Classification and thermal history of petroleum based on light hydrocarbons

Thompson, K. F. M.

doi:10.1016/0016-7037(83)90143-6

Cited by 356 publications

(149 citation statements)

References 16 publications

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“…11), as the case of residual oil saturations found in several dry wells in the Barents Sea. The residual oil (or parent oil) left behind in the deeper traps will be more depleted in the lighter molecular compounds than it was before Thompson, 1983). Issues of migration/fractionation/remigration are the subject of Paper 5.…”

Section: Migrational or Evaporative Fractionation Remigration Uplifmentioning

confidence: 99%

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Thermal maturity, hydrocarbon potential and kerogen type of some Triassic–Lower Cretaceous sediments from the SW Barents Sea and Svalbard

Abay

Karlsen

Pedersen

et al. 2017

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Rock-Eval and total organic carbon (TOC) analyses of 144 samples representing Triassic–Lower Cretaceous intervals from the SW Barents Sea (the Svalis Dome, the Nordkapp and Hammerfest basins, and the Bjarmeland Platform) and Svalbard demonstrate lateral variations in source rock properties. Good to excellent source rocks are present in the Lower–Middle Triassic Botneheia and Steinkobbe, and Upper Jurassic Hekkingen formations, 1 – 7 wt% and 6 – 19 wt% TOC, respectively. Hydrogen indices of 298 – 609 mg HC/g TOC in the Botneheia Formation from Svalbard, and 197 – 540 mg HC/g TOC in the Steinkobbe Formation of Svalis Dome suggest Type II (oil-prone) and Type II/III (oil/gas-prone) kerogens, respectively. The Kobbe Formation (Botneheia/Steinkobbe-equivalent) is organic-lean and generally gas-prone (Type III kerogen) on the Bjarmeland Platform and in the Nordkapp Basin, and is a good source rock with Type III/II kerogen in the Hammerfest Basin. In the investigated wells, the Hekkingen Formation is more oil-prone on the Bjarmeland Platform than in the Nordkapp Basin, while Lower Cretaceous samples have poor potential for oil. Upper Triassic samples show potential mainly for gas; however, coal/coaly-shale samples in well 7430/07-U-01 (Bjarmeland Platform) are oil/gas-prone. Most samples analysed are immature to early mature; thus, the variation in petroleum potential and kerogen type is a function of organic facies rather than maturity levels.

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Section: Migrational or Evaporative Fractionation Remigration Uplifmentioning

confidence: 99%

“…(Mango, 1987(Mango, , 1990a(Mango, , b, 1994Schaefer and Leythaeuser, 1980;Schaefer and Littke, 1988;Seifert and Moldowan, 1978;Ten Haven, 1996;Thompson, 1987;Thompson, 1983).…”

Section: Paper 5 45mentioning

confidence: 99%

Thermal maturity, hydrocarbon potential and kerogen type of some Triassic–Lower Cretaceous sediments from the SW Barents Sea and Svalbard

Abay

Karlsen

Pedersen

et al. 2017

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“…To help determine the origin of heavy oil at Kuh-e-Mond, a viscosity gradient model should be incorporated in composition simulations using Toil and Boil approach to define the extent of the biodegradation. For more accurate results, using a series of biomarker parameters of fluid inclusion oils is also required to assess fractionation and maturation of the petroleum fluids in the region (Thompson 1979(Thompson , 1983(Thompson , 1987(Thompson , 1988. The main focus of this research work was on delineation and understanding of thermodynamic conditions, physical properties, and composition of the heavy oil in the Kuh-eMond heavy oil field in Iran.…”

Section: Discussionmentioning

confidence: 99%

PVTX characteristics of oil inclusions from Asmari formation in Kuh-e-Mond heavy oil field in Iran

Shariatinia

Haghighi

Shafiei

et al. 2014

Int J Earth Sci (Geol Rundsch)

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“…Na podstawie wartości wskaźników I i H przyjęto natomiast klasyfikację rop przytoczoną w tablicy 2 [8,10].…”

Section: Podstawy Teoretyczne Analizy Rop Naftowychunclassified

Oznaczanie jakościowe i ilościowe (GC-FID) wybranych składników ropy naftowej

Bieleń

Janiga

2016

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Oznaczanie jakościowe i ilościowe (GC-FID) wybranych składników ropy naftowejZmodyfikowano metodę GC-FID oznaczania ilościowego składników ropy naftowej. Dotychczasowa metodyka wymagała modyfikacji, w tym przede wszystkim dobrania innego rozpuszczalnika do próbek ropy naftowej. Do tej pory wykorzystywano disiarczek węgla (CS 2 ), który jest związkiem silnie kancerogennym, a więc jednym z powodów zmiany rozpuszczalnika były aspekty zdrowotne. Rozszerzono stosowaną metodę o analizę ilościową wybranych komponentów występujących w ropie naftowej. Opracowano analizę ilościową wybranych n-alkanów i izoalkanów oraz niskowrzących związków aromatycznych (BTX). Dobrano program temperaturowy w celu analizy standardów, które posłużyły do utworzenia krzywych kalibracyjnych. Na podstawie tychże krzywych oznaczono wybrane związki chemiczne w sposób ilościowy w około 10 ropach naftowych.Słowa kluczowe: ropa naftowa, n-alkany, izoalkany, BTX. Qualitative and quantitative determination (GC-FID) of selected components of crude oilGC-FID method for the quantification of crude oil components was modified. Previous methodology required modification and a new solvent selection for oil samples. Carbon disulfide (CS 2 ) had been used so far and because of it's highly carcinogenic properties, the author proposed solvent replacement. The method was extended to be used for the quantitative analysis of selected components present in crude oil. Quantitative analysis of the selected n-alkane, iso-alkanes and low-boiling aromatics (BTX) was developed. A temperature program was adjusted for the analysis of standards which were used for the creation of calibration curves. Quantitative analysis of selected compounds was determined based on the curves in about 10 crude oil samples.

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Classification and thermal history of petroleum based on light hydrocarbons

Cited by 356 publications

References 16 publications

Thermal maturity, hydrocarbon potential and kerogen type of some Triassic–Lower Cretaceous sediments from the SW Barents Sea and Svalbard

Thermal maturity, hydrocarbon potential and kerogen type of some Triassic–Lower Cretaceous sediments from the SW Barents Sea and Svalbard

PVTX characteristics of oil inclusions from Asmari formation in Kuh-e-Mond heavy oil field in Iran

Oznaczanie jakościowe i ilościowe (GC-FID) wybranych składników ropy naftowej

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