FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1970440610> ?p ?o ?g. }

• W1970440610 endingPage "506" @default.
• W1970440610 startingPage "489" @default.
• W1970440610 abstract "The Jeffara escarpment spans 400 km from southeastern Tunisia to sorthwestern Libya, and marks the northern edge of the Berkine–Ghadames Basin. Its horseshoe shape provides a good 3D control of regional-scale depositional architecture. Historically, the political border between Tunisia and Libya hindered the integration of studies over its entirety, which led to the establishment of separate litho-biostratigraphic frameworks. Field-work undertaken on both sides of the border has allowed the unification of lithostratigraphic schemes developed in both countries. Published stratigraphic ages of the different formations and members are compared and integrated in order to propose a unified bio-lithostratigraphic framework. The correlation of serial sections along the Jeffara escarpment shows that two major tectonic unconformities divide the Early Cretaceous sedimentary pattern. The first one is dated as Late Aptian and is commonly associated with the European “Austrian” tectonic phase. The second, which has previously not been recognized as a regional significant surface in Libya, occurs during the Middle Albian and marks moreover the transition from a siliciclastic to a carbonate-dominated sedimentation regime. These two important regional unconformities form the lower and upper boundaries of the Kiklah–Aïn el Guettar Formations, and can be associated with intra-plate deformation linked with the opening of the central segment of the South Atlantic and the Equatorial Atlantic oceans." @default.
• W1970440610 created "2016-06-24" @default.
• W1970440610 creator A5006675696 @default.
• W1970440610 creator A5023741514 @default.
• W1970440610 creator A5051278160 @default.
• W1970440610 creator A5057862464 @default.
• W1970440610 creator A5058573025 @default.
• W1970440610 date "2010-10-01" @default.
• W1970440610 modified "2023-10-10" @default.
• W1970440610 title "Timing of early to mid-cretaceous tectonic phases along North Africa: New insights from the Jeffara escarpment (Libya–Tunisia)" @default.
• W1970440610 cites W1978470997 @default.
• W1970440610 cites W1980642926 @default.
• W1970440610 cites W1982594203 @default.
• W1970440610 cites W1983060065 @default.
• W1970440610 cites W1983134347 @default.
• W1970440610 cites W1983382058 @default.
• W1970440610 cites W1985985468 @default.
• W1970440610 cites W1987291994 @default.
• W1970440610 cites W1992043392 @default.
• W1970440610 cites W2003403415 @default.
• W1970440610 cites W2006032174 @default.
• W1970440610 cites W2008031852 @default.
• W1970440610 cites W2009997800 @default.
• W1970440610 cites W2026324572 @default.
• W1970440610 cites W2035560495 @default.
• W1970440610 cites W2036964633 @default.
• W1970440610 cites W2037455329 @default.
• W1970440610 cites W2046853743 @default.
• W1970440610 cites W2047387556 @default.
• W1970440610 cites W2051375008 @default.
• W1970440610 cites W2055439406 @default.
• W1970440610 cites W2059745127 @default.
• W1970440610 cites W2062113061 @default.
• W1970440610 cites W2068580384 @default.
• W1970440610 cites W2068991796 @default.
• W1970440610 cites W2069232301 @default.
• W1970440610 cites W2082924252 @default.
• W1970440610 cites W2085075988 @default.
• W1970440610 cites W2093980733 @default.
• W1970440610 cites W2108998966 @default.
• W1970440610 cites W2109934455 @default.
• W1970440610 cites W2128116599 @default.
• W1970440610 cites W2128671902 @default.
• W1970440610 cites W2130837160 @default.
• W1970440610 cites W2155647553 @default.
• W1970440610 cites W2160304608 @default.
• W1970440610 cites W2524280057 @default.
• W1970440610 cites W2600930298 @default.
• W1970440610 cites W2753353811 @default.
• W1970440610 cites W2889763753 @default.
• W1970440610 doi "https://doi.org/10.1016/j.jafrearsci.2010.04.010" @default.
• W1970440610 hasPublicationYear "2010" @default.
• W1970440610 type Work @default.
• W1970440610 sameAs 1970440610 @default.
• W1970440610 citedByCount "64" @default.
• W1970440610 countsByYear W19704406102012 @default.
• W1970440610 countsByYear W19704406102013 @default.
• W1970440610 countsByYear W19704406102014 @default.
• W1970440610 countsByYear W19704406102015 @default.
• W1970440610 countsByYear W19704406102016 @default.
• W1970440610 countsByYear W19704406102017 @default.
• W1970440610 countsByYear W19704406102018 @default.
• W1970440610 countsByYear W19704406102019 @default.
• W1970440610 countsByYear W19704406102020 @default.
• W1970440610 countsByYear W19704406102021 @default.
• W1970440610 countsByYear W19704406102022 @default.
• W1970440610 countsByYear W19704406102023 @default.
• W1970440610 crossrefType "journal-article" @default.
• W1970440610 hasAuthorship W1970440610A5006675696 @default.
• W1970440610 hasAuthorship W1970440610A5023741514 @default.
• W1970440610 hasAuthorship W1970440610A5051278160 @default.
• W1970440610 hasAuthorship W1970440610A5057862464 @default.
• W1970440610 hasAuthorship W1970440610A5058573025 @default.
• W1970440610 hasBestOaLocation W19704406102 @default.
• W1970440610 hasConcept C109007969 @default.
• W1970440610 hasConcept C12294951 @default.
• W1970440610 hasConcept C126753816 @default.
• W1970440610 hasConcept C127313418 @default.
• W1970440610 hasConcept C151730666 @default.
• W1970440610 hasConcept C161820406 @default.
• W1970440610 hasConcept C179226041 @default.
• W1970440610 hasConcept C189473229 @default.
• W1970440610 hasConcept C191735495 @default.
• W1970440610 hasConcept C2778609275 @default.
• W1970440610 hasConcept C50682988 @default.
• W1970440610 hasConcept C6494504 @default.
• W1970440610 hasConcept C77928131 @default.
• W1970440610 hasConcept C93257316 @default.
• W1970440610 hasConceptScore W1970440610C109007969 @default.
• W1970440610 hasConceptScore W1970440610C12294951 @default.
• W1970440610 hasConceptScore W1970440610C126753816 @default.
• W1970440610 hasConceptScore W1970440610C127313418 @default.
• W1970440610 hasConceptScore W1970440610C151730666 @default.
• W1970440610 hasConceptScore W1970440610C161820406 @default.
• W1970440610 hasConceptScore W1970440610C179226041 @default.
• W1970440610 hasConceptScore W1970440610C189473229 @default.
• W1970440610 hasConceptScore W1970440610C191735495 @default.
• W1970440610 hasConceptScore W1970440610C2778609275 @default.

• next