The impact of organic matter deposition and pre-oil window diagenetic transformation on commonly utilized thermal maturity indicators

dc.contributor.advisorPedersen, Per Kent
dc.contributor.advisorDewing, Keith
dc.contributor.authorSynnott, Dane Patrick
dc.contributor.committeememberFowler, Martin
dc.contributor.committeememberSanei, Hamed
dc.contributor.committeememberLarter, Stephen
dc.contributor.committeememberCuriale, Joseph
dc.date2021-11
dc.date.accessioned2021-08-26T18:07:04Z
dc.date.available2021-08-26T18:07:04Z
dc.date.issued2021-08-19
dc.description.abstractDespite decades of research on organic matter deposition, alteration, and preservation, the processes affecting and altering organic matter at low maturity are relatively poorly understood. Processes that affect deposition of organic matter, such as wildfires, or influence its preservation after deposition, such as diagenetic clay catalyzed transformation, can reduce the reliability of commonly applied thermal maturity proxies. This thesis integrated organic geochemistry and petrographic examination of samples from the Upper Cretaceous in Western Canada and the Canadian Arctic Islands to better understand processes that altered organic matter during deposition and early diagenetic. Samples from the Upper Cretaceous Kanguk Formation of the Canadian Arctic Islands have abundances of pyrogenic polycyclic aromatic hydrocarbon compounds and combustion-related organic macerals that show a distinct trend of increasing wildfire influence from the Turonian to the Campanian. This trend corresponds with increasing amounts of terrigenous organic matter in the marine Sverdrup Basin, in addition to increasing angiosperm-derived biomarkers. High rates of terrigenous organic matter deposition, accelerated by wildfires, have an important impact on the preservation of organic matter in a marine basin, as observed through degradation trends correlated to elevated primary productivity. A stratigraphically-controlled thermal maturity transect of samples ranging from eogenesis up to the peak of catagenesis was collected from the Upper Cretaceous Western Canadian Sedimentary Basin and examined using integrated organic geochemistry and organic petrology. The diagenetic transformation of hopanoid and steroid compounds was investigated, and key chemical transformations were calibrated to a maturity level. This investigation demonstrated that early clay-catalyzed backbone rearrangement in both hopanoid and steroid compounds has a profound impact on the hopanoid and steroid composition at higher maturity levels as well as on commonly applied thermal maturity indicators. A detailed calibration was completed, producing a correlation between a wide variety of common geochemical and optical thermal maturity indicators. Although each indicator has drawbacks, thirteen proxies are found to be effective, and a multi-disciplinary approach is recommended.en_US
dc.identifier.citationSynnott, D. P. (2021). The impact of organic matter deposition and pre-oil window diagenetic transformation on commonly utilized thermal maturity indicators (Doctoral thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca.en_US
dc.identifier.doihttp://dx.doi.org/10.11575/PRISM/39120
dc.identifier.urihttp://hdl.handle.net/1880/113766
dc.language.isoengen_US
dc.publisher.facultyScienceen_US
dc.publisher.institutionUniversity of Calgaryen
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.en_US
dc.subjectOrganic Geochemistryen_US
dc.subjectDiagenesisen_US
dc.subjectOrganic Petrologyen_US
dc.subjectThermal Maturityen_US
dc.subject.classificationGeochemistryen_US
dc.subject.classificationGeologyen_US
dc.titleThe impact of organic matter deposition and pre-oil window diagenetic transformation on commonly utilized thermal maturity indicatorsen_US
dc.typedoctoral thesisen_US
thesis.degree.disciplineGeoscienceen_US
thesis.degree.grantorUniversity of Calgaryen_US
thesis.degree.nameDoctor of Philosophy (PhD)en_US
ucalgary.item.requestcopytrueen_US
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