Stratigraphic architecture of alluvial terraces in the Yunganza river

The study of fluvial sedimentation patterns (FSP) allow us to analyze tectonic and climatic behavior in a specific region, and, understand how rivers modify the relief. FSP can be studied from the analysis of the stratigraphic record of their deposits. In the northern Andes, FSP interact with erosio...

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Autor Principal: Romero, Cristian (author)
Outros autores: Cisneros Medina, Andrea (author), Condoy Guiracocha, Darwin (author), Carranco Andino, Fausto (author), Gramal Aguilar, Ana Belén (author), Betancourt Valdivieso, Franz (author)
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Idioma:spa
Publicado: 2020
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Acceso en liña:https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482
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author Romero, Cristian
author2 Cisneros Medina, Andrea
Condoy Guiracocha, Darwin
Carranco Andino, Fausto
Gramal Aguilar, Ana Belén
Betancourt Valdivieso, Franz
author2_role author
author
author
author
author
author_facet Romero, Cristian
Cisneros Medina, Andrea
Condoy Guiracocha, Darwin
Carranco Andino, Fausto
Gramal Aguilar, Ana Belén
Betancourt Valdivieso, Franz
author_role author
collection Revista FIGEMPA: Investigación y Desarrollo
dc.creator.none.fl_str_mv Romero, Cristian
Cisneros Medina, Andrea
Condoy Guiracocha, Darwin
Carranco Andino, Fausto
Gramal Aguilar, Ana Belén
Betancourt Valdivieso, Franz
dc.date.none.fl_str_mv 2020-12-31
dc.format.none.fl_str_mv application/pdf
text/xml
application/zip
dc.identifier.none.fl_str_mv https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482
10.29166/revfig.v1i2.2482
dc.language.none.fl_str_mv spa
dc.publisher.none.fl_str_mv Facultad de Ingeniería en Geología, Minas, Petróleos y Ambiental - Universidad Central del Ecuador
dc.relation.none.fl_str_mv https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482/3587
https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482/4959
https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482/3924
dc.rights.none.fl_str_mv http://creativecommons.org/licenses/by-nc/4.0
info:eu-repo/semantics/openAccess
dc.source.none.fl_str_mv FIGEMPA: Investigación y Desarrollo; Vol. 10 No. 2 (2020): Natural resources and pandemic; 61-71
FIGEMPA: Investigación y Desarrollo; Vol. 10 Núm. 2 (2020): Recursos naturales y pandemia; 61-71
2602-8484
1390-7042
10.29166/revfig.v1i2
reponame:Revista FIGEMPA: Investigación y Desarrollo
instname:Universidad Central del Ecuador
instacron:UCE
dc.subject.none.fl_str_mv Terrazas aluviales
Sedimentología fluvial
rio Yunganza
Alluvial terraces
Fluvial sedimentology
Yunganza river
dc.title.none.fl_str_mv Stratigraphic architecture of alluvial terraces in the Yunganza river
Arquitectura estratigráfica de terrazas aluviales en el río Yunganza
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
description The study of fluvial sedimentation patterns (FSP) allow us to analyze tectonic and climatic behavior in a specific region, and, understand how rivers modify the relief. FSP can be studied from the analysis of the stratigraphic record of their deposits. In the northern Andes, FSP interact with erosion rates and detritus available for sedimentation rates. In the south of the sub-Andean zone, the Yunganza river basin corresponds to a confined fluvial basin and feeder of the Santiago river, and offers the opportunity to study this region FSP. The aim of this research is to present the stratigraphic record analysis of: ancient alluvial terraces (TA-1 and TA-2) and alluvial deposits (DA) in the Yunganza river basin, in the vicinity of El Rosario in order to define PSF. Our research is supported by documentation of the lithological record, sedimentary structures, stratigraphic architecture, thickness and paleo-currents measurement. Seven facies are described: LT-1 and LT-2 describe conglomerates associated with distal debris flows, whilst, LT-3 describes conglomerates and breccias associated with proximal debris flows. LT-4, and LT-5, and LT-6 describe sandstones genetically linked to bars and fluvial channel macro-forms, last, LT-7 describes siltstones associated with flood plains. Paleocurrent data indicate that: TA-1 presents flow direction to NE-E, whereas, TA-2 indicates a sediment transport direction to N. The TA-1 modal composition indicates a detrital provenance of a sedimentary block rich in quarts, while the TA-2 modal composition indicates a recycling period of TA-1. The thickness measurement in TA-1 and TA-2 indicates an intensely erosive period in TA-1. Finally, fluvial sedimentation patterns in the Yunganza river are genetically linked to periods of exhumation on the west side of the river.
