FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3201664650> ?p ?o ?g. }

• W3201664650 endingPage "459" @default.
• W3201664650 startingPage "437" @default.
• W3201664650 abstract "Myanmar has a long history of petroleum production, but little information has so far been published pertaining to the detailed composition of the country's oils. The present paper reports the results of the analysis of a total of 28 Cenozoic oil samples collected from producing fields/wells or natural seepages in the onshore Salin and Chindwin Basins of the Central Myanmar Depression and from Ramree Island in the Rakhine Coastal Belt. In addition, a set of 68 mudstones and coals from four Oligocene – Paleocene formations were collected along the western margin of the Central Myanmar Depression and were analysed for petroleum generation potential. Data on five oil samples from the Assam Province of India, situated to the north of the Central Myanmar Depression, were also included in the study for comparison purposes. Previous studies have suggested that the Eocene succession in the Central Myanmar Depression includes organic‐rich source rocks. However, none of the analysed rock samples show any potential for the generation of appreciable amounts of liquid petroleum components. The samples were collected at the basin margin and only cover a small fraction of the succession, and they are probably not therefore representative of the actual source rocks present in deeply buried kitchen areas in the Central Myanmar Depression. The oils from the Central Myanmar Depression appear to have been generated from the same overall source type, which is dominated by terrigenous, higher land‐plant –derived kerogen. Several different parameters consistently show clear north–south trends in the Salin Basin with respect to both thermal maturity and source facies. Oils from the Chindwin Basin in the north of the depression can be distinguished from those of the Salin Basin further south using subtle variations in biomarkers. The oils collected from Ramree Island represent a different basin and are easily distinguished in that they are generated from a predominantly marine source rock, albeit one with a significant terrigenous input. However, one sample from Ramree Island was generated from a predominantly terrigenous source, which may suggest the existence of two viable petroleum systems in the Rakhine Coastal Belt or of marked facies variations within the source succession. Oils from the Central Myanmar Depression and the Assam Province of India are remarkably similar, thus suggesting generation from highly similar source rock types, presumably of Eocene age. This could be a result of these two areas being physically connected during the Eocene as suggested by modern plate reconstructions." @default.
• W3201664650 created "2021-10-11" @default.
• W3201664650 creator A5016360576 @default.
• W3201664650 creator A5037757810 @default.
• W3201664650 creator A5057151388 @default.
• W3201664650 creator A5057477709 @default.
• W3201664650 creator A5062166148 @default.
• W3201664650 creator A5078609014 @default.
• W3201664650 date "2021-09-29" @default.
• W3201664650 modified "2023-10-17" @default.
• W3201664650 title "PETROLEUM GEOCHEMISTRY OF OILS FROM MYANMAR – A PRELIMINARY ASSESSMENT" @default.
• W3201664650 cites W1983522549 @default.
• W3201664650 cites W1985919442 @default.
• W3201664650 cites W1987562178 @default.
• W3201664650 cites W1994316586 @default.
• W3201664650 cites W1996272249 @default.
• W3201664650 cites W1996991081 @default.
• W3201664650 cites W2001641957 @default.
• W3201664650 cites W2003256570 @default.
• W3201664650 cites W2006262040 @default.
• W3201664650 cites W2008147184 @default.
• W3201664650 cites W2013232003 @default.
• W3201664650 cites W2017633530 @default.
• W3201664650 cites W2023432832 @default.
• W3201664650 cites W2025963416 @default.
• W3201664650 cites W2045878430 @default.
• W3201664650 cites W2052282628 @default.
• W3201664650 cites W2055434212 @default.
• W3201664650 cites W2069893306 @default.
• W3201664650 cites W2073556681 @default.
• W3201664650 cites W2083066801 @default.
• W3201664650 cites W2090462415 @default.
• W3201664650 cites W2094890929 @default.
• W3201664650 cites W2094963690 @default.
• W3201664650 cites W2303582121 @default.
• W3201664650 cites W2513352095 @default.
• W3201664650 cites W2519057242 @default.
• W3201664650 cites W2917802387 @default.
• W3201664650 cites W2937294608 @default.
• W3201664650 cites W2941893226 @default.
• W3201664650 cites W2972650086 @default.
• W3201664650 cites W2986397561 @default.
• W3201664650 cites W2988897983 @default.
• W3201664650 cites W3092639891 @default.
• W3201664650 doi "https://doi.org/10.1111/jpg.12799" @default.
• W3201664650 hasPublicationYear "2021" @default.
• W3201664650 type Work @default.
• W3201664650 sameAs 3201664650 @default.
• W3201664650 citedByCount "0" @default.
• W3201664650 crossrefType "journal-article" @default.
• W3201664650 hasAuthorship W3201664650A5016360576 @default.
• W3201664650 hasAuthorship W3201664650A5037757810 @default.
• W3201664650 hasAuthorship W3201664650A5057151388 @default.
• W3201664650 hasAuthorship W3201664650A5057477709 @default.
• W3201664650 hasAuthorship W3201664650A5062166148 @default.
• W3201664650 hasAuthorship W3201664650A5078609014 @default.
• W3201664650 hasConcept C109007969 @default.
• W3201664650 hasConcept C126559015 @default.
• W3201664650 hasConcept C127313418 @default.
• W3201664650 hasConcept C150117547 @default.
• W3201664650 hasConcept C151730666 @default.
• W3201664650 hasConcept C16674752 @default.
• W3201664650 hasConcept C17409809 @default.
• W3201664650 hasConcept C18903297 @default.
• W3201664650 hasConcept C199285206 @default.
• W3201664650 hasConcept C2779196632 @default.
• W3201664650 hasConcept C548895740 @default.
• W3201664650 hasConcept C86803240 @default.
• W3201664650 hasConceptScore W3201664650C109007969 @default.
• W3201664650 hasConceptScore W3201664650C126559015 @default.
• W3201664650 hasConceptScore W3201664650C127313418 @default.
• W3201664650 hasConceptScore W3201664650C150117547 @default.
• W3201664650 hasConceptScore W3201664650C151730666 @default.
• W3201664650 hasConceptScore W3201664650C16674752 @default.
• W3201664650 hasConceptScore W3201664650C17409809 @default.
• W3201664650 hasConceptScore W3201664650C18903297 @default.
• W3201664650 hasConceptScore W3201664650C199285206 @default.
• W3201664650 hasConceptScore W3201664650C2779196632 @default.
• W3201664650 hasConceptScore W3201664650C548895740 @default.
• W3201664650 hasConceptScore W3201664650C86803240 @default.
• W3201664650 hasIssue "4" @default.
• W3201664650 hasLocation W32016646501 @default.
• W3201664650 hasOpenAccess W3201664650 @default.
• W3201664650 hasPrimaryLocation W32016646501 @default.
• W3201664650 hasRelatedWork W1664607627 @default.
• W3201664650 hasRelatedWork W1839869967 @default.
• W3201664650 hasRelatedWork W1999578849 @default.
• W3201664650 hasRelatedWork W2013040945 @default.
• W3201664650 hasRelatedWork W2022856206 @default.
• W3201664650 hasRelatedWork W2263691624 @default.
• W3201664650 hasRelatedWork W2599012014 @default.
• W3201664650 hasRelatedWork W3040065123 @default.
• W3201664650 hasRelatedWork W4205935626 @default.
• W3201664650 hasRelatedWork W4255820049 @default.
• W3201664650 hasVolume "44" @default.
• W3201664650 isParatext "false" @default.
• W3201664650 isRetracted "false" @default.
• W3201664650 magId "3201664650" @default.

• next