FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3190596332> ?p ?o ?g. }

• W3190596332 endingPage "112" @default.
• W3190596332 startingPage "83" @default.
• W3190596332 abstract "A fully integrated 3D basin model was built to study the lithospheric structural evolution and the thermal history of the offshore part of the Gippsland Basin to investigate the type, timing and magnitude of its initial opening mechanism and their effects on source rocks. The applied workflow included seismic interpretation of major faults and magmatic features, seismic reinterpretation of existing main stratigraphic boundaries and adjustment of the basement topography. Different scenarios for a McKenzie-type basal heat flow evolution were tested based on a two-step inversion approach, which translates the thickness changes of lithospheric layers into basal heat flow. Finally, a crustal layer model was assigned to the existing 3D numerical basin model and the effects on thermal maturation of petroleum source rocks were investigated. The results of the calibrated inversion model suggest intense lithospheric stretching and mantle upwelling during the Early Cretaceous caused initial breakup and subsidence of the Gippsland Basin. This syn-rift phase was accompanied by increasing basal heat flow from initially ∼50 mW/m2 to a maximum of 80–90 mW/m2. The resulting upwelled Moho with an associated crustal thickness of locally only 8 km agrees with geophysical observations. Elevated paleogeothermal gradients between 50 and 60 °C/km prevailed from ca 120 to 80 Ma. Episodes of compression, uplift, erosion, and thermal subsidence resulted in fast and continuous cooling during the early post-rift and a constant basal heat flow of 45–50 mW/m2 since the Eocene. Two main pulses of petroleum generation were identified in the Paleocene and in the Miocene–Pliocene. This novel two-step crustal layer inversion method allows a detailed reconstruction of the thermal history of rift basins and can provide useful information about the maturation of petroleum source rocks.KEY POINTSA temperature history reconstruction of the Gippsland Basin is given based on a large-scale numerical 3D model.Tectonically induced strong variability in paleoheat flows is recognised.Strong maturation and petroleum generation developed during the Paleogene and Neogene." @default.
• W3190596332 created "2021-08-16" @default.
• W3190596332 creator A5008304205 @default.
• W3190596332 creator A5038985275 @default.
• W3190596332 creator A5047072062 @default.
• W3190596332 creator A5050650955 @default.
• W3190596332 creator A5051727515 @default.
• W3190596332 creator A5068610074 @default.
• W3190596332 creator A5070560590 @default.
• W3190596332 creator A5072997716 @default.
• W3190596332 creator A5090750831 @default.
• W3190596332 date "2021-08-02" @default.
• W3190596332 modified "2023-10-17" @default.
• W3190596332 title "Lithospheric evolution, thermo-tectonic history and source-rock maturation in the Gippsland Basin, Victoria, southeastern Australia" @default.
• W3190596332 cites W1550053570 @default.
• W3190596332 cites W1581029888 @default.
• W3190596332 cites W1967728769 @default.
• W3190596332 cites W1989445090 @default.
• W3190596332 cites W1998881096 @default.
• W3190596332 cites W2003394352 @default.
• W3190596332 cites W2009022965 @default.
• W3190596332 cites W2010171236 @default.
• W3190596332 cites W2014984083 @default.
• W3190596332 cites W2019297366 @default.
• W3190596332 cites W2029435338 @default.
• W3190596332 cites W2032022180 @default.
• W3190596332 cites W2034753142 @default.
• W3190596332 cites W2042722234 @default.
• W3190596332 cites W2056936756 @default.
• W3190596332 cites W2058950793 @default.
• W3190596332 cites W2061999061 @default.
• W3190596332 cites W2065947578 @default.
• W3190596332 cites W2076548720 @default.
• W3190596332 cites W2084259535 @default.
• W3190596332 cites W2102234201 @default.
• W3190596332 cites W2110811989 @default.
• W3190596332 cites W2124474119 @default.
• W3190596332 cites W2142262462 @default.
• W3190596332 cites W2155830057 @default.
• W3190596332 cites W2293592303 @default.
• W3190596332 cites W2295217984 @default.
• W3190596332 cites W2335953896 @default.
• W3190596332 cites W2346533957 @default.
• W3190596332 cites W2549448324 @default.
• W3190596332 cites W2586717909 @default.
• W3190596332 cites W2745541099 @default.
• W3190596332 cites W2747166583 @default.
• W3190596332 cites W2748881983 @default.
• W3190596332 cites W2749125476 @default.
• W3190596332 cites W2750389069 @default.
• W3190596332 cites W2980067621 @default.
• W3190596332 cites W2997379171 @default.
• W3190596332 cites W3023081685 @default.
• W3190596332 cites W4249818201 @default.
• W3190596332 cites W4252408948 @default.
• W3190596332 doi "https://doi.org/10.1080/08120099.2021.1938219" @default.
• W3190596332 hasPublicationYear "2021" @default.
• W3190596332 type Work @default.
• W3190596332 sameAs 3190596332 @default.
• W3190596332 citedByCount "3" @default.
• W3190596332 countsByYear W31905963322022 @default.
• W3190596332 countsByYear W31905963322023 @default.
• W3190596332 crossrefType "journal-article" @default.
• W3190596332 hasAuthorship W3190596332A5008304205 @default.
• W3190596332 hasAuthorship W3190596332A5038985275 @default.
• W3190596332 hasAuthorship W3190596332A5047072062 @default.
• W3190596332 hasAuthorship W3190596332A5050650955 @default.
• W3190596332 hasAuthorship W3190596332A5051727515 @default.
• W3190596332 hasAuthorship W3190596332A5068610074 @default.
• W3190596332 hasAuthorship W3190596332A5070560590 @default.
• W3190596332 hasAuthorship W3190596332A5072997716 @default.
• W3190596332 hasAuthorship W3190596332A5090750831 @default.
• W3190596332 hasBestOaLocation W31905963321 @default.
• W3190596332 hasConcept C100951216 @default.
• W3190596332 hasConcept C109007969 @default.
• W3190596332 hasConcept C12294951 @default.
• W3190596332 hasConcept C126559015 @default.
• W3190596332 hasConcept C127313418 @default.
• W3190596332 hasConcept C151730666 @default.
• W3190596332 hasConcept C162973429 @default.
• W3190596332 hasConcept C16942324 @default.
• W3190596332 hasConcept C180851071 @default.
• W3190596332 hasConcept C1893757 @default.
• W3190596332 hasConcept C50682988 @default.
• W3190596332 hasConcept C5900021 @default.
• W3190596332 hasConcept C67236022 @default.
• W3190596332 hasConcept C77928131 @default.
• W3190596332 hasConcept C97995005 @default.
• W3190596332 hasConceptScore W3190596332C100951216 @default.
• W3190596332 hasConceptScore W3190596332C109007969 @default.
• W3190596332 hasConceptScore W3190596332C12294951 @default.
• W3190596332 hasConceptScore W3190596332C126559015 @default.
• W3190596332 hasConceptScore W3190596332C127313418 @default.
• W3190596332 hasConceptScore W3190596332C151730666 @default.
• W3190596332 hasConceptScore W3190596332C162973429 @default.
• W3190596332 hasConceptScore W3190596332C16942324 @default.
• W3190596332 hasConceptScore W3190596332C180851071 @default.
• W3190596332 hasConceptScore W3190596332C1893757 @default.

• next