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TitreOrganic geochemistry of Silurian graptolitic shale and its petroleum source rock potential, Canadian Arctic Archipelago
AuteurObermajer, M; Dewing, K; Fowler, M G
Source27th International Meeting on Organic Geochemistry, IMOG 2015 Prague, book of abstracts; par IMOG Organizing Committee; 2015, 275-276 pages
Année2015
Séries alt.Secteur des sciences de la Terre, Contribution externe 20140514
ÉditeurEuropean Association of Organic Geochemists
RéunionInternational Meeting on Organic Geochemistry; Prague; CZ; Septembre 13-18, 2015
Documentlivre
Lang.anglais
Mediapapier; en ligne; numérique
Formatspdf
ProvinceTerritoires du Nord-Ouest; Nunavut
Sujetsgéochimie organique; roches mères; schistes; hydrocarbures; maturation thermique; indice d'hydrogène; Graptolites; Formation de Cape Phillips ; Bassin de Sverdrup ; combustibles fossiles; Silurien
ProgrammeBassin de Sverdrup de l'ouest de l'Arctique, GEM2 : La géocartographie de l'énergie et des minéraux
LiensOnline - En ligne (PDF, 100 MB)
Résumé(disponible en anglais seulement)
The widespread series of open marine graptolite-rich rocks that formed during the Ordovician-Silurian time in many areas of the world are amongst some of the most prolific petroleum source rocks. In the Canadian Arctic Archipelago this series is represented by basinal deep-water facies of the Cape Phillips Formation deposited on an enclosed embayment, beginning in the latest Ordovician and continuing for most of the Silurian. These strata, typically a few hundred meters thick and occurring over an area of approximately 500 km x 200 km, are known to contain intervals with elevated contents of organic matter and have been previously considered as one of the best potential hydrocarbon source rocks of the Franklinian successions. Despite that, this stratigraphic interval has received little attention in studies of petroleum systems of the Canadian Arctic which concentrated mostly on the Mesozoic sequences of the Sverdrup Basin where major hydrocarbon discoveries were made.
A Rock-Eval/TOC reconnaissance of over 500, mostly subsurface samples from the Cape Phillips Formation revealed TOC contents greater than 1% in the 80% of the analysed samples, with a maximum of 13.6% and an average of 2.3%. There are at least two main cycles of higher TOC within the unit that can be correlated throughout most of the formation occurrence area, a 50 to 75 m thick interval at the base and a second interval near the top of the formation. Tmax and PI values are commonly greater than 445oC and 0.40 respectively, indicating that most of the samples are thermally mature with respect to oil generation. Although the Hydrogen Index (HI) values approach 600 in some less mature samples, there is an apparent decrease in the HI values to less than 200 in samples with Tmax greater than 440oC. This change occurs over a 430oC to 440oC Tmax range (Fig. 1), suggesting that most petroleum might have been generated relatively early at what could otherwise be interpreted as the onset of the "oil window".
Extract yields, although quite variable, are commonly below 100 mg HC/g TOC, most likely reflecting hydrocarbon cracking, expulsion or destruction. Such interpretation is supported by the proportion of hydrocarbons in extracts which is greater than 40% in almost all of the extracts and greater than 60% in more than half of the samples, perhaps indicating hydrocarbon staining. Saturate fraction gas chromatograms are characterized by a smooth distribution of n-alkanes, often superimposed over a broad but low baseline hump. Pristane/phytane ratios are greater than 1.0 with an average of 1.4. Terpane and sterane biomarkers are fairly consistent amongst extracted samples. Terpane signatures are typically dominated by a large C30 hopane peak, smooth homohopane profile with the relative C31-C35 abundances decreasing with increasing carbon number and minor predominace of Ts over Tm. In several samples, however, these signatures appear quite mature as they are dominated by high abundances of tricyclic terpanes. Some of those samples also show low amounts of diasteranes relative to regular steranes. This characteristic might be source-related, as the presence of diastaranes in the Cape Phillips samples is otherwise more prominent. The regular steranes typically show C29>C27>C28 regular steranes pattern, likely reflecting contribution from several types of algae.
The overall biomarker characteristics are similar to those of the crude oil produced from Devonian reservoirs at Bent Horn. As the Cape Phillips Formation appears mature in close proximity to Bent Horn field, it has been considered as a main source of this oil. However, the pyrolysis data indicating possibility of an early generation of hydrocarbons within these strata could suggest potential for some occurrences of Cape Phillips sourced oil also in the areas of relatively lower thermal maturity of this formation, such as the south-eastern region of the Franklinian Basin.
Résumé(Résumé en langage clair et simple, non publié)
La présente étude présente les résultats d'analyses géochimiques organiques d'échantillons de roche et d'extraits organiques de la formation de Cape Phillips dans l'archipel arctique canadien. Cette unité couvre une zone d'environ 500 km x 200 km et elle est habituellement épaisse de quelques centaines de mètres. Comme elle contient plusieurs intervalles ayant des teneurs élevées en matière organique, on considère qu'elle comporte de la roche présentant un des meilleurs potentiels comme source d'hydrocarbures et elle a été corrélée avec le pétrole brut produit à partir des réservoirs du Dévonien dans le gisement de Bent Horn. Les données géochimiques organiques détaillées rapportées dans ce document comprennent les résultats d'études de pyrolyse Rock-Eval / COT (carbone organique total), d'extraction par solvant-chromatographie en phase gazeuse, ainsi que de chromatographie en phase gazeuse-spectrométrie de masse, et pourraient être très utiles pour les études et les évaluations des systèmes pétroliers de l'Arctique canadien.
GEOSCAN ID296102