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dc.contributor.author
Gutierrez, Cecilia Inés  
dc.contributor.author
Plotek, Berenice Lia  
dc.contributor.author
Likerman, Jeremias  
dc.contributor.author
Cristallini, Ernesto Osvaldo  
dc.date.available
2025-01-31T15:05:25Z  
dc.date.issued
2024  
dc.identifier.citation
Analog Models and Trishear Kinematics: A Sandbox Experiment; American Geophysical Union 2024 meeting; Washington; Estados Unidos; 2024; 1-2  
dc.identifier.uri
http://hdl.handle.net/11336/253424  
dc.description.abstract
Numerous studies have focused on comparing the kinematics of fault-propagation folds using numerical models, yet there is a scarcity of research directly comparing these features with velocity fields obtained from analog models. This study aims to bridge that gap by conducting laboratory experiments specifically designed to simulate fault-propagation folds.Sandbox experiments are a commonly used experimental approach in geology to investigate geological processes. These models generally emphasize geometry and kinematics while attempting to simulate natural prototypes. In this research, we focused on the kinematics involved in the formation of a simple fault-propagation fold composed of a single reverse fault.To simulate the development of this thrust, we used a rigid plastic sheet inside an acrylic box with a moving wall filled with sand. The kinematic field was obtained by applying particle image velocimetry (PIVlab), and the resulting vectors were compared with those proposed by the theoretical trishear model. The data collected from the analog models aligned well with the theoretical framework.The observed translations and rotations across the phases of the experiment corroborate the proposed kinematics. There are two main rotations in the kinematic field. The first consists of horizontal vectors rotating counterclockwise until they become parallel to the reverse fault, occurring from the backlimb and in the hanging block of the main fault. The second rotation, of smaller magnitude, occurs exclusively in the frontal sector close to the tip. The vectors that were parallel to the fault begin a new clockwise rotