FAULT PATTERN IN CONTINENTAL ZONES OF LITHOSPHERIC EXTENSION
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
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. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru