2020-10-11T11:11:58Z
dc.date.available	2020-10-11T11:11:58Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31166748
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 6, 80-82
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17975
dc.description.abstract	The forms described here developed in fault zones when the rocks were affected by dynamic factors (pressure). The aim of this work is to classify faults according to their mechanics in accordance with the idea that they are divided into those generated by processes of shear and separation, i.e., into strike-slips and tension faults. When sheared, the rocks are affected by the dynamic load and transformed by it.
dc.title	COMPLEXES FILLING STRIKE-SLIP FAULT ZONES
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.