Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska

Thesis (M.S.) University of Alaska Fairbanks, 2007 This study documents the stratigraphy, facies, facies associations, depositional environment, sequence stratigraphy, and conodont biostratigraphy of the upper Nanushuk River section of the Lisburne Group. 1621 meters of Kayak Shale and Lisburne Grou...

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Main Author: White, Jesse Garnett
Format: Thesis
Language:English
Published: 2007
Subjects:
Online Access:http://hdl.handle.net/11122/6939
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/6939 2023-05-15T15:46:57+02:00 Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska White, Jesse Garnett 2007-12 http://hdl.handle.net/11122/6939 en_US eng http://hdl.handle.net/11122/6939 Department of Geology and Geophysics Thesis ms 2007 ftunivalaska 2023-02-23T21:36:44Z Thesis (M.S.) University of Alaska Fairbanks, 2007 This study documents the stratigraphy, facies, facies associations, depositional environment, sequence stratigraphy, and conodont biostratigraphy of the upper Nanushuk River section of the Lisburne Group. 1621 meters of Kayak Shale and Lisburne Group rocks were measured and studied for facies analysis. Sixteen lithofacies and eleven microfacies were identified composing six facies assemblages. Facies analysis, stacking patterns, and associations suggest that the Nansushuk River section represents a homoclinal carbonate ramp recording an intertidal (Kayak Shale) and open marine to basin transitional sequence. Facies associations, stacking patterns and marine flooding surfaces helped to delineate major sequence boundaries and maximum flooding surfaces. Six 3rd order stratigraphic sequences have been identified in the Nanushuk River section. The section ranges in age from Osagean to lower Morrowan based on conodont biostratigraphy. The reservoir rock potential of the Nanushuk River section resides primarily in the dolomite of the Wachsmuth Limestone. The remainder of the section is considered 'tight' from a microfacies standpoint. Regionally, this study is important for paleogeographic reconstruction of the Lisburne Group across northern Alaska and adds to the general geologic knowledge of the Lisburne Group by obtaining stratigraphic data from a relatively isolated area in the Brooks Range. 1. Introduction -- 2. Conodont biostratigraphy and stratigraphy -- 3. Carbonate depositional models -- 4. Facies -- 5. Depositional model and sequence stratigraphy -- 6. Diagenesis -- 7. Source rock and reservoir potential -- 8. Discussion, conclusions, and future recommendations -- References -- CD-ROM Appendices : Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska. Thesis Brooks Range Alaska University of Alaska: ScholarWorks@UA Fairbanks Kayak ENVELOPE(103.217,103.217,71.533,71.533)
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Thesis (M.S.) University of Alaska Fairbanks, 2007 This study documents the stratigraphy, facies, facies associations, depositional environment, sequence stratigraphy, and conodont biostratigraphy of the upper Nanushuk River section of the Lisburne Group. 1621 meters of Kayak Shale and Lisburne Group rocks were measured and studied for facies analysis. Sixteen lithofacies and eleven microfacies were identified composing six facies assemblages. Facies analysis, stacking patterns, and associations suggest that the Nansushuk River section represents a homoclinal carbonate ramp recording an intertidal (Kayak Shale) and open marine to basin transitional sequence. Facies associations, stacking patterns and marine flooding surfaces helped to delineate major sequence boundaries and maximum flooding surfaces. Six 3rd order stratigraphic sequences have been identified in the Nanushuk River section. The section ranges in age from Osagean to lower Morrowan based on conodont biostratigraphy. The reservoir rock potential of the Nanushuk River section resides primarily in the dolomite of the Wachsmuth Limestone. The remainder of the section is considered 'tight' from a microfacies standpoint. Regionally, this study is important for paleogeographic reconstruction of the Lisburne Group across northern Alaska and adds to the general geologic knowledge of the Lisburne Group by obtaining stratigraphic data from a relatively isolated area in the Brooks Range. 1. Introduction -- 2. Conodont biostratigraphy and stratigraphy -- 3. Carbonate depositional models -- 4. Facies -- 5. Depositional model and sequence stratigraphy -- 6. Diagenesis -- 7. Source rock and reservoir potential -- 8. Discussion, conclusions, and future recommendations -- References -- CD-ROM Appendices : Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska.
format Thesis
author White, Jesse Garnett
spellingShingle White, Jesse Garnett
Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska
author_facet White, Jesse Garnett
author_sort White, Jesse Garnett
title Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska
title_short Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska
title_full Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska
title_fullStr Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska
title_full_unstemmed Carbonate facies and sequence stratigraphy of the carboniferous Lisburne group, Upper Nanushuk River Region, Central Brooks Range, Alaska
title_sort carbonate facies and sequence stratigraphy of the carboniferous lisburne group, upper nanushuk river region, central brooks range, alaska
publishDate 2007
url http://hdl.handle.net/11122/6939
long_lat ENVELOPE(103.217,103.217,71.533,71.533)
geographic Fairbanks
Kayak
geographic_facet Fairbanks
Kayak
genre Brooks Range
Alaska
genre_facet Brooks Range
Alaska
op_relation http://hdl.handle.net/11122/6939
Department of Geology and Geophysics
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