InSAR from the Socotra Island from June to October 2017
In this work, InSAR from the Socotra island using Sentinel 1A data from June to October of 2017 was elaborated using European Space Agency's SNAP. The results revealed that the island experienced general subsidence which is confirmed by the data of a GPS station from the Nevada Geodetic laborat...
- Autores:
-
Reyes Martínez, Daniel
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2017
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/39803
- Acceso en línea:
- http://hdl.handle.net/1992/39803
- Palabra clave:
- Subsidencias (Geología)
Movimientos tectónicos
Sensores remotos
Radar de apertura sintética
Geociencias
- Rights
- openAccess
- License
- http://creativecommons.org/licenses/by-nc-sa/4.0/
id |
UNIANDES2_ad62a714659a8a8a0bdbb9d2a65c3fbc |
---|---|
oai_identifier_str |
oai:repositorio.uniandes.edu.co:1992/39803 |
network_acronym_str |
UNIANDES2 |
network_name_str |
Séneca: repositorio Uniandes |
repository_id_str |
|
dc.title.es_CO.fl_str_mv |
InSAR from the Socotra Island from June to October 2017 |
title |
InSAR from the Socotra Island from June to October 2017 |
spellingShingle |
InSAR from the Socotra Island from June to October 2017 Subsidencias (Geología) Movimientos tectónicos Sensores remotos Radar de apertura sintética Geociencias |
title_short |
InSAR from the Socotra Island from June to October 2017 |
title_full |
InSAR from the Socotra Island from June to October 2017 |
title_fullStr |
InSAR from the Socotra Island from June to October 2017 |
title_full_unstemmed |
InSAR from the Socotra Island from June to October 2017 |
title_sort |
InSAR from the Socotra Island from June to October 2017 |
dc.creator.fl_str_mv |
Reyes Martínez, Daniel |
dc.contributor.advisor.none.fl_str_mv |
Pearse, Jillian |
dc.contributor.author.none.fl_str_mv |
Reyes Martínez, Daniel |
dc.contributor.jury.none.fl_str_mv |
Tary, Jean Baptiste |
dc.subject.keyword.es_CO.fl_str_mv |
Subsidencias (Geología) Movimientos tectónicos Sensores remotos Radar de apertura sintética |
topic |
Subsidencias (Geología) Movimientos tectónicos Sensores remotos Radar de apertura sintética Geociencias |
dc.subject.themes.none.fl_str_mv |
Geociencias |
description |
In this work, InSAR from the Socotra island using Sentinel 1A data from June to October of 2017 was elaborated using European Space Agency's SNAP. The results revealed that the island experienced general subsidence which is confirmed by the data of a GPS station from the Nevada Geodetic laboratory that also recorded continuous subsidence in the year 2010 in a period of 5 months. Unfortunately, this was the most recent recorded data. Since the island is located between three ridges (Sheba ridge to the north, Gulf of Aden ridge to the north west, and the Carlsbridge rift to the south east), uplift was expected and finding only subsidence was unforeseen. One cause for this subsidence is attributed to the formation of pull apart basins in strike-fault systems en echelon (Burg, 2017) which is supported by the reported presence of normal faults in the northeast of the island (Beydoun & Roy, 1969; Fournier, Huchon, Khanbari, & Leroy, 2007). However, this mechanism only explains the subsidence in the west block; one of the two similar sized blocks that form the whole island according to various studies (Fournier, Huchon, Khanbari, & Leroy, 2007) separated by the Haddiboh transform zone. A probable cause for this subsidence may be the activity of scars from past continental collisions that lie deep in the crust and that control topography (Heron, Pysklywec, & Stephenson, 2016), however with InSAR it is impossible to determine where are these structures and to prove their existence more geophysical surveys are needed to examine the crust's structure there |
publishDate |
2017 |
dc.date.issued.none.fl_str_mv |
2017 |
dc.date.accessioned.none.fl_str_mv |
2020-06-10T16:33:05Z |
dc.date.available.none.fl_str_mv |
2020-06-10T16:33:05Z |
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/1992/39803 |
dc.identifier.pdf.none.fl_str_mv |
u807219.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/1992/39803 |
identifier_str_mv |
u807219.pdf instname:Universidad de los Andes reponame:Repositorio Institucional Séneca repourl:https://repositorio.uniandes.edu.co/ |
dc.language.iso.es_CO.fl_str_mv |
spa |
language |
spa |
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.es_CO.fl_str_mv |
38 hojas |
dc.format.mimetype.es_CO.fl_str_mv |
application/pdf |
dc.publisher.es_CO.fl_str_mv |
Uniandes |
dc.publisher.program.es_CO.fl_str_mv |
Geociencias |
dc.publisher.faculty.es_CO.fl_str_mv |
Facultad de Ciencias |
dc.publisher.department.es_CO.fl_str_mv |
Departamento de Geociencias |
dc.source.es_CO.fl_str_mv |
instname:Universidad de los Andes reponame:Repositorio Institucional Séneca |
instname_str |
Universidad de los Andes |
institution |
Universidad de los Andes |
reponame_str |
Repositorio Institucional Séneca |
collection |
Repositorio Institucional Séneca |
bitstream.url.fl_str_mv |
https://repositorio.uniandes.edu.co/bitstreams/f76bd8d3-4adb-48f2-be71-5f681e0becd2/download https://repositorio.uniandes.edu.co/bitstreams/710d3ccb-bbc3-4835-860f-62f1aae40744/download https://repositorio.uniandes.edu.co/bitstreams/6a2865a7-8821-418f-ad94-7ce0c4f3eb64/download |
