FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4306353676> ?p ?o ?g. }

• W4306353676 endingPage "48" @default.
• W4306353676 startingPage "17" @default.
• W4306353676 abstract "The following problem is solved by the present research: the probable sources of Paleozoic hydrocarbon deposits are determined on the basis of modeling the hydrocarbon foci of generation Paleozoic-Mesozoic oil source formations (for example, the southeast of Western Siberia, Tomsk Region). The research area is the lands Ostanino field group: the Selveikin area of deep drilling, the Ostaninskoye and Gerasimovskoye oil and gas condensate fields. Pre-Jurassic strata with oil source potential, including the Paleozoic Larinskaya (S1lr), Mirnaya (D13mr), Chuzikskaya (D2cz), Chaginskaya (D3cg) and Kehoregskaya (C1kh) formations, as well as Jurassic Bazhenovskaya (J3bg) and Tyumenskaya (J1-2tm ) formations, and, accordingly, the reservoirs of the weathering crust and bed-rock Paleozoic reservoirs are the objects of study. The subject of analysis was selected in accordance with the concept of the geothermal regime of the subsoil, as a leading factor in the implementation of the generation potential of the parent sediments. The research methods are digital paleotemperature modeling and historical-geological analysis. The results and conclusions concerning the fundamental problems of “Paleozoic oil” are obtained. 1. Source of the Paleozoic oil deposits can be both the Domanic type rocks of the Paleozoic formations and the Jurassic oil source formations. Thus, both upward vertical interstratal HC migration and downward HC migration can take place. Therefore, the two concepts of “main source” are compatible and should not be considered, as often, orthodoxly alternative. 2. The domanicoid rocks of the Paleozoic formations are most likely the source for Paleozoic gas and gas condensate deposits. 3. Paleozoic formations the roof of the bed-rock Paleozoic (on the Ostankinskaya group of fields – C1kh and D3cg) can be only the source of the «Paleozoic oil» and gas deposits in the Pre-Jurassic oil and gas complex. 4. Bazhenov formation – J3bg may be the “Jurassic” source of oil deposits in the Pre-Jurassic oil and gas complex. The results were obtained and conclusions were drawn concerning the applied (search) aspects of the problem: 1. Results additionally substantiate the author’s search criterion for the oil and gas content of the Paleozoic – these are anomalous geophysical and petrophysical characteristics of the Jurassic section. 2. The absence of hydrocarbon deposits in the Jurassic section is most likely a negative sign of the Paleozoic oil and gas content. 4. The low density of the modern heat flow (less than 40 mW/m2) is most likely a negative sign of oil deposits in the Paleozoic. 3. High paleotemperatures in terms of VR (more than 175oC) are most likely a negative sign of oil and gas deposits in the Paleozoic. 4. Reasons have been obtained to state that oil deposits in the Paleozoic cannot be richer than oil deposits in the Jurassic." @default.
• W4306353676 created "2022-10-16" @default.
• W4306353676 creator A5013478097 @default.
• W4306353676 creator A5018393993 @default.
• W4306353676 creator A5019358008 @default.
• W4306353676 creator A5050147173 @default.
• W4306353676 creator A5062573034 @default.
• W4306353676 creator A5063021440 @default.
• W4306353676 date "2022-09-30" @default.
• W4306353676 modified "2023-10-16" @default.
• W4306353676 title "Paleozoic and Mesozoic hydrocarbon foci of generation and assessment of their role in formation oil deposits of the Pre-Jurassic complex of Western Siberia" @default.
• W4306353676 cites W1991587087 @default.
• W4306353676 cites W2013415471 @default.
• W4306353676 cites W2015485692 @default.
• W4306353676 cites W2032271236 @default.
• W4306353676 cites W2046577709 @default.
• W4306353676 cites W2060608385 @default.
• W4306353676 cites W2070369011 @default.
• W4306353676 cites W2075769266 @default.
• W4306353676 cites W2086682049 @default.
• W4306353676 cites W2532772026 @default.
• W4306353676 cites W2767549855 @default.
