FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2899022182> ?p ?o ?g. }

• W2899022182 endingPage "50" @default.
• W2899022182 startingPage "50" @default.
• W2899022182 abstract "More than 60 trillion cubic feet (Tcf) of natural gas have been recently discovered in the Levant Basin (eastern Mediterranean region) offshore Cyprus, Egypt and Israel, Palestine. Un-explored areas, such as the Lebanese offshore, may yield additional discoveries. This contribution focuses the Saida-Tyr Platform (STP), an offshore geological feature adjacent to the southern Lebanese coastline – part of the eastern margin of the Levant Basin. First, an extensive synthesis of recent published research work, tackling crustal modeling, structural geology and stratigraphy will be presented. Then, a new local crustal model and the interpretation of seismic reflection specifically on the STP are discussed and emplaced in the context of the upcoming petroleum exploration activities in this region. Characteristic structural features form the limits of the STP which is believed to be an extension of the Arabian continent into the Levant Basin. Its westernmost limit consists of the extension of the crustal interface, previously termed “hinge zone”, where major plate-scale deformations are preferentially localized. The northward extension of this “hinge zone” beyond the STP can be mapped by means of major similar deformation structures ( i.e. S-N-trending anticlines) and can be associated to the Levant Fracture System (LFS) – the northwestern border of the Arabian plate. The northern limit of the STP ( i.e. the Saida Fault) is a typical E-W, presently active, structure that is inherited from an older, deeply rooted regional fault system, extending eastward throughout the Palmyra Basin. The STP is characterized by a variety of potential plays for hydrocarbon exploration. Jurassic and Cretaceous clastics and carbonates are believed to include reservoir plays, which could have been charged by deeper Mesozoic source rocks, and sealed by Upper Cretaceous marly layers. The edge of the Cretaceous carbonate platforms and potential carbonate buildups are well recognizable on seismic reflection profiles. The western and northern anticlinal structures bordering the STP are excellent targets for Oligo-Miocene biogenic gas charging systems. Based on integrating geodynamics, tectono-stratigraphic interpretations and petroleum systems analyses, such plays are well constrained and the exploration risk is therefore lowered." @default.
• W2899022182 created "2018-11-09" @default.
• W2899022182 creator A5018327330 @default.
• W2899022182 creator A5060567860 @default.
• W2899022182 creator A5068074132 @default.
• W2899022182 creator A5084571003 @default.
• W2899022182 creator A5088123387 @default.
• W2899022182 date "2018-01-01" @default.
• W2899022182 modified "2023-10-18" @default.
• W2899022182 title "Key geological characteristics of the Saida-Tyr Platform along the eastern margin of the Levant Basin, offshore Lebanon: implications for hydrocarbon exploration" @default.
• W2899022182 cites W1492942587 @default.
• W2899022182 cites W1503493870 @default.
• W2899022182 cites W1584354900 @default.
• W2899022182 cites W1585871258 @default.
• W2899022182 cites W1971027692 @default.
• W2899022182 cites W1975207430 @default.
• W2899022182 cites W1976497240 @default.
• W2899022182 cites W1979249320 @default.
• W2899022182 cites W1983523823 @default.
• W2899022182 cites W1986730322 @default.
• W2899022182 cites W1988098630 @default.
• W2899022182 cites W1993524516 @default.
• W2899022182 cites W1998730078 @default.
• W2899022182 cites W2002913742 @default.
• W2899022182 cites W2007478149 @default.
• W2899022182 cites W2016219895 @default.
• W2899022182 cites W2019967542 @default.
• W2899022182 cites W2027315840 @default.
• W2899022182 cites W2027881359 @default.
• W2899022182 cites W2029566765 @default.
• W2899022182 cites W2031815022 @default.
• W2899022182 cites W2037312261 @default.
• W2899022182 cites W2040601759 @default.
• W2899022182 cites W2040912248 @default.
• W2899022182 cites W2049684881 @default.
• W2899022182 cites W2055364230 @default.
• W2899022182 cites W2056687199 @default.
• W2899022182 cites W2056955907 @default.
• W2899022182 cites W2061387615 @default.
• W2899022182 cites W2061448960 @default.
• W2899022182 cites W2064317759 @default.
• W2899022182 cites W2064782689 @default.
• W2899022182 cites W2064936022 @default.
• W2899022182 cites W2064977139 @default.
• W2899022182 cites W2067117119 @default.
• W2899022182 cites W2076032489 @default.
• W2899022182 cites W2099894253 @default.
• W2899022182 cites W2112368683 @default.
• W2899022182 cites W2113688945 @default.
• W2899022182 cites W2118311364 @default.
• W2899022182 cites W2118343338 @default.
• W2899022182 cites W2139364698 @default.
• W2899022182 cites W2141728530 @default.
• W2899022182 cites W2146171617 @default.
• W2899022182 cites W2154139172 @default.
• W2899022182 cites W2154174575 @default.
• W2899022182 cites W2156235478 @default.
• W2899022182 cites W2156301488 @default.
• W2899022182 cites W2158566372 @default.
• W2899022182 cites W2162424679 @default.
• W2899022182 cites W2163411283 @default.
• W2899022182 cites W2165036844 @default.
• W2899022182 cites W2313801305 @default.
• W2899022182 cites W2330091543 @default.
• W2899022182 cites W2510114941 @default.
• W2899022182 cites W2540235806 @default.
• W2899022182 cites W2553615290 @default.
• W2899022182 cites W2789770144 @default.
• W2899022182 cites W2793394278 @default.
• W2899022182 cites W2794357842 @default.
• W2899022182 cites W2804272659 @default.
• W2899022182 cites W2883565450 @default.
• W2899022182 cites W2898946975 @default.
• W2899022182 cites W2904401725 @default.
• W2899022182 cites W40847255 @default.
• W2899022182 cites W4205268883 @default.
• W2899022182 cites W4206873747 @default.
• W2899022182 doi "https://doi.org/10.2516/ogst/2018045" @default.
• W2899022182 hasPublicationYear "2018" @default.
• W2899022182 type Work @default.
• W2899022182 sameAs 2899022182 @default.
• W2899022182 citedByCount "13" @default.
• W2899022182 countsByYear W28990221822018 @default.
• W2899022182 countsByYear W28990221822019 @default.
• W2899022182 countsByYear W28990221822020 @default.
• W2899022182 countsByYear W28990221822021 @default.
• W2899022182 countsByYear W28990221822022 @default.
• W2899022182 countsByYear W28990221822023 @default.
• W2899022182 crossrefType "journal-article" @default.
• W2899022182 hasAuthorship W2899022182A5018327330 @default.
• W2899022182 hasAuthorship W2899022182A5060567860 @default.
• W2899022182 hasAuthorship W2899022182A5068074132 @default.
• W2899022182 hasAuthorship W2899022182A5084571003 @default.
• W2899022182 hasAuthorship W2899022182A5088123387 @default.
• W2899022182 hasBestOaLocation W28990221821 @default.
• W2899022182 hasConcept C109007969 @default.
• W2899022182 hasConcept C109281948 @default.
• W2899022182 hasConcept C111368507 @default.

• next