FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3210777195> ?p ?o ?g. }

• W3210777195 abstract "Abstract D31 cluster is located in the prolific Mumbai Offshore Basin, Western part of India. B-192Afield is part of this cluster, where Bassein (Middle Eocene),Mukta and Panvel (Early Oligocene)Formations are the main reservoirs. The reservoirs are complex in terms of reservoir heterogeneity. They were deposited in a shallow marine carbonate platform.Sea level fluctuations andchange in depositional environment impacted the porosity development. The main objective of this study was to integrate spectral gamma ray signatures with seismic interpretation for demarcating significant stratigraphic surfaces and differentiating depositional environments for robust reservoir characterization. Regionally, Bassein Formation (Middle Eocene) is characterized by thick foraminiferal and algal wackestone, packstone and occasional grainstone facies.The Mukta Formation (Early Oligocene),which unconformably overlies the Bassein Formation, is characterized by presence of fossiliferous limestone with shale intercalations. In the present study, data from four exploration wells data have been analyzed, where spectral gamma ray log patterns in carbonate reservoirs appear to have a distinctive relationship to depositional facies and stratigraphic surfaces in the Bassein and Mukta Formations. Different cross plots have also been utilized for analyzing the depositional conditions (i.e. oxic or anoxic).Later, the spectral log interpretations have been integrated with seismic interpretation. This study is part of a larger effort for reservoir characterization, as a basis for seismic interpretation and integrated reservoir modelling. The spectral gamma ray signatures demarcated significant stratigraphic surfaces. In BasseinFormation, three different units have been marked as Upper, Middle and Lower Bassein. The major lithological boundary between the Bassein and Mukta Formation is also well demarcated with spectral GR signature. The carbonate strata of Bassein & Mukta Formation have also been subdivided with U-Th-K abundance.The Low Th-Low U units indicative of pure carbonate and deposition in oxidizing environment whereas Low Th-High Uis indicative ofreducing environment, which gave a relative sea level fluctuation in the area.The major stratigraphic boundaries identified from these spectral GR logs has been incorporated in the seismicinterpretation and used for regional seismic mapping.As porosity development is governed by thesea level fluctuations,this study also gave an indication of the possibility of porous zonein the reservoir section. These results can be useful as a basis for applying spectral GR signature as a tool for stratigraphic interpretation in un-cored heterogenous carbonate sections. Along with the petrophysical interpretation, integration of core analysis, biostratigraphy and seismic attribute are critical for detailed carbonate reservoir characterization incorporating depositional environment.This approach can be applied to support commercial development of the complex carbonate reservoirs." @default.
• W3210777195 created "2021-11-08" @default.
• W3210777195 creator A5021621089 @default.
• W3210777195 creator A5025931603 @default.
• W3210777195 creator A5044513123 @default.
• W3210777195 creator A5052660882 @default.
• W3210777195 creator A5054522345 @default.
• W3210777195 creator A5076809405 @default.
• W3210777195 date "2021-10-04" @default.
• W3210777195 modified "2023-10-16" @default.
• W3210777195 title "Utilization of Spectral Gamma Ray Logs to Ascertain Stratigraphic Surfaces in Carbonate Reservoir and Integration with Seismic Interpretation: An Integrated Case Study from Eocene-Oligocene Carbonate Reservoirs, D31 Cluster, Mumbai Offshore Basin, India" @default.
• W3210777195 cites W2039890251 @default.
• W3210777195 cites W2108911062 @default.
• W3210777195 cites W2116221979 @default.
• W3210777195 cites W2395183450 @default.
• W3210777195 doi "https://doi.org/10.2118/205709-ms" @default.
• W3210777195 hasPublicationYear "2021" @default.
• W3210777195 type Work @default.
• W3210777195 sameAs 3210777195 @default.
• W3210777195 citedByCount "0" @default.
• W3210777195 crossrefType "proceedings-article" @default.
• W3210777195 hasAuthorship W3210777195A5021621089 @default.
• W3210777195 hasAuthorship W3210777195A5025931603 @default.
• W3210777195 hasAuthorship W3210777195A5044513123 @default.
• W3210777195 hasAuthorship W3210777195A5052660882 @default.
• W3210777195 hasAuthorship W3210777195A5054522345 @default.
• W3210777195 hasAuthorship W3210777195A5076809405 @default.
• W3210777195 hasConcept C109007969 @default.
• W3210777195 hasConcept C126753816 @default.
• W3210777195 hasConcept C127313418 @default.
• W3210777195 hasConcept C14641988 @default.
• W3210777195 hasConcept C146588470 @default.
• W3210777195 hasConcept C151730666 @default.
• W3210777195 hasConcept C162284963 @default.
• W3210777195 hasConcept C187320778 @default.
• W3210777195 hasConcept C191735495 @default.
• W3210777195 hasConcept C191897082 @default.
• W3210777195 hasConcept C192562407 @default.
• W3210777195 hasConcept C19320362 @default.
• W3210777195 hasConcept C2778609275 @default.
• W3210777195 hasConcept C2780659211 @default.
• W3210777195 hasConcept C5900021 @default.
• W3210777195 hasConcept C6494504 @default.
• W3210777195 hasConceptScore W3210777195C109007969 @default.
• W3210777195 hasConceptScore W3210777195C126753816 @default.
• W3210777195 hasConceptScore W3210777195C127313418 @default.
• W3210777195 hasConceptScore W3210777195C14641988 @default.
• W3210777195 hasConceptScore W3210777195C146588470 @default.
• W3210777195 hasConceptScore W3210777195C151730666 @default.
• W3210777195 hasConceptScore W3210777195C162284963 @default.
• W3210777195 hasConceptScore W3210777195C187320778 @default.
• W3210777195 hasConceptScore W3210777195C191735495 @default.
• W3210777195 hasConceptScore W3210777195C191897082 @default.
• W3210777195 hasConceptScore W3210777195C192562407 @default.
• W3210777195 hasConceptScore W3210777195C19320362 @default.
• W3210777195 hasConceptScore W3210777195C2778609275 @default.
• W3210777195 hasConceptScore W3210777195C2780659211 @default.
• W3210777195 hasConceptScore W3210777195C5900021 @default.
• W3210777195 hasConceptScore W3210777195C6494504 @default.
• W3210777195 hasLocation W32107771951 @default.
• W3210777195 hasOpenAccess W3210777195 @default.
• W3210777195 hasPrimaryLocation W32107771951 @default.
• W3210777195 hasRelatedWork W1779917143 @default.
• W3210777195 hasRelatedWork W1978202421 @default.
• W3210777195 hasRelatedWork W2015969524 @default.
• W3210777195 hasRelatedWork W2378691413 @default.
• W3210777195 hasRelatedWork W2800033930 @default.
• W3210777195 hasRelatedWork W2900865825 @default.
• W3210777195 hasRelatedWork W3035653353 @default.
• W3210777195 hasRelatedWork W3148990409 @default.
• W3210777195 hasRelatedWork W4220673238 @default.
• W3210777195 hasRelatedWork W4307663924 @default.
• W3210777195 isParatext "false" @default.
• W3210777195 isRetracted "false" @default.
• W3210777195 magId "3210777195" @default.
• W3210777195 workType "article" @default.