• W4306353676 cites W2774871611 @default.
• W4306353676 cites W2798127614 @default.
• W4306353676 cites W2885356981 @default.
• W4306353676 cites W2892287055 @default.
• W4306353676 cites W2936672373 @default.
• W4306353676 cites W2945892448 @default.
• W4306353676 cites W2980056957 @default.
• W4306353676 cites W3089072217 @default.
• W4306353676 cites W3097686327 @default.
• W4306353676 cites W3117172442 @default.
• W4306353676 cites W3137618568 @default.
• W4306353676 cites W3149954374 @default.
• W4306353676 cites W3216972751 @default.
• W4306353676 cites W4233345504 @default.
• W4306353676 doi "https://doi.org/10.18599/grs.2022.3.3" @default.
• W4306353676 hasPublicationYear "2022" @default.
• W4306353676 type Work @default.
• W4306353676 citedByCount "0" @default.
• W4306353676 crossrefType "journal-article" @default.
• W4306353676 hasAuthorship W4306353676A5013478097 @default.
• W4306353676 hasAuthorship W4306353676A5018393993 @default.
• W4306353676 hasAuthorship W4306353676A5019358008 @default.
• W4306353676 hasAuthorship W4306353676A5050147173 @default.
• W4306353676 hasAuthorship W4306353676A5062573034 @default.
• W4306353676 hasAuthorship W4306353676A5063021440 @default.
• W4306353676 hasBestOaLocation W43063536761 @default.
• W4306353676 hasConcept C109007969 @default.
• W4306353676 hasConcept C113740612 @default.
• W4306353676 hasConcept C126559015 @default.
• W4306353676 hasConcept C127313418 @default.
• W4306353676 hasConcept C13106087 @default.
• W4306353676 hasConcept C151730666 @default.
• W4306353676 hasConcept C17409809 @default.
• W4306353676 hasConcept C178790620 @default.
• W4306353676 hasConcept C185592680 @default.
• W4306353676 hasConcept C202783661 @default.
• W4306353676 hasConcept C5900021 @default.
• W4306353676 hasConcept C59427239 @default.
• W4306353676 hasConceptScore W4306353676C109007969 @default.
• W4306353676 hasConceptScore W4306353676C113740612 @default.
• W4306353676 hasConceptScore W4306353676C126559015 @default.
• W4306353676 hasConceptScore W4306353676C127313418 @default.
• W4306353676 hasConceptScore W4306353676C13106087 @default.
• W4306353676 hasConceptScore W4306353676C151730666 @default.
• W4306353676 hasConceptScore W4306353676C17409809 @default.
• W4306353676 hasConceptScore W4306353676C178790620 @default.
• W4306353676 hasConceptScore W4306353676C185592680 @default.
• W4306353676 hasConceptScore W4306353676C202783661 @default.
• W4306353676 hasConceptScore W4306353676C5900021 @default.
• W4306353676 hasConceptScore W4306353676C59427239 @default.
• W4306353676 hasIssue "2" @default.
• W4306353676 hasLocation W43063536761 @default.
• W4306353676 hasLocation W43063536762 @default.
• W4306353676 hasOpenAccess W4306353676 @default.
• W4306353676 hasPrimaryLocation W43063536761 @default.
• W4306353676 hasRelatedWork W1578456421 @default.
• W4306353676 hasRelatedWork W1989830028 @default.
• W4306353676 hasRelatedWork W2337712059 @default.
• W4306353676 hasRelatedWork W2367617664 @default.
• W4306353676 hasRelatedWork W2369654030 @default.
• W4306353676 hasRelatedWork W2371175707 @default.
• W4306353676 hasRelatedWork W273225047 @default.
• W4306353676 hasRelatedWork W3151082666 @default.
• W4306353676 hasRelatedWork W4291667190 @default.
• W4306353676 hasRelatedWork W4306353676 @default.
• W4306353676 hasVolume "24" @default.
• W4306353676 isParatext "false" @default.
• W4306353676 isRetracted "false" @default.
• W4306353676 workType "article" @default.