FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4360841878> ?p ?o ?g. }

• W4360841878 endingPage "229812" @default.
• W4360841878 startingPage "229812" @default.
• W4360841878 abstract "The Punta del Este Basin is located at the offshore of Uruguay, and it is considered an underexplored basin with a high potential for holding hydrocarbon plays. Geologically, it constitutes an aborted rift related to the Gondwana fragmentation process, and subsequent opening of the Atlantic Ocean (Upper Jurassic - Lower Cretaceous). The stratigraphic and tectonic evolution comprises four phases from the Paleozoic pre-rift stage to present-day post-rift stage (Neogene/Quaternary). Due to the estimated hydrocarbon potential of this basin, exploratory activities have been intensified in the last decades, based on the acquisition of a significant amount of geophysical data which allowed a better comprehension of the basin's geology. Previous studies related to this basin were mainly oriented to the stratigraphy, structural framework, and petroleum systems comprehension. This research is focused on the thermal evolution of the Punta del Este Basin and its correlation with the crustal geological structure. For this purpose, a heat flow model was developed in order to understand thermal evolution through geological time. A 2D heat flow modelling based on pseudo wells was carried out to research and reconstruct the paleo heat flow. Bottom-hole temperatures (BHTs), seabed heat flow measurements, and Moho discontinuity depth interpretations have been employed in the reconstruction of heat flow evolution through time. A structural analysis based on seismic interpretation allowed to identify the Moho discontinuity and define four crustal domains in the study area: proximal (unattenuated crust), necking, hyperextended (stretched and thinned transition crust), and oceanic crust. The thermal model shows a strong correlation between heat flow and crustal thickness. In this way, the proximal domain develops low heat flow values while the distal sector shows higher values, due to the strong influence of the rifting event in crust thinning." @default.
• W4360841878 created "2023-03-25" @default.
• W4360841878 creator A5029102049 @default.
• W4360841878 creator A5037565490 @default.
• W4360841878 creator A5039375029 @default.
• W4360841878 creator A5061651094 @default.
• W4360841878 date "2023-05-01" @default.
• W4360841878 modified "2023-10-02" @default.
• W4360841878 title "Heat flow modelling of the Punta del Este Basin (offshore Uruguay) and its correlation with structural crustal domains" @default.
• W4360841878 cites W1506946271 @default.
• W4360841878 cites W1984434911 @default.
• W4360841878 cites W1992192773 @default.
• W4360841878 cites W2005379967 @default.
• W4360841878 cites W2034753142 @default.
• W4360841878 cites W2069299766 @default.
• W4360841878 cites W2152068950 @default.
• W4360841878 cites W2603221747 @default.
• W4360841878 cites W2776966260 @default.
• W4360841878 doi "https://doi.org/10.1016/j.tecto.2023.229812" @default.
• W4360841878 hasPublicationYear "2023" @default.
• W4360841878 type Work @default.
• W4360841878 citedByCount "0" @default.
• W4360841878 crossrefType "journal-article" @default.
• W4360841878 hasAuthorship W4360841878A5029102049 @default.
• W4360841878 hasAuthorship W4360841878A5037565490 @default.
• W4360841878 hasAuthorship W4360841878A5039375029 @default.
• W4360841878 hasAuthorship W4360841878A5061651094 @default.
• W4360841878 hasConcept C109007969 @default.
• W4360841878 hasConcept C114793014 @default.
• W4360841878 hasConcept C12294951 @default.
• W4360841878 hasConcept C127313418 @default.
• W4360841878 hasConcept C151730666 @default.
• W4360841878 hasConcept C165205528 @default.
• W4360841878 hasConcept C16942324 @default.
• W4360841878 hasConcept C2776698055 @default.
• W4360841878 hasConcept C50682988 @default.
• W4360841878 hasConcept C5900021 @default.
• W4360841878 hasConcept C77928131 @default.
• W4360841878 hasConceptScore W4360841878C109007969 @default.
• W4360841878 hasConceptScore W4360841878C114793014 @default.
• W4360841878 hasConceptScore W4360841878C12294951 @default.
• W4360841878 hasConceptScore W4360841878C127313418 @default.
• W4360841878 hasConceptScore W4360841878C151730666 @default.
• W4360841878 hasConceptScore W4360841878C165205528 @default.
• W4360841878 hasConceptScore W4360841878C16942324 @default.
• W4360841878 hasConceptScore W4360841878C2776698055 @default.
• W4360841878 hasConceptScore W4360841878C50682988 @default.
• W4360841878 hasConceptScore W4360841878C5900021 @default.
• W4360841878 hasConceptScore W4360841878C77928131 @default.
• W4360841878 hasLocation W43608418781 @default.
• W4360841878 hasOpenAccess W4360841878 @default.
• W4360841878 hasPrimaryLocation W43608418781 @default.
• W4360841878 hasRelatedWork W1978330345 @default.
• W4360841878 hasRelatedWork W1999086522 @default.
• W4360841878 hasRelatedWork W2014206039 @default.
• W4360841878 hasRelatedWork W2024773182 @default.
• W4360841878 hasRelatedWork W2050063417 @default.
• W4360841878 hasRelatedWork W2084633516 @default.
• W4360841878 hasRelatedWork W2314412274 @default.
• W4360841878 hasRelatedWork W2325222095 @default.
• W4360841878 hasRelatedWork W2798266913 @default.
• W4360841878 hasRelatedWork W4293733699 @default.
• W4360841878 hasVolume "854" @default.
• W4360841878 isParatext "false" @default.
• W4360841878 isRetracted "false" @default.
• W4360841878 workType "article" @default.