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- Transfer_zone abstract "A transfer zone in geology is an area where deformational strain is transferred from one structural element to another typically from fault to fault in rift systems. Therefore, listric faults and monoclinal folds in the hanging wall are typical structures linked by transfer zones; however, complexities do exist. The terms interbasin and intrabasin transfer zones have been proposed to delineate the magnitude of the transfer zone. Transfer zones can be described according to the fault dip directions; synthetic or conjugate and according to their deformation style; convergent or divergent. Transfer zones can be farther identified by its maturity or (fault propagation evolution); whether the major fault relationship is approaching, overlapping, collateral or collinear. Since transfer zones are normally found in extensional settings many studies have been done within the East African rift system and the Gulf of Suez rift system. Transfer zones have also played a role in hydrocarbon exploration and extraction within the Albertine graben.".
- Transfer_zone wikiPageID "39341090".
- Transfer_zone wikiPageLength "8316".
- Transfer_zone wikiPageOutDegree "7".
- Transfer_zone wikiPageRevisionID "683267035".
- Transfer_zone wikiPageWikiLink Category:Structural_geology.
- Transfer_zone wikiPageWikiLink Category:Tectonics.
- Transfer_zone wikiPageWikiLink East_African_Rift.
- Transfer_zone wikiPageWikiLink Fault_(geology).
- Transfer_zone wikiPageWikiLink Gulf_of_Suez_rift.
- Transfer_zone wikiPageWikiLink Lake_Malawi.
- Transfer_zone wikiPageWikiLink Rift.
- Transfer_zone wikiPageWikiLinkText "Transfer zone".
- Transfer_zone wikiPageUsesTemplate Template:Orphan.
- Transfer_zone wikiPageUsesTemplate Template:Reflist.
- Transfer_zone subject Category:Structural_geology.
- Transfer_zone subject Category:Tectonics.
- Transfer_zone hypernym Area.
- Transfer_zone type Place.
- Transfer_zone comment "A transfer zone in geology is an area where deformational strain is transferred from one structural element to another typically from fault to fault in rift systems. Therefore, listric faults and monoclinal folds in the hanging wall are typical structures linked by transfer zones; however, complexities do exist. The terms interbasin and intrabasin transfer zones have been proposed to delineate the magnitude of the transfer zone.".
- Transfer_zone label "Transfer zone".
- Transfer_zone sameAs Q18394813.
- Transfer_zone sameAs m.011lg35_.
- Transfer_zone sameAs Q18394813.
- Transfer_zone wasDerivedFrom Transfer_zone?oldid=683267035.
- Transfer_zone isPrimaryTopicOf Transfer_zone.