Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska

Thesis (M.S.) University of Alaska Fairbanks, 2010 "The character of structures in the Gilead Creek region is influenced by the mechanical stratigraphy in the area. Shortening is distributed throughout the mechanical stratigraphy along detachments in the incompetent Kayak, Kavik, Kingak, and Hu...

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Main Author: Speeter, Garrett
Format: Thesis
Language:English
Published: 2010
Subjects:
Online Access:http://hdl.handle.net/11122/12781
id ftunivalaska:oai:scholarworks.alaska.edu:11122/12781
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/12781 2023-05-15T15:46:57+02:00 Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska Speeter, Garrett 2010-12 http://hdl.handle.net/11122/12781 en_US eng http://hdl.handle.net/11122/12781 Department of Geology and Geophysics Orogenic belts Brooks Range Orogeny Geological folds Geological basins Thesis ms 2010 ftunivalaska 2023-02-23T21:37:59Z Thesis (M.S.) University of Alaska Fairbanks, 2010 "The character of structures in the Gilead Creek region is influenced by the mechanical stratigraphy in the area. Shortening is distributed throughout the mechanical stratigraphy along detachments in the incompetent Kayak, Kavik, Kingak, and Hue Shales. Detachment intervals separate competent Lisburne Group, Echooka Formation, Ledge Sandstone/Shublik Formation, Gilead sandstone, and moderately competent Seabee Formation from each other and allow the competent units to fold at distinct wavelengths according to their mechanical properties. Thick, competent units tend to form long-wavelength folds. Thin, competent units form relatively short-wavelength folds. Thin, competent units that are structurally bound to a thicker, structurally more dominant unit, adhere to the structural style of the dominant unit unless there is some detachment between them. Strain is distributed through shale intervals in the moderately competent units, allowing short-wavelength folds in the thin competent beds. The dominant trend of structures in the area is northeast overprinted on east. East-trending structures formed during the ~60 Ma event that formed the main axis of the Brooks Range and its foothills. Northeast-trending structures formed during the formation of the northeastern Brooks Range dated at ~45 Ma, ~35 Ma, and ~27 Ma, manifest locally by the compressional uplift of the Echooka anticlinorium southeast of Gilead Creek"--Leaf iii. Alaska Division of Geological and Geophysical Surveys, The University of Alaska’s Geophysical Institute, The University of Alaska Geology and Geophysics Department, The Alaska Space Grant Program, The Geological Society of America John T. Dillon award for tectonic and structural fieldwork in Alaska, The American Association of Petroleum Geologists, and BP Amoco 1. Geologic setting -- 1.1. Introduction and significance -- 1.2. Geologic setting -- 1.3. Regional stratigraphy -- 1.4. Regional structure -- 2. Methods and data -- 2.1. Geologic ... Thesis Brooks Range Alaska University of Alaska: ScholarWorks@UA Dillon ENVELOPE(-108.935,-108.935,55.933,55.933) 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
topic Orogenic belts
Brooks Range
Orogeny
Geological folds
Geological basins
spellingShingle Orogenic belts
Brooks Range
Orogeny
Geological folds
Geological basins
Speeter, Garrett
Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska
topic_facet Orogenic belts
Brooks Range
Orogeny
Geological folds
Geological basins
description Thesis (M.S.) University of Alaska Fairbanks, 2010 "The character of structures in the Gilead Creek region is influenced by the mechanical stratigraphy in the area. Shortening is distributed throughout the mechanical stratigraphy along detachments in the incompetent Kayak, Kavik, Kingak, and Hue Shales. Detachment intervals separate competent Lisburne Group, Echooka Formation, Ledge Sandstone/Shublik Formation, Gilead sandstone, and moderately competent Seabee Formation from each other and allow the competent units to fold at distinct wavelengths according to their mechanical properties. Thick, competent units tend to form long-wavelength folds. Thin, competent units form relatively short-wavelength folds. Thin, competent units that are structurally bound to a thicker, structurally more dominant unit, adhere to the structural style of the dominant unit unless there is some detachment between them. Strain is distributed through shale intervals in the moderately competent units, allowing short-wavelength folds in the thin competent beds. The dominant trend of structures in the area is northeast overprinted on east. East-trending structures formed during the ~60 Ma event that formed the main axis of the Brooks Range and its foothills. Northeast-trending structures formed during the formation of the northeastern Brooks Range dated at ~45 Ma, ~35 Ma, and ~27 Ma, manifest locally by the compressional uplift of the Echooka anticlinorium southeast of Gilead Creek"--Leaf iii. Alaska Division of Geological and Geophysical Surveys, The University of Alaska’s Geophysical Institute, The University of Alaska Geology and Geophysics Department, The Alaska Space Grant Program, The Geological Society of America John T. Dillon award for tectonic and structural fieldwork in Alaska, The American Association of Petroleum Geologists, and BP Amoco 1. Geologic setting -- 1.1. Introduction and significance -- 1.2. Geologic setting -- 1.3. Regional stratigraphy -- 1.4. Regional structure -- 2. Methods and data -- 2.1. Geologic ...
format Thesis
author Speeter, Garrett
author_facet Speeter, Garrett
author_sort Speeter, Garrett
title Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska
title_short Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska
title_full Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska
title_fullStr Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska
title_full_unstemmed Character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the Gilead creek region of the Northeastern Brooks Range, Alaska
title_sort character and controls of fold-and-thrust deformation from pre-orogenic to foreland basin deposits: an example from the gilead creek region of the northeastern brooks range, alaska
publishDate 2010
url http://hdl.handle.net/11122/12781
long_lat ENVELOPE(-108.935,-108.935,55.933,55.933)
ENVELOPE(103.217,103.217,71.533,71.533)
geographic Dillon
Fairbanks
Kayak
geographic_facet Dillon
Fairbanks
Kayak
genre Brooks Range
Alaska
genre_facet Brooks Range
Alaska
op_relation http://hdl.handle.net/11122/12781
Department of Geology and Geophysics
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