Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada
The Swayze Greenstone Belt is an Archean granitoid-greenstone terrain located in the central part of the Superior Province in Canada. In this region, a number of geophysical projects have been completed by MERC (Mineral Exploration Research Centre, Laurentian University, Sudbury) using different met...
- Autores:
-
Satizábal Pazos, Daniel Mauricio
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2020
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/51280
- Acceso en línea:
- http://hdl.handle.net/1992/51280
- Palabra clave:
- Geofísica
Gravimetría (Geofísica)
Geociencias
- Rights
- openAccess
- License
- http://creativecommons.org/licenses/by-nc-sa/4.0/
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dc.title.spa.fl_str_mv |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
title |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
spellingShingle |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada Geofísica Gravimetría (Geofísica) Geociencias |
title_short |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
title_full |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
title_fullStr |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
title_full_unstemmed |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
title_sort |
Analysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, Canada |
dc.creator.fl_str_mv |
Satizábal Pazos, Daniel Mauricio |
dc.contributor.advisor.none.fl_str_mv |
Nitescu, Bogdan |
dc.contributor.author.none.fl_str_mv |
Satizábal Pazos, Daniel Mauricio |
dc.contributor.jury.none.fl_str_mv |
Pedraza Hernández, Andrés Fernando |
dc.subject.armarc.none.fl_str_mv |
Geofísica Gravimetría (Geofísica) |
topic |
Geofísica Gravimetría (Geofísica) Geociencias |
dc.subject.themes.none.fl_str_mv |
Geociencias |
description |
The Swayze Greenstone Belt is an Archean granitoid-greenstone terrain located in the central part of the Superior Province in Canada. In this region, a number of geophysical projects have been completed by MERC (Mineral Exploration Research Centre, Laurentian University, Sudbury) using different methods. In addition, the Geological Survey of Canada has collected geophysical data that is publicly available. The main objective of this project consisted in doing an analysis and modelling of public regional gravity and aeromagnetic data of the Swayze Greenstone Belt with the aim of examining the geometry and depth extent of the geological bodies that occur in the area of the belt. Gravity and aeromagnetic data from the Geoscience Data base of the Geological Survey of Canada was used, and the GM-SYS tool extension from Oasis montaj - Educational software edition version 9.8.1 was used for forward modelling of the gravity data. Five models were built, three transverse and two longitudinal to the geological structures. The residual magnetic total field of the SGB and its first vertical derivative were analyzed qualitatively by comparing them with the geological units and main structures of the area. A general perspective of the geometry and depth extent of the formations and groups of the SGB was obtained, being concluded that the Brett Lake Syncline is a tight fold, which changes to an open fold in the western part of the Swayze area. The Woman River Anticline is an open to tight fold. The structures modeled under the Brett Lake Syncline vary in depth between 5 and 9 km, whereas for the structures under the Woman River Anticline vary between 2 and 15 km. The deepest parts in the greenstone rocks are located in the central-southern area of the SGB. Furthermore, it was observed the geometry of the SGB and the surrounding and intruding tonalite-granodiorite plutons form a typical Archean keel-and-dome pattern. |
publishDate |
2020 |
dc.date.issued.none.fl_str_mv |
2020 |
dc.date.accessioned.none.fl_str_mv |
2021-08-10T18:18:31Z |
dc.date.available.none.fl_str_mv |
2021-08-10T18:18:31Z |
dc.type.spa.fl_str_mv |
Trabajo de grado - Pregrado |
dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/bachelorThesis |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_7a1f |
dc.type.content.spa.fl_str_mv |
Text |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/TP |
format |
http://purl.org/coar/resource_type/c_7a1f |
dc.identifier.uri.none.fl_str_mv |
http://hdl.handle.net/1992/51280 |
dc.identifier.pdf.none.fl_str_mv |
22903.pdf |
dc.identifier.instname.spa.fl_str_mv |
instname:Universidad de los Andes |
dc.identifier.reponame.spa.fl_str_mv |
reponame:Repositorio Institucional Séneca |
dc.identifier.repourl.spa.fl_str_mv |
repourl:https://repositorio.uniandes.edu.co/ |
url |
http://hdl.handle.net/1992/51280 |
identifier_str_mv |
22903.pdf instname:Universidad de los Andes reponame:Repositorio Institucional Séneca repourl:https://repositorio.uniandes.edu.co/ |
dc.language.iso.none.fl_str_mv |
eng |
language |
eng |
dc.rights.uri.*.fl_str_mv |
http://creativecommons.org/licenses/by-nc-sa/4.0/ |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.coar.spa.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-sa/4.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
dc.format.extent.none.fl_str_mv |
48 hojas |
dc.format.mimetype.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidad de los Andes |
dc.publisher.program.none.fl_str_mv |
Geociencias |
dc.publisher.faculty.none.fl_str_mv |
Facultad de Ciencias |
dc.publisher.department.none.fl_str_mv |
Departamento de Geociencias |
publisher.none.fl_str_mv |
Universidad de los Andes |
institution |
Universidad de los Andes |
