{"id":{"repo_id":"carleton","oai_identifier":"oai:carleton.scholaris.ca:20.500.14718/27319"},"canonical_url":"https://search.dev.ndltd.org/etd/carleton/oai:carleton.scholaris.ca:20.500.14718/27319","repository":{"repo_id":"carleton","name":"Carleton University","base_url":"https://carleton.scholaris.ca/server/oai/request"},"display":{"title":"Structures in the Wabush Formation west of Wabush Lake with special reference to the Smallwood Mine","abstract":"Wabush Formation consists of a lower carbonate-silicate member and an upper iron-oxide member. The stratigraphic succession of the rocks associated with the Wabush Formation is established from surface geological mapping and diamond drilling.In the northern part of the Smallwood Mine the Wabush Formation appears to be composed of two iron-oxide and two carbonate-silicate members. This repetition is due not to primary deposition or to thrust faulting but to repeated folding. The first generation of folds trends easterly, the second generation trends 020°1 southwest of Wabush Lake, and 350° to 010° west of the central part of the lake. Folds of the third generation trend 040° to 060°. Both sets of later folds are overturned to the west or northwest. The rocks of the Wabush Formation have, therefore, undergone deformation by forces acting at different times in different directions.1. All angular values expressed in three figures refer to azimuth.","abstract_html":"Wabush Formation consists of a lower carbonate-silicate member and an upper iron-oxide member. The stratigraphic succession of the rocks associated with the Wabush Formation is established from surface geological mapping and diamond drilling.In the northern part of the Smallwood Mine the Wabush Formation appears to be composed of two iron-oxide and two carbonate-silicate members. This repetition is due not to primary deposition or to thrust faulting but to repeated folding. The first generation of folds trends easterly, the second generation trends 020°1 southwest of Wabush Lake, and 350° to 010° west of the central part of the lake. Folds of the third generation trend 040° to 060°. Both sets of later folds are overturned to the west or northwest. The rocks of the Wabush Formation have, therefore, undergone deformation by forces acting at different times in different directions.1. All angular values expressed in three figures refer to azimuth.","abstract_has_math":false,"creators":["Hamilton, Courtney George"],"institution":"Carleton University","degree_name":"Master of Science (M.Sc.)","degree_level":"Master's","degree_discipline":"Geology","degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1967,"date_issued":"1967","date_published":"1967","updated_at":"2026-07-24T01:34:36Z","subjects":[],"languages":["en"],"rights":["Copyright © 1967 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner."],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier.doi","label":"DOI","values":["10.22215/etd/1967-13044"],"render_values":[{"text":"10.22215/etd/1967-13044","href":"https://doi.org/10.22215/etd/1967-13044","code":true}]}]},"links":{"outbound_url":"https://hdl.handle.net/20.500.14718/27319","outbound_label":"Handle","outbound_source":"dc:identifier.uri"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Hamilton, Courtney George"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.accessioned","label":"Dc Date Accessioned","values":["2025-04-08T16:25:50Z"]},{"key":"dc:date.available","label":"Dc Date Available","values":["2025-04-08T16:25:50Z"]},{"key":"dc:date.issued","label":"Date","values":["1967"]},{"key":"dc:publisher","label":"Institution","values":["Carleton University"]},{"key":"dc:type","label":"Dc Type","values":["thesis"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Geology"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Master's"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Master of Science (M.Sc.)"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language.iso","label":"Language (ISO)","values":["en"]},{"key":"dc:rights","label":"Dc Rights","values":["Copyright © 1967 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner."]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier.doi","label":"DOI","values":["10.22215/etd/1967-13044"]},{"key":"dc:identifier.uri","label":"Identifier URI","values":["https://hdl.handle.net/20.500.14718/27319"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Wabush Formation consists of a lower carbonate-silicate member and an upper iron-oxide member. The stratigraphic succession of the rocks associated with the Wabush Formation is established from surface geological mapping and diamond drilling.In the northern part of the Smallwood Mine the Wabush Formation appears to be composed of two iron-oxide and two carbonate-silicate members. This repetition is due not to primary deposition or to thrust faulting but to repeated folding. The first generation of folds trends easterly, the second generation trends 020°1 southwest of Wabush Lake, and 350° to 010° west of the central part of the lake. Folds of the third generation trend 040° to 060°. Both sets of later folds are overturned to the west or northwest. The rocks of the Wabush Formation have, therefore, undergone deformation by forces acting at different times in different directions.1. All angular values expressed in three figures refer to azimuth."]},{"key":"dc:title","label":"Title","values":["Structures in the Wabush Formation west of Wabush Lake with special reference to the Smallwood Mine"]}]}],"canonical_facts":{"dc:creator":["Hamilton, Courtney George"],"dc:date.accessioned":["2025-04-08T16:25:50Z"],"dc:date.available":["2025-04-08T16:25:50Z"],"dc:date.issued":["1967"],"dc:description.abstract":["Wabush Formation consists of a lower carbonate-silicate member and an upper iron-oxide member. The stratigraphic succession of the rocks associated with the Wabush Formation is established from surface geological mapping and diamond drilling.In the northern part of the Smallwood Mine the Wabush Formation appears to be composed of two iron-oxide and two carbonate-silicate members. This repetition is due not to primary deposition or to thrust faulting but to repeated folding. The first generation of folds trends easterly, the second generation trends 020°1 southwest of Wabush Lake, and 350° to 010° west of the central part of the lake. Folds of the third generation trend 040° to 060°. Both sets of later folds are overturned to the west or northwest. The rocks of the Wabush Formation have, therefore, undergone deformation by forces acting at different times in different directions.1. All angular values expressed in three figures refer to azimuth."],"dc:identifier.doi":["10.22215/etd/1967-13044"],"dc:identifier.uri":["https://hdl.handle.net/20.500.14718/27319"],"dc:language.iso":["en"],"dc:publisher":["Carleton University"],"dc:rights":["Copyright © 1967 the author(s). Theses may be used for non-commercial research, educational, or related academic purposes only. Such uses include personal study, research, scholarship, and teaching. Theses may only be shared by linking to Carleton University Institutional Repository and no part may be used without proper attribution to the author. No part may be used for commercial purposes directly or indirectly via a for-profit platform; no adaptation or derivative works are permitted without consent from the copyright owner."],"dc:title":["Structures in the Wabush Formation west of Wabush Lake with special reference to the Smallwood Mine"],"dc:type":["thesis"],"thesis:degree_discipline":["Geology"],"thesis:degree_level":["Master's"],"thesis:degree_name":["Master of Science (M.Sc.)"]},"updated_at":"2026-07-24T01:34:36Z"}