Matches in SemOpenAlex for { <https://semopenalex.org/work/W2955011656> ?p ?o ?g. }
Showing items 1 to 89 of
89
with 100 items per page.
- W2955011656 endingPage "36" @default.
- W2955011656 startingPage "1" @default.
- W2955011656 abstract "The southern parts of the un-elevated (Foothills zone) folded belt in Iraq includes the area of Kirkuk and Diyala governorates. It is part of the Zagros fold thrust belt and it is characterized by presence of long relatively narrow northwest trending anticlines separated by broad flat bottom synclines. The northeastern flanks of all the exposed anticlines suffered from thrusting parallel to their axial trends. The surface thrusts always initiate within the salt bearing horizons of the Lower – Middle Miocene mobile sequence and migrate up stratigraphy to the post-Middle Miocene upper competent sequence. The pre-Miocene lower competent sequence is always affected by at least two high angles major up thrusts dipping toward each others, and trending parallel to the axial trend of the major anticlines.Geometrical analyses based on surface and subsurface (seismic and drill holes) data elucidate the following. The major anticlines are fault propagation folds formed in response to the thrust movements on the major up thrusts. Thickness variations of the Maestrichtian strata across the major up thrusts postulates that these up thrusts were actually normal faults forming grabens and half grabens during the Maestrichtian age. Reactivation of the extension movements on these grabens during the lower and the middle Miocene ages resulted in the restricted deposition of the lower and the middle Miocene rock salt facies of both Dhiban and Fatha Formations.Compressive stress field acting during and after the Pliocene resulted in inversion of movements of the former normal faults and converts them into up thrusts and also resulted into formation of the major and the minor structures of the studied area. The on lapping of Maqdadiah – Bai Hassan sequences over the top of Injanah Formation postulates that the contraction and the elevation of the major anticlines were started at the onset of the Pliocene. This contraction phase was coaxial with the former extension phases, and both were oriented in NE – SW direction.The major structures were formed by a combination of neutral surface flexure slip and flow, and body translation mechanisms. The flexure slip and flow of therocks of the mobile sequence resulted into formation of several types of duplexes and triangle zones. The lower Miocene reservoir rocks are intensively influenced by these duplexes and triangle zones especially at the down flanks of the major anticlines and beneath the surface synclines. This criterion has a special importance in the oil industry." @default.
- W2955011656 created "2019-07-12" @default.
- W2955011656 creator A5004089820 @default.
- W2955011656 creator A5050620844 @default.
- W2955011656 date "2005-01-01" @default.
- W2955011656 modified "2023-09-23" @default.
- W2955011656 title "INVERSION AND FOLDING OF THE SOUTHERN UN-ELEVATED FOLDED BELT IN NORTH IRAQ" @default.
- W2955011656 cites W1902422292 @default.
- W2955011656 cites W1993744042 @default.
- W2955011656 cites W2001231214 @default.
- W2955011656 cites W2026903476 @default.
- W2955011656 cites W2058192699 @default.
- W2955011656 cites W2073951015 @default.
- W2955011656 cites W2134946466 @default.
- W2955011656 cites W2293077824 @default.
- W2955011656 cites W2325360446 @default.
- W2955011656 hasPublicationYear "2005" @default.
- W2955011656 type Work @default.
- W2955011656 sameAs 2955011656 @default.
- W2955011656 citedByCount "1" @default.
- W2955011656 countsByYear W29550116562020 @default.
- W2955011656 crossrefType "journal-article" @default.
- W2955011656 hasAuthorship W2955011656A5004089820 @default.
- W2955011656 hasAuthorship W2955011656A5050620844 @default.
- W2955011656 hasConcept C109007969 @default.
- W2955011656 hasConcept C114679195 @default.
- W2955011656 hasConcept C116637073 @default.
- W2955011656 hasConcept C127313418 @default.
- W2955011656 hasConcept C127413603 @default.
- W2955011656 hasConcept C146588470 @default.
- W2955011656 hasConcept C149465734 @default.
- W2955011656 hasConcept C1507633 @default.
- W2955011656 hasConcept C151730666 @default.
- W2955011656 hasConcept C165205528 @default.
- W2955011656 hasConcept C166839181 @default.
- W2955011656 hasConcept C175551986 @default.
- W2955011656 hasConcept C1893757 @default.
- W2955011656 hasConcept C193748577 @default.
- W2955011656 hasConcept C52678131 @default.
- W2955011656 hasConcept C53942344 @default.
- W2955011656 hasConcept C69168840 @default.
- W2955011656 hasConcept C78519656 @default.
- W2955011656 hasConceptScore W2955011656C109007969 @default.
- W2955011656 hasConceptScore W2955011656C114679195 @default.
- W2955011656 hasConceptScore W2955011656C116637073 @default.
- W2955011656 hasConceptScore W2955011656C127313418 @default.
- W2955011656 hasConceptScore W2955011656C127413603 @default.
- W2955011656 hasConceptScore W2955011656C146588470 @default.
- W2955011656 hasConceptScore W2955011656C149465734 @default.
- W2955011656 hasConceptScore W2955011656C1507633 @default.
- W2955011656 hasConceptScore W2955011656C151730666 @default.
- W2955011656 hasConceptScore W2955011656C165205528 @default.
- W2955011656 hasConceptScore W2955011656C166839181 @default.
- W2955011656 hasConceptScore W2955011656C175551986 @default.
- W2955011656 hasConceptScore W2955011656C1893757 @default.
- W2955011656 hasConceptScore W2955011656C193748577 @default.
- W2955011656 hasConceptScore W2955011656C52678131 @default.
- W2955011656 hasConceptScore W2955011656C53942344 @default.
- W2955011656 hasConceptScore W2955011656C69168840 @default.
- W2955011656 hasConceptScore W2955011656C78519656 @default.
- W2955011656 hasLocation W29550116561 @default.
- W2955011656 hasOpenAccess W2955011656 @default.
- W2955011656 hasPrimaryLocation W29550116561 @default.
- W2955011656 hasRelatedWork W1604238471 @default.
- W2955011656 hasRelatedWork W1904767651 @default.
- W2955011656 hasRelatedWork W1974772377 @default.
- W2955011656 hasRelatedWork W1998274827 @default.
- W2955011656 hasRelatedWork W2009324021 @default.
- W2955011656 hasRelatedWork W2017040547 @default.
- W2955011656 hasRelatedWork W2021499990 @default.
- W2955011656 hasRelatedWork W2023351384 @default.
- W2955011656 hasRelatedWork W2024809700 @default.
- W2955011656 hasRelatedWork W2027521923 @default.
- W2955011656 hasRelatedWork W2033779701 @default.
- W2955011656 hasRelatedWork W2038582040 @default.
- W2955011656 hasRelatedWork W2043721786 @default.
- W2955011656 hasRelatedWork W2104623132 @default.
- W2955011656 hasRelatedWork W2120163775 @default.
- W2955011656 hasRelatedWork W2163135050 @default.
- W2955011656 hasRelatedWork W2181781799 @default.
- W2955011656 hasRelatedWork W2214787065 @default.
- W2955011656 hasRelatedWork W2979468867 @default.
- W2955011656 hasRelatedWork W3081977547 @default.
- W2955011656 isParatext "false" @default.
- W2955011656 isRetracted "false" @default.
- W2955011656 magId "2955011656" @default.
- W2955011656 workType "article" @default.