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Al consultar y hacer uso de este recurso, está aceptando las condiciones de uso establecidas por los autores.http://creativecommons.org/licenses/by-nc-sa/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Nitescu, Bogdan98c78473-43b4-4659-ab3e-25e0970851a5400Satizábal Pazos, Daniel Mauricio523a5eae-e45f-46f5-89aa-5f005d5e0e55500Pedraza Hernández, Andrés Fernando2021-08-10T18:18:31Z2021-08-10T18:18:31Z2020http://hdl.handle.net/1992/5128022903.pdfinstname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/The Swayze Greenstone Belt is an Archean granitoid-greenstone terrain located in the central part of the Superior Province in Canada. In this region, a number of geophysical projects have been completed by MERC (Mineral Exploration Research Centre, Laurentian University, Sudbury) using different methods. In addition, the Geological Survey of Canada has collected geophysical data that is publicly available. The main objective of this project consisted in doing an analysis and modelling of public regional gravity and aeromagnetic data of the Swayze Greenstone Belt with the aim of examining the geometry and depth extent of the geological bodies that occur in the area of the belt. Gravity and aeromagnetic data from the Geoscience Data base of the Geological Survey of Canada was used, and the GM-SYS tool extension from Oasis montaj - Educational software edition version 9.8.1 was used for forward modelling of the gravity data. Five models were built, three transverse and two longitudinal to the geological structures. The residual magnetic total field of the SGB and its first vertical derivative were analyzed qualitatively by comparing them with the geological units and main structures of the area. A general perspective of the geometry and depth extent of the formations and groups of the SGB was obtained, being concluded that the Brett Lake Syncline is a tight fold, which changes to an open fold in the western part of the Swayze area. The Woman River Anticline is an open to tight fold. The structures modeled under the Brett Lake Syncline vary in depth between 5 and 9 km, whereas for the structures under the Woman River Anticline vary between 2 and 15 km. The deepest parts in the greenstone rocks are located in the central-southern area of the SGB. Furthermore, it was observed the geometry of the SGB and the surrounding and intruding tonalite-granodiorite plutons form a typical Archean keel-and-dome pattern.El Swayze Greenstone Belt es un terreno compuesto de granitoides y rocas verdes del Arcaico, ubicado en la parte central de la provincia superior en Canadá. En esta región, el MERC (Mineral Exploration Research Centre, Laurentian University, Sudbury) ha completado una serie de proyectos geofísicos utilizando diferentes métodos. Además, el Servicio Geológico de Canadá ha recopilado datos geofísicos que están a disposición del público. El objetivo principal de este proyecto consistió en realizar un análisis y modelado de datos gravitacionales y aeromagnéticos regionales públicos del Swayze Greenstone Belt con el objetivo de examinar la geometría y extensión de profundidad de los cuerpos geológicos que ocurren en el área. Estos datos se obtuvieron de la Geoscience Data base del Servicio Geológico de Canadá, y se utilizó la extensión de la herramienta GM-SYS de Oasis montaj - Educational software edition version 9.8.1 para el modelado directo de los datos gravitacionales. Se construyeron cinco modelos, tres transversales y dos longitudinales a las estructuras geológicas. El campo magnético residual total del SGB y su primera derivada vertical se analizaron cualitativamente comparándolos con las unidades geológicas y estructuras principales del área. Se obtuvo una perspectiva general de la geometría y extensión de profundidad de las formaciones y grupos del SGB, concluyendo que el sinclinal de Brett Lake es un pliegue estrecho, que cambia a un pliegue abierto en la parte occidental del área de Swayze. El anticlinal de Woman River es un pliegue abierto a cerrado. Las estructuras modeladas bajo el sinclinal de Brett Lake varían en profundidad entre 5 y 9 km, mientras que para el anticlinal de Woman River varían entre 2 y 15 km. Las partes más profundas de las rocas verdes se encuentran en la zona centro-sur del SGB. Además, se observó que la geometría del SGB y los plutones de tonalita-granodiorita circundantes e intrusivos forman un patrón típico de keel-and-dome arcaico.GeocientíficoPregrado48 hojasapplication/pdfengUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de GeocienciasAnalysis and interpretation of regional geophysical data in the Swayze Greenstone Belt of the superior province, CanadaTrabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesishttp://purl.org/coar/resource_type/c_7a1fhttp://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/TPGeofísicaGravimetría (Geofísica)Geociencias201520679PublicationTEXT22903.pdf.txt22903.pdf.txtExtracted texttext/plain79700https://repositorio.uniandes.edu.co/bitstreams/fe616b9a-b86f-4938-b13b-5fe84f82699a/downloadcb9eaf598900512ae638516ee480421cMD54ORIGINAL22903.pdfapplication/pdf5435650https://repositorio.uniandes.edu.co/bitstreams/ebea5642-83e7-4831-805e-1b9f65d767f0/download602691ca7a488213df0aad784a1848e4MD51THUMBNAIL22903.pdf.jpg22903.pdf.jpgIM Thumbnailimage/jpeg9073https://repositorio.uniandes.edu.co/bitstreams/cb0edc5d-7903-4111-9579-9473f48c1698/download34cebd9f3a522a085683bc7f53a3079bMD551992/51280oai:repositorio.uniandes.edu.co:1992/512802023-10-10 18:18:35.884http://creativecommons.org/licenses/by-nc-sa/4.0/open.accesshttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.co |