Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/126540
Type: Thesis
Title: Isotopic and trace element constraints on the paleodepositional environment and redox history of the Greater McArthur Basin, Northern Territory
Author: Bullen, M. M.
Issue Date: 2017
School/Discipline: School of Physical Sciences
Abstract: The Limbunya Package of the Greater McArthur Basin, Northern Territory, hosts the oldest known hydrocarbon reservoirs. Despite the prospective nature of the Fraynes Formation (ca. 1638 Ma), the depositional environment and redox conditions for these organic-rich sediments and the associated carbonates is not well understood. Utilising high resolution stable and radiogenic isotope proxy records (δ13C, Sr87/Sr86 and Nd143/Nd144 ), we show that basin restriction was prevalent during deposition of the Fraynes Formation. As basin restriction has been suggested for the correlative Barney Creek Formation, we argue that this event affected the entire Greater McArthur Basin. The δ13C and Sr87/Sr86 isotopic signatures measured in this study (Manbulloo S1 core) are compared to corresponding stratigraphic units from the central McArthur Basin (LV09001 core). The results show evidence for coherent basin-wide C and Sr isotopic patterns that in turn could be used for the chemostratigraphy purposes during the deposition of the organic rich shales (Fraynes and Barney Creek Formations) and the overlying Reward dolomite sequences. Differences in δ13C isotope signal in the underlying Campbell Springs Dolomite (Teena Dolomite equivalent) are proposed to be related either to differences in the C isotope composition of local DIC pools at these two paleo-locations (i.e., LV09001 and Manbulloo sites), or the isotopically lighter δ13C signal in the latter core could reflect deeper depth of the deposition for dolomite at this site. Linking redox-sensitive trace element enrichments with total organic carbon data indicates that the water column was anoxic to euxinic during the deposition of the Fraynes Formation, with episodes of euxinia driven by the relatively high input of organic matter. Overall, knowledge gained here, particularly in regard to the links between paleo-depositional environments, redox conditions, and the occurrences of organic-rich shales, can be applied to other Precambrian frontier basins.
Dissertation Note: Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2017
Where: Greater McArthur Basin, Northern Territory
Keywords: Honours; Geology; Greater McArthur Basin; Paleoproterozoic, C-Sr-Nd isotopes; depositional environment; redox; chemostratigraphy
Description: This item is only available electronically.
Provenance: This electronic version is made publicly available by the University of Adelaide in accordance with its open access policy for student theses. Copyright in this thesis remains with the author. This thesis may incorporate third party material which has been used by the author pursuant to Fair Dealing exceptions. If you are the author of this thesis and do not wish it to be made publicly available, or you are the owner of any included third party copyright material you wish to be removed from this electronic version, please complete the take down form located at: http://www.adelaide.edu.au/legals
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