FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2085798447> ?p ?o ?g. }

• W2085798447 endingPage "226" @default.
• W2085798447 startingPage "203" @default.
• W2085798447 abstract "The Cretaceous-Tertiary northwest-trending Sirt Basin system, Libya, is a rift/sag basin formed on Pan-African to Paleozoic-aged basement of North Africa. In this study, we investigate the rift-basin architecture and tectonic framework of the western Sirt Basin. Using remote sensed data, supported by borehole data from about 300 deep wells and surface geologic maps, we constructed geological cross sections and surface geology maps. Indication of the relative timing of structures and movement along faults has been determined where possible. Direction statistics for all the interpreted linear features acquired in the study area were calculated and given as a total distribution and then the totals are broken down by the major basin elements of the area. Hundreds of lineaments were recognized. Their lengths, range between a hundred meters up to hundreds of kilometers and the longest of the dominant trends are between N35W–N55W and between N55E–N65E which coincides with Sirt Basin structures. The produced rose diagrams reveal that the majority of the surface linear features in the region have four preferred orientations: N40-50W in the Zallah Trough, N45–55W in the Dur al Abd Trough, N35–55W in the Az Zahrah-Al Hufrah Platform, and in contrast in the Waddan Uplift a N55–65E trend. We recognize six lithostratigraphic sequences (phases) in the area’s stratigraphic framework. A Pre-graben (Pre-rift) initiation stage involved the Pre-Cretaceous sediments formed before the main Sirt Basin subsidence. Then followed a Cretaceous to Eocene graben-fill stage that can divided into four structurally-active and structurally-inactive periods, and finally a terminal continental siliciclastics-rich package representing the post-rift stage of the development in post-Eocene time. In general five major fault systems dissect and divide the study area into geomorphological elevated blocks and depressions. Most of the oil fields present in the study area are associated with structural hinge zones and adjoining highs. Late Eocene rocks exposed in the western part of the basin exhibit a complex network of branching segmented normal and strike-slip faults, generally with a NNW–SSE structural orientations. Many surface structural features have been interpreted from satellite images which confirm sinistral strike-slip kinematics. Relay ramp structures, numerous elongate asymmetric synclines associated with shallow west limbs and steeper dipping east limbs are developed in the hangingwalls adjacent to west downthrowing normal faults. These structural patterns reflect Cretaceous/Tertiary extensional tectonics with additional control by underlying pre-existing Pan-African basement fabrics and ENE–WSW trending Hercynian structures. We relate the Sirt Basin rift development as exemplified in our study area to the break-up of Gondwana represented by the structural evolution of the West-Central African rift system, and the South and Central Atlantic, the Tethys and the Indian Oceans." @default.
• W2085798447 created "2016-06-24" @default.
• W2085798447 creator A5045910083 @default.
• W2085798447 creator A5047318536 @default.
• W2085798447 date "2014-12-01" @default.
• W2085798447 modified "2023-10-02" @default.
• W2085798447 title "Rift architecture and evolution: The Sirt Basin, Libya: The influence of basement fabrics and oblique tectonics" @default.
• W2085798447 cites W119777211 @default.
• W2085798447 cites W1502373347 @default.
• W2085798447 cites W1964337549 @default.
• W2085798447 cites W1980966991 @default.
• W2085798447 cites W1988540193 @default.
• W2085798447 cites W1989003977 @default.
• W2085798447 cites W1996346422 @default.
• W2085798447 cites W2000579727 @default.
• W2085798447 cites W2001625261 @default.
• W2085798447 cites W2006254584 @default.
• W2085798447 cites W2009638437 @default.
• W2085798447 cites W2021321788 @default.
• W2085798447 cites W2021741467 @default.
• W2085798447 cites W2024793243 @default.
• W2085798447 cites W2032367455 @default.
• W2085798447 cites W2041983494 @default.
• W2085798447 cites W2046853743 @default.
• W2085798447 cites W2061207025 @default.
• W2085798447 cites W2067041472 @default.
• W2085798447 cites W2068580384 @default.
• W2085798447 cites W2068991796 @default.
