High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska

Thesis (M.S.) University of Alaska Fairbanks, 2004 Triassic age rocks constitute an important sedimentary interval on the North Slope of Alaska, because they include organic-rich source rocks that generated much of the oil that accumulated in the Prudhoe Bay field. Three detailed measured sections i...

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Main Author: Kelly, Landon Neal
Format: Thesis
Language:English
Published: 2004
Subjects:
Online Access:http://hdl.handle.net/11122/6013
id ftunivalaska:oai:scholarworks.alaska.edu:11122/6013
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/6013 2023-05-15T15:46:58+02:00 High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska Kelly, Landon Neal 2004-08 http://hdl.handle.net/11122/6013 en_US eng http://hdl.handle.net/11122/6013 Department of Geology and Geophysics Thesis 2004 ftunivalaska 2023-02-23T21:36:34Z Thesis (M.S.) University of Alaska Fairbanks, 2004 Triassic age rocks constitute an important sedimentary interval on the North Slope of Alaska, because they include organic-rich source rocks that generated much of the oil that accumulated in the Prudhoe Bay field. Three detailed measured sections in the northeast and north-central Brooks Range are characterized using sequence stratigraphy, chemostratigraphy, biostratigraphy and ichnofabric, allowing interpretations about the evolution of the depositional environment and general paleogeographic setting through the Middle and Upper Triassic. High resolution correlation provides insight into the timing and pattern of source rock accumulation in the Shublik and Otuk Formations. Sequence and chemo-stratigraphic analyses suggest that deposition took place on a broad, low-angle shelf under fluctuating paleoceanographic conditions. Recorded are three third order sequences, each containing a sea level rise and highstand. Glauconitic, phosphatic, and organic-rich rocks of the Shublik and Otuk Formations indicate deposition in an environment characterized by oceanic upwelling. Organic and inorganic geochemical data support interpretations concerning paleoxygenation gradients. The cerium anomaly, manganese, phosphorus, vanadium, total organic carbon, and calcium-manganese ratio indicate dominantly oxic bottom waters during the Middle Triassic, dominantly low oxygen or anoxic conditions during much of the Upper Triassic, and a return to more oxic conditions in the late Upper Triassic. Ch. 1. Introduction -- ch. 2. Facies descriptions and formation subdivisions -- ch. 3. Facies associations and interpretations -- ch. 4. Sequence stratigraphy -- ch. 5. Geochemistry -- ch. 6. Results and conclusions -- Appendix 1 -- Appendix 2 -- References cited. Thesis Brooks Range north slope Prudhoe Bay Alaska University of Alaska: ScholarWorks@UA Fairbanks
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Thesis (M.S.) University of Alaska Fairbanks, 2004 Triassic age rocks constitute an important sedimentary interval on the North Slope of Alaska, because they include organic-rich source rocks that generated much of the oil that accumulated in the Prudhoe Bay field. Three detailed measured sections in the northeast and north-central Brooks Range are characterized using sequence stratigraphy, chemostratigraphy, biostratigraphy and ichnofabric, allowing interpretations about the evolution of the depositional environment and general paleogeographic setting through the Middle and Upper Triassic. High resolution correlation provides insight into the timing and pattern of source rock accumulation in the Shublik and Otuk Formations. Sequence and chemo-stratigraphic analyses suggest that deposition took place on a broad, low-angle shelf under fluctuating paleoceanographic conditions. Recorded are three third order sequences, each containing a sea level rise and highstand. Glauconitic, phosphatic, and organic-rich rocks of the Shublik and Otuk Formations indicate deposition in an environment characterized by oceanic upwelling. Organic and inorganic geochemical data support interpretations concerning paleoxygenation gradients. The cerium anomaly, manganese, phosphorus, vanadium, total organic carbon, and calcium-manganese ratio indicate dominantly oxic bottom waters during the Middle Triassic, dominantly low oxygen or anoxic conditions during much of the Upper Triassic, and a return to more oxic conditions in the late Upper Triassic. Ch. 1. Introduction -- ch. 2. Facies descriptions and formation subdivisions -- ch. 3. Facies associations and interpretations -- ch. 4. Sequence stratigraphy -- ch. 5. Geochemistry -- ch. 6. Results and conclusions -- Appendix 1 -- Appendix 2 -- References cited.
format Thesis
author Kelly, Landon Neal
spellingShingle Kelly, Landon Neal
High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska
author_facet Kelly, Landon Neal
author_sort Kelly, Landon Neal
title High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska
title_short High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska
title_full High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska
title_fullStr High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska
title_full_unstemmed High resolution sequence stratigraphy and geochemistry of middle and upper Triassic sedimentary rocks, northeast and central Brooks Range, Alaska
title_sort high resolution sequence stratigraphy and geochemistry of middle and upper triassic sedimentary rocks, northeast and central brooks range, alaska
publishDate 2004
url http://hdl.handle.net/11122/6013
geographic Fairbanks
geographic_facet Fairbanks
genre Brooks Range
north slope
Prudhoe Bay
Alaska
genre_facet Brooks Range
north slope
Prudhoe Bay
Alaska
op_relation http://hdl.handle.net/11122/6013
Department of Geology and Geophysics
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