The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska
Thesis (M.S.) University of Alaska Fairbanks, 2003 The distribution of fold related fractures and other mesoscopic structures in asymmetrically folded Mississippian to Pennsylvanian Lisbume Group carbonates gives clues concerning the mechanism of folding. Since fracture sets pre-date and post-date f...
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ftunivalaska:oai:scholarworks.alaska.edu:11122/14933 2024-04-28T08:14:58+00:00 The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska Shackleton, John Ryan 2003-05 http://hdl.handle.net/11122/14933 en_US eng http://hdl.handle.net/11122/14933 Department of Geology and Geophysics Faults (Geology) Alaska West Porcupine Lake Valley Folds (Geology) Geology Stratigraphic Pennsylvanian Mississippian Thesis ms 2003 ftunivalaska 2024-04-03T14:16:26Z Thesis (M.S.) University of Alaska Fairbanks, 2003 The distribution of fold related fractures and other mesoscopic structures in asymmetrically folded Mississippian to Pennsylvanian Lisbume Group carbonates gives clues concerning the mechanism of folding. Since fracture sets pre-date and post-date folding, it is important, but sometimes difficult, to determine which fracture sets are related to folding. Higher density of fold related fractures and dissolution cleavage in the hinges than limbs of two folds in the study area is evidence for fixed hinge detachment folding. However, geometric modeling of box shaped folds in the study area suggests that some folds may have formed by either detachment folding or trishear fault propagation folding. Formulaic modeling of fracture density in a stratigraphic section using stratigraphic attributes such as lithology, bed thickness, and chert content predicts general trends in fracture density, but other factors such as slip along bed contacts may obscure the relationship between fracture density, lithology and bed thickness. Thesis Brooks Range Alaska University of Alaska: ScholarWorks@UA |
institution |
Open Polar |
collection |
University of Alaska: ScholarWorks@UA |
op_collection_id |
ftunivalaska |
language |
English |
topic |
Faults (Geology) Alaska West Porcupine Lake Valley Folds (Geology) Geology Stratigraphic Pennsylvanian Mississippian |
spellingShingle |
Faults (Geology) Alaska West Porcupine Lake Valley Folds (Geology) Geology Stratigraphic Pennsylvanian Mississippian Shackleton, John Ryan The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska |
topic_facet |
Faults (Geology) Alaska West Porcupine Lake Valley Folds (Geology) Geology Stratigraphic Pennsylvanian Mississippian |
description |
Thesis (M.S.) University of Alaska Fairbanks, 2003 The distribution of fold related fractures and other mesoscopic structures in asymmetrically folded Mississippian to Pennsylvanian Lisbume Group carbonates gives clues concerning the mechanism of folding. Since fracture sets pre-date and post-date folding, it is important, but sometimes difficult, to determine which fracture sets are related to folding. Higher density of fold related fractures and dissolution cleavage in the hinges than limbs of two folds in the study area is evidence for fixed hinge detachment folding. However, geometric modeling of box shaped folds in the study area suggests that some folds may have formed by either detachment folding or trishear fault propagation folding. Formulaic modeling of fracture density in a stratigraphic section using stratigraphic attributes such as lithology, bed thickness, and chert content predicts general trends in fracture density, but other factors such as slip along bed contacts may obscure the relationship between fracture density, lithology and bed thickness. |
format |
Thesis |
author |
Shackleton, John Ryan |
author_facet |
Shackleton, John Ryan |
author_sort |
Shackleton, John Ryan |
title |
The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska |
title_short |
The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska |
title_full |
The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska |
title_fullStr |
The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska |
title_full_unstemmed |
The relationship between fracturing, asymmetric folding, and normal faulting in Lisburne Group carbonates: West Porcupine Lake Valley, Northeastern Brooks Range, Alaska |
title_sort |
relationship between fracturing, asymmetric folding, and normal faulting in lisburne group carbonates: west porcupine lake valley, northeastern brooks range, alaska |
publishDate |
2003 |
url |
http://hdl.handle.net/11122/14933 |
genre |
Brooks Range Alaska |
genre_facet |
Brooks Range Alaska |
op_relation |
http://hdl.handle.net/11122/14933 Department of Geology and Geophysics |
_version_ |
1797580803293577216 |