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network_acronym_str REVFIGEMPA
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publishDate 2020
publisher.none.fl_str_mv Facultad de Ingeniería en Geología, Minas, Petróleos y Ambiental - Universidad Central del Ecuador
reponame_str Revista FIGEMPA: Investigación y Desarrollo
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repository.name.fl_str_mv Revista FIGEMPA: Investigación y Desarrollo - Universidad Central del Ecuador
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spelling Stratigraphic architecture of alluvial terraces in the Yunganza riverArquitectura estratigráfica de terrazas aluviales en el río YunganzaRomero, CristianCisneros Medina, AndreaCondoy Guiracocha, DarwinCarranco Andino, FaustoGramal Aguilar, Ana BelénBetancourt Valdivieso, FranzTerrazas aluvialesSedimentología fluvialrio YunganzaAlluvial terracesFluvial sedimentologyYunganza riverThe study of fluvial sedimentation patterns (FSP) allow us to analyze tectonic and climatic behavior in a specific region, and, understand how rivers modify the relief. FSP can be studied from the analysis of the stratigraphic record of their deposits. In the northern Andes, FSP interact with erosion rates and detritus available for sedimentation rates. In the south of the sub-Andean zone, the Yunganza river basin corresponds to a confined fluvial basin and feeder of the Santiago river, and offers the opportunity to study this region FSP. The aim of this research is to present the stratigraphic record analysis of: ancient alluvial terraces (TA-1 and TA-2) and alluvial deposits (DA) in the Yunganza river basin, in the vicinity of El Rosario in order to define PSF. Our research is supported by documentation of the lithological record, sedimentary structures, stratigraphic architecture, thickness and paleo-currents measurement. Seven facies are described: LT-1 and LT-2 describe conglomerates associated with distal debris flows, whilst, LT-3 describes conglomerates and breccias associated with proximal debris flows. LT-4, and LT-5, and LT-6 describe sandstones genetically linked to bars and fluvial channel macro-forms, last, LT-7 describes siltstones associated with flood plains. Paleocurrent data indicate that: TA-1 presents flow direction to NE-E, whereas, TA-2 indicates a sediment transport direction to N. The TA-1 modal composition indicates a detrital provenance of a sedimentary block rich in quarts, while the TA-2 modal composition indicates a recycling period of TA-1. The thickness measurement in TA-1 and TA-2 indicates an intensely erosive period in TA-1. Finally, fluvial sedimentation patterns in the Yunganza river are genetically linked to periods of exhumation on the west side of the river.El estudio de patrones de sedimentación fluvial (PSF) permite analizar el comportamiento tectónico y climático en una determinada región, además entender cómo los ríos modifican el relieve. Los PSF pueden ser estudiados a partir del análisis del registro estratigráfico de sus depósitos. En los Andes del norte, los PSF interactúan con tasas de erosión y generación de detrito disponible para la sedimentación. En el sur, del levantamiento subandino ecuatoriano, la cuenca del río Yunganza es una cuenca fluvial confinada, alimentadora del río Santiago y ofrece la posibilidad de estudiar los PSF de esta región. El objetivo de esta investigación es presentar el análisis del registro estratigráfico de terrazas aluviales antiguas (TA-1 y TA-2) y depósitos aluviales modernos (DA), en la cuenca alta del río Yunganza, en el sector El Rosario, con el fin de definir PSF. Esta investigación es soportada por la documentación del registro litológico, las estructuras sedimentarias, la arquitectura estratigráfica, la medición de espesores y paleocorrientes. De esta manera, 7 facies son descritas: LT-1 y LT-2 describen a conglomerados asociados a flujos de escombros distales, mientras que LT-3 describe litologías de conglomerados y brechas asociadas a flujos de escombros proximales. LT-4, LT-5 y LT-6 describen litologías arenosas vinculadas genéticamente a macroformas de barras y canales fluviales; LT-7 describe litologías limosas que se asocian a planicies de inundación. Datos de paleocorrientes indican que: TA-1 presenta una dirección de flujo N-NE, mientras que TA-2 indican una dirección de transporte de sedimento hacia el N. La composición modal en TA-1 indica una procedencia detrítica de un bloque sedimentario rico en cuarzo, mientras que TA-2 indica un periodo de reciclaje de TA-1. La medición de espesores en TA-1 y TA-2 indica un periodo erosivo en TA-1. Finalmente, los patrones de sedimentación en el río Yunganza están vinculados genéticamente a periodos de exhumación del flanco oeste del río.Facultad de Ingeniería en Geología, Minas, Petróleos y Ambiental - Universidad Central del Ecuador2020-12-31info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdftext/xmlapplication/ziphttps://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/248210.29166/revfig.v1i2.2482FIGEMPA: Investigación y Desarrollo; Vol. 10 No. 2 (2020): Natural resources and pandemic; 61-71FIGEMPA: Investigación y Desarrollo; Vol. 10 Núm. 2 (2020): Recursos naturales y pandemia; 61-712602-84841390-704210.29166/revfig.v1i2reponame:Revista FIGEMPA: Investigación y Desarrolloinstname:Universidad Central del Ecuadorinstacron:UCEspahttps://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482/3587https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482/4959https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482/3924Derechos de autor 2020 Cristian Romero, Andrea Cisneros Medina, Darwin Condoy Guiracocha, Fausto Carranco Andino, Ana Belén Gramal Aguilar, Franz Betancourt Valdiviesohttp://creativecommons.org/licenses/by-nc/4.0info:eu-repo/semantics/openAccess2023-04-20T13:43:40Zoai:revistadigital.uce.edu.ec:article/2482Portal de revistashttps://revistadigital.uce.edu.ec/Universidad públicahttps://uce.edu.ec/**Ecuador*602-84841390-7042opendoar:02023-04-20T13:43:40Revista FIGEMPA: Investigación y Desarrollo - Universidad Central del Ecuadorfalse
spellingShingle Stratigraphic architecture of alluvial terraces in the Yunganza river
Romero, Cristian
Terrazas aluviales
Sedimentología fluvial
rio Yunganza
Alluvial terraces
Fluvial sedimentology
Yunganza river
status_str publishedVersion
title Stratigraphic architecture of alluvial terraces in the Yunganza river
title_full Stratigraphic architecture of alluvial terraces in the Yunganza river
title_fullStr Stratigraphic architecture of alluvial terraces in the Yunganza river
title_full_unstemmed Stratigraphic architecture of alluvial terraces in the Yunganza river
title_short Stratigraphic architecture of alluvial terraces in the Yunganza river
title_sort Stratigraphic architecture of alluvial terraces in the Yunganza river
topic Terrazas aluviales
Sedimentología fluvial
rio Yunganza
Alluvial terraces
Fluvial sedimentology
Yunganza river
url https://revistadigital.uce.edu.ec/index.php/RevFIG/article/view/2482