• W2085798447 cites W2087370836 @default.
• W2085798447 cites W2093313937 @default.
• W2085798447 cites W2108998966 @default.
• W2085798447 cites W2120108738 @default.
• W2085798447 cites W2124969384 @default.
• W2085798447 cites W2126789535 @default.
• W2085798447 cites W2138960479 @default.
• W2085798447 cites W2150279239 @default.
• W2085798447 cites W2153210255 @default.
• W2085798447 cites W2154463579 @default.
• W2085798447 cites W2157320902 @default.
• W2085798447 cites W2168564774 @default.
• W2085798447 cites W2326091031 @default.
• W2085798447 cites W2330155903 @default.
• W2085798447 cites W2947307941 @default.
• W2085798447 cites W3123620808 @default.
• W2085798447 cites W4230903011 @default.
• W2085798447 cites W4250767209 @default.
• W2085798447 cites W4376043613 @default.
• W2085798447 doi "https://doi.org/10.1016/j.jafrearsci.2014.06.020" @default.
• W2085798447 hasPublicationYear "2014" @default.
• W2085798447 type Work @default.
• W2085798447 sameAs 2085798447 @default.
• W2085798447 citedByCount "17" @default.
• W2085798447 countsByYear W20857984472015 @default.
• W2085798447 countsByYear W20857984472016 @default.
• W2085798447 countsByYear W20857984472017 @default.
• W2085798447 countsByYear W20857984472019 @default.
• W2085798447 countsByYear W20857984472021 @default.
• W2085798447 countsByYear W20857984472022 @default.
• W2085798447 countsByYear W20857984472023 @default.
• W2085798447 crossrefType "journal-article" @default.
• W2085798447 hasAuthorship W2085798447A5045910083 @default.
• W2085798447 hasAuthorship W2085798447A5047318536 @default.
• W2085798447 hasConcept C109007969 @default.
• W2085798447 hasConcept C114793014 @default.
• W2085798447 hasConcept C12294951 @default.
• W2085798447 hasConcept C127313418 @default.
• W2085798447 hasConcept C127413603 @default.
• W2085798447 hasConcept C139719470 @default.
• W2085798447 hasConcept C147176958 @default.
• W2085798447 hasConcept C151730666 @default.
• W2085798447 hasConcept C162324750 @default.
• W2085798447 hasConcept C166839181 @default.
• W2085798447 hasConcept C2781297371 @default.
• W2085798447 hasConcept C32239851 @default.
• W2085798447 hasConcept C50682988 @default.
• W2085798447 hasConcept C77928131 @default.
• W2085798447 hasConcept C92596616 @default.
• W2085798447 hasConceptScore W2085798447C109007969 @default.
• W2085798447 hasConceptScore W2085798447C114793014 @default.
• W2085798447 hasConceptScore W2085798447C12294951 @default.
• W2085798447 hasConceptScore W2085798447C127313418 @default.
• W2085798447 hasConceptScore W2085798447C127413603 @default.
• W2085798447 hasConceptScore W2085798447C139719470 @default.
• W2085798447 hasConceptScore W2085798447C147176958 @default.
• W2085798447 hasConceptScore W2085798447C151730666 @default.
• W2085798447 hasConceptScore W2085798447C162324750 @default.
• W2085798447 hasConceptScore W2085798447C166839181 @default.
• W2085798447 hasConceptScore W2085798447C2781297371 @default.
• W2085798447 hasConceptScore W2085798447C32239851 @default.
• W2085798447 hasConceptScore W2085798447C50682988 @default.
• W2085798447 hasConceptScore W2085798447C77928131 @default.
• W2085798447 hasConceptScore W2085798447C92596616 @default.
• W2085798447 hasLocation W20857984471 @default.
• W2085798447 hasOpenAccess W2085798447 @default.
• W2085798447 hasPrimaryLocation W20857984471 @default.
• W2085798447 hasRelatedWork W1547228752 @default.
• W2085798447 hasRelatedWork W1969919599 @default.
• W2085798447 hasRelatedWork W2011607514 @default.

• next