Matches in SemOpenAlex for { <https://semopenalex.org/work/W4365812892> ?p ?o ?g. }
- W4365812892 endingPage "229838" @default.
- W4365812892 startingPage "229838" @default.
- W4365812892 abstract "We determined the basement depths in the fold-and-thrust belt (FTB) and the associated Aruma and Pabdeh foreland basins of the United Arab Emirates. Additionally, we investigated the relationship between shallow sedimentary structures and deep basement features. The Late Cretaceous Aruma basin is associated with Semail ophiolite thrusting and loading, while the late Oligocene to Miocene Pabdeh basin is associated with the culmination of Musandam and early Zagros collision. In the northern portions of the study area, seismic reflection profiles and derivative maps of gravity and magnetic data show NNW–SSE striking thrusts, backthrusts, and folds. The southern region around Jabal Hafit is dominated by the Tarabat backthrust, which cuts across the Upper Cretaceous and Cenozoic successions. Moreover, the Mesozoic platform carbonates are dissected by thrust faults. These thrusts may have originated from Jurassic extensional faults that were reactivated during the Late Cretaceous ophiolite obduction, as well as the late Oligocene to the early Miocene culmination of Musandam resulting from the collision of the Arabian Plate and Central Iran along the Zagros Suture. Results of the 3D gravity inversion indicate that the basement depths range from 11.5 km along uplifted areas of the FTB to 18.8 km within the deeper parts of the foreland basin. Significant northward increases in both basement depth and the thickness of the late Oligocene-early Miocene successions indicate a northward increase in the severity of thrusting and crustal loading along the Khusub thrust. The basement uplifts are found to be correlated with shallower anticlinal features, indicating a direct relationship between basement uplifts and shallow sedimentary structures. Therefore, we suggest that the basement structures were reactivated during the Late Cretaceous ophiolite obduction and the late Oligocene-early Miocene Zagros collision." @default.
- W4365812892 created "2023-04-16" @default.
- W4365812892 creator A5002404863 @default.
- W4365812892 creator A5004105550 @default.
- W4365812892 creator A5078913490 @default.
- W4365812892 creator A5087258938 @default.
- W4365812892 date "2023-06-01" @default.
- W4365812892 modified "2023-10-15" @default.
- W4365812892 title "Basement morphology of the fold-and-thrust belt and foreland basin of the United Arab Emirates: Evidence for thick-skinned tectonics in the northern Oman-UAE Mountains" @default.
- W4365812892 cites W1546293839 @default.
- W4365812892 cites W1669380268 @default.
- W4365812892 cites W1849948281 @default.
- W4365812892 cites W1968874005 @default.
- W4365812892 cites W1981545340 @default.
- W4365812892 cites W1985748982 @default.
- W4365812892 cites W1986550752 @default.
- W4365812892 cites W1995764164 @default.
- W4365812892 cites W2018568653 @default.
- W4365812892 cites W2020974273 @default.
- W4365812892 cites W2032063496 @default.
- W4365812892 cites W2034524636 @default.
- W4365812892 cites W2037176839 @default.
- W4365812892 cites W2051983668 @default.
- W4365812892 cites W2062852444 @default.
- W4365812892 cites W2065247298 @default.
- W4365812892 cites W2068785216 @default.
- W4365812892 cites W2074163083 @default.
- W4365812892 cites W2079842543 @default.
- W4365812892 cites W2083772074 @default.
- W4365812892 cites W2088533800 @default.
- W4365812892 cites W2100232339 @default.
- W4365812892 cites W2108855048 @default.
- W4365812892 cites W2115092948 @default.
- W4365812892 cites W2122975106 @default.
- W4365812892 cites W2145995786 @default.
- W4365812892 cites W2154733372 @default.
- W4365812892 cites W2155730907 @default.
- W4365812892 cites W2168168701 @default.
- W4365812892 cites W2170482959 @default.
- W4365812892 cites W2186549523 @default.
- W4365812892 cites W2188209491 @default.
- W4365812892 cites W2259645488 @default.
- W4365812892 cites W2283545049 @default.
- W4365812892 cites W2302174328 @default.
- W4365812892 cites W2622650055 @default.
- W4365812892 cites W2804272421 @default.
- W4365812892 cites W2807997537 @default.
- W4365812892 cites W2810148111 @default.
- W4365812892 cites W2885402384 @default.
- W4365812892 cites W2893144252 @default.
- W4365812892 cites W2925183314 @default.
- W4365812892 cites W2947373622 @default.
- W4365812892 cites W2955574704 @default.
- W4365812892 cites W2960608112 @default.
- W4365812892 cites W2992040756 @default.
- W4365812892 cites W2999006960 @default.
- W4365812892 cites W3028628319 @default.
- W4365812892 cites W3033728818 @default.
- W4365812892 cites W3036894459 @default.
- W4365812892 cites W3041421974 @default.
- W4365812892 cites W3089995550 @default.
- W4365812892 cites W3182576933 @default.
- W4365812892 cites W3186725027 @default.
- W4365812892 cites W335357478 @default.
- W4365812892 cites W4213429578 @default.
- W4365812892 cites W4223638870 @default.
- W4365812892 cites W4280496939 @default.
- W4365812892 cites W4281625749 @default.
- W4365812892 cites W4282835425 @default.
- W4365812892 cites W4296209044 @default.
- W4365812892 doi "https://doi.org/10.1016/j.tecto.2023.229838" @default.
- W4365812892 hasPublicationYear "2023" @default.
- W4365812892 type Work @default.
- W4365812892 citedByCount "0" @default.
- W4365812892 crossrefType "journal-article" @default.
- W4365812892 hasAuthorship W4365812892A5002404863 @default.
- W4365812892 hasAuthorship W4365812892A5004105550 @default.
- W4365812892 hasAuthorship W4365812892A5078913490 @default.
- W4365812892 hasAuthorship W4365812892A5087258938 @default.
- W4365812892 hasConcept C109007969 @default.
- W4365812892 hasConcept C12294951 @default.
- W4365812892 hasConcept C127313418 @default.
- W4365812892 hasConcept C127413603 @default.
- W4365812892 hasConcept C147176958 @default.
- W4365812892 hasConcept C1507633 @default.
- W4365812892 hasConcept C151730666 @default.
- W4365812892 hasConcept C153220577 @default.
- W4365812892 hasConcept C165205528 @default.
- W4365812892 hasConcept C1893757 @default.
- W4365812892 hasConcept C193748577 @default.
- W4365812892 hasConcept C2781297371 @default.
- W4365812892 hasConcept C53942344 @default.
- W4365812892 hasConcept C6494504 @default.
- W4365812892 hasConcept C73707237 @default.
- W4365812892 hasConcept C77928131 @default.
- W4365812892 hasConcept C78519656 @default.
- W4365812892 hasConceptScore W4365812892C109007969 @default.
- W4365812892 hasConceptScore W4365812892C12294951 @default.