bitstream.checksum.fl_str_mv |
6c898b38c29d9c3dc358e2b19554a6ff 3338def9387345986a528db1c16b16de 476100f10af7ec74669954b1ce254c3e |
bitstream.checksumAlgorithm.fl_str_mv |
MD5 MD5 MD5 |
repository.name.fl_str_mv |
Repositorio institucional Séneca |
repository.mail.fl_str_mv |
adminrepositorio@uniandes.edu.co |
_version_ |
1812133815694393344 |
spelling |
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_abf2Pearse, Jillian32e2a8f0-1189-487e-ab71-cda91515551a400Reyes Martínez, Daniela3b1294a-1905-4d16-83af-867ff5a1a2e6500Tary, Jean Baptiste2020-06-10T16:33:05Z2020-06-10T16:33:05Z2017http://hdl.handle.net/1992/39803u807219.pdfinstname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/In this work, InSAR from the Socotra island using Sentinel 1A data from June to October of 2017 was elaborated using European Space Agency's SNAP. The results revealed that the island experienced general subsidence which is confirmed by the data of a GPS station from the Nevada Geodetic laboratory that also recorded continuous subsidence in the year 2010 in a period of 5 months. Unfortunately, this was the most recent recorded data. Since the island is located between three ridges (Sheba ridge to the north, Gulf of Aden ridge to the north west, and the Carlsbridge rift to the south east), uplift was expected and finding only subsidence was unforeseen. One cause for this subsidence is attributed to the formation of pull apart basins in strike-fault systems en echelon (Burg, 2017) which is supported by the reported presence of normal faults in the northeast of the island (Beydoun & Roy, 1969; Fournier, Huchon, Khanbari, & Leroy, 2007). However, this mechanism only explains the subsidence in the west block; one of the two similar sized blocks that form the whole island according to various studies (Fournier, Huchon, Khanbari, & Leroy, 2007) separated by the Haddiboh transform zone. A probable cause for this subsidence may be the activity of scars from past continental collisions that lie deep in the crust and that control topography (Heron, Pysklywec, & Stephenson, 2016), however with InSAR it is impossible to determine where are these structures and to prove their existence more geophysical surveys are needed to examine the crust's structure there"En este trabajo se realizó InSAR usando el software y datos de la Agencia Espacial Europea de la isla Socotra, Yemen, usando imágenes de la misión Sentinel 1A desde junio hasta octubre del 2017. Los resultados revelan que durante este periodo de 5 meses la isla experimentó en promedio una subsidencia de -1cm, lo que es soportado por datos de una estación GPS del Laboratorio de Geodesia de Nevada que en 2010 registro subsidencia continua para un periodo también de 5 meses. Desafortunadamente no se encuentran datos más recientes. Como la isla está ubicada en medio de 3 dorsales oceánicas (Sheba al norte, La del Golfo de Aden al noroeste y la Carlsbridge al sureste) se esperaba lograr medir algún levantamiento y la subsidencia resulto ser imprevista. Una causa para esta subsidencia se le atribuyó a la formación de cuencas transextensionales en medio de fallas de rumbo en echelon (Burg, 2017) lo que es soportado por el reporte de fallas normales en el noroeste de la isla (Beydoun & Roy, 1969) (Fournier, Huchon, Khanbari, & Leroy, 2007). Sin embargo, este mecanismo solo explica la subsidencia en el bloque del oeste; uno de los dos bloques de similar tamaño que conforman toda la isla según varios estudios (Fournier, Huchon, Khanbari, & Leroy, 2007) separados por la zona transformante de Hadibboh. Se cree que una causa probable para la subsidencia en el bloque este de la isla sea la presencia de cicatrices por colisiones continentales que yacen profundo en la corteza y que controlan la topografía (Heron, Pysklywec, & Stephenson, 2016), sin embargo, con InSAR resulta imposible determinar dónde están estas estructuras y para probar su existencia seguramente hacen falta más estudios geofísicos en la región para determinar la estructura de la corteza ahí."--Tomado del Formato de Documento de GradoGeocientíficoPregrado38 hojasapplication/pdfspaUniandesGeocienciasFacultad de CienciasDepartamento de Geocienciasinstname:Universidad de los Andesreponame:Repositorio Institucional SénecaInSAR from the Socotra Island from June to October 2017Trabajo 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/TPSubsidencias (Geología)Movimientos tectónicosSensores remotosRadar de apertura sintéticaGeocienciasPublicationORIGINALu807219.pdfapplication/pdf2669036https://repositorio.uniandes.edu.co/bitstreams/f76bd8d3-4adb-48f2-be71-5f681e0becd2/download6c898b38c29d9c3dc358e2b19554a6ffMD51TEXTu807219.pdf.txtu807219.pdf.txtExtracted texttext/plain42439https://repositorio.uniandes.edu.co/bitstreams/710d3ccb-bbc3-4835-860f-62f1aae40744/download3338def9387345986a528db1c16b16deMD54THUMBNAILu807219.pdf.jpgu807219.pdf.jpgIM Thumbnailimage/jpeg4770https://repositorio.uniandes.edu.co/bitstreams/6a2865a7-8821-418f-ad94-7ce0c4f3eb64/download476100f10af7ec74669954b1ce254c3eMD551992/39803oai:repositorio.uniandes.edu.co:1992/398032023-10-10 15:28:05.527http://creativecommons.org/licenses/by-nc-sa/4.0/open.accesshttps://repositorio.uniandes.edu.coRepositorio institucional Sénecaadminrepositorio@uniandes.edu.co |