FAULT PATTERN IN CONTINENTAL ZONES OF LITHOSPHERIC EXTENSION

dc.contributor.author	Seminsky K.Zh.
dc.date.accessioned	2022-05-02T07:48:53Z
dc.date.available	2022-05-02T07:48:53Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=14996619
dc.identifier.citation	Geologiya i Geofizika, 2004, 45, 4, 443-454
dc.identifier.issn	0016-7886
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/37316
dc.description.abstract	A typical pattern shared by second-order faults in extended lithosphere was revealed based on field geological and structural data from the Obruchev Fault in the Baikal Rift and published evidence of rift-related faulting worldwide. The typical fault family is dominated by rift-parallel synthetic and antithetic normal faults and includes transverse faults of normal, strike-slip, and oblique slip geometry and rift-parallel reverse faults and thrusts. The coexistence of faults of various types within first-order extension zones is accounted for by accommodation of shear strain and by the kinematics of large basin-parallel normal faults. The suggested typical pattern can be used for reference in interpretation of faulting histories in rifted continental lithosphere.
dc.subject	Faults
dc.subject	faulting pattern
dc.subject	Baikal rift
dc.subject	zones of extension
dc.title	FAULT PATTERN IN CONTINENTAL ZONES OF LITHOSPHERIC EXTENSION
dc.type	Статья

Files in this item

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