The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland
The rocks on Quirpon Island represent a well exposed cross section through the lower transported slices of the Hare Bay Allochthon and the uppermost parts of the autochthon. This thesis examines in detail the structural geometry of a part of the Hare Bay Allochthon. Its purpose is to analyze in deta...
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Memorial University of Newfoundland
1982
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ftmemorialuniv:oai:research.library.mun.ca:6925 2023-10-01T03:57:37+02:00 The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland Woodworth-Lynas, C. M. T. 1982 application/pdf https://research.library.mun.ca/6925/ https://research.library.mun.ca/6925/1/CTMWoodWorth-Lynas.pdf https://research.library.mun.ca/6925/3/CTMWoodWorth-Lynas.pdf en eng Memorial University of Newfoundland https://research.library.mun.ca/6925/1/CTMWoodWorth-Lynas.pdf https://research.library.mun.ca/6925/3/CTMWoodWorth-Lynas.pdf Woodworth-Lynas, C. M. T. <https://research.library.mun.ca/view/creator_az/Woodworth-Lynas=3AC=2E_M=2E_T=2E=3A=3A.html> (1982) The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland. Masters thesis, Memorial University of Newfoundland. thesis_license Thesis NonPeerReviewed 1982 ftmemorialuniv 2023-09-03T06:46:07Z The rocks on Quirpon Island represent a well exposed cross section through the lower transported slices of the Hare Bay Allochthon and the uppermost parts of the autochthon. This thesis examines in detail the structural geometry of a part of the Hare Bay Allochthon. Its purpose is to analyze in detail the deformational and metamorphic histories of the individual thrust slices and of the uppermost autochthon in order to correlate these histories as far as possible. Detailed field work reveals a reversed metamorphic gradient. Also, structural complexity and the numbers of generations of structures increases in higher slices. The highest slice at Quirpon, the retrogressed, mylonitic, actinolite greenschists of the Goose Cove Schist, rests above the sedimentary and volcanic rocks of the Maiden Point Formation to which heat was transferred from the cooling greenschists causing pervasive lower greenschist facies metamorphism. Much of the underlying middle Ordovician Goose Tickle Formation flysch, previously believed to be entirely autochthonous throughout the Hare Bay area, occurs as discrete, detached slivers within the Maiden Point Formation. Large scale, isoclinal, precleavage folds have been identified in both of these formations and are syn-emplacement in age. A well defined magnetic anomaly immediately east of Quirpon Island may indicate the presence of an outlier of ophiolite of the White Hills Peridotite, the highest structural slice in the Hare Bay Allochthon. Thesis Newfoundland Memorial University of Newfoundland: Research Repository Goose Tickle ENVELOPE(-56.017,-56.017,51.260,51.260) Maiden Point ENVELOPE(-55.765,-55.765,51.217,51.217) Quirpon ENVELOPE(-55.431,-55.431,51.583,51.583) Quirpon Island ENVELOPE(-55.431,-55.431,51.617,51.617) Tickle ENVELOPE(-67.733,-67.733,-67.116,-67.116) White Hills ENVELOPE(-54.748,-54.748,49.617,49.617) |
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Open Polar |
collection |
Memorial University of Newfoundland: Research Repository |
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ftmemorialuniv |
language |
English |
description |
The rocks on Quirpon Island represent a well exposed cross section through the lower transported slices of the Hare Bay Allochthon and the uppermost parts of the autochthon. This thesis examines in detail the structural geometry of a part of the Hare Bay Allochthon. Its purpose is to analyze in detail the deformational and metamorphic histories of the individual thrust slices and of the uppermost autochthon in order to correlate these histories as far as possible. Detailed field work reveals a reversed metamorphic gradient. Also, structural complexity and the numbers of generations of structures increases in higher slices. The highest slice at Quirpon, the retrogressed, mylonitic, actinolite greenschists of the Goose Cove Schist, rests above the sedimentary and volcanic rocks of the Maiden Point Formation to which heat was transferred from the cooling greenschists causing pervasive lower greenschist facies metamorphism. Much of the underlying middle Ordovician Goose Tickle Formation flysch, previously believed to be entirely autochthonous throughout the Hare Bay area, occurs as discrete, detached slivers within the Maiden Point Formation. Large scale, isoclinal, precleavage folds have been identified in both of these formations and are syn-emplacement in age. A well defined magnetic anomaly immediately east of Quirpon Island may indicate the presence of an outlier of ophiolite of the White Hills Peridotite, the highest structural slice in the Hare Bay Allochthon. |
format |
Thesis |
author |
Woodworth-Lynas, C. M. T. |
spellingShingle |
Woodworth-Lynas, C. M. T. The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland |
author_facet |
Woodworth-Lynas, C. M. T. |
author_sort |
Woodworth-Lynas, C. M. T. |
title |
The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland |
title_short |
The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland |
title_full |
The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland |
title_fullStr |
The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland |
title_full_unstemmed |
The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland |
title_sort |
geology and structure of the hare bay allochton at quirpon island, northern newfoundland |
publisher |
Memorial University of Newfoundland |
publishDate |
1982 |
url |
https://research.library.mun.ca/6925/ https://research.library.mun.ca/6925/1/CTMWoodWorth-Lynas.pdf https://research.library.mun.ca/6925/3/CTMWoodWorth-Lynas.pdf |
long_lat |
ENVELOPE(-56.017,-56.017,51.260,51.260) ENVELOPE(-55.765,-55.765,51.217,51.217) ENVELOPE(-55.431,-55.431,51.583,51.583) ENVELOPE(-55.431,-55.431,51.617,51.617) ENVELOPE(-67.733,-67.733,-67.116,-67.116) ENVELOPE(-54.748,-54.748,49.617,49.617) |
geographic |
Goose Tickle Maiden Point Quirpon Quirpon Island Tickle White Hills |
geographic_facet |
Goose Tickle Maiden Point Quirpon Quirpon Island Tickle White Hills |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
https://research.library.mun.ca/6925/1/CTMWoodWorth-Lynas.pdf https://research.library.mun.ca/6925/3/CTMWoodWorth-Lynas.pdf Woodworth-Lynas, C. M. T. <https://research.library.mun.ca/view/creator_az/Woodworth-Lynas=3AC=2E_M=2E_T=2E=3A=3A.html> (1982) The geology and structure of the Hare Bay Allochton at Quirpon Island, northern Newfoundland. Masters thesis, Memorial University of Newfoundland. |
op_rights |
thesis_license |
_version_ |
1778529426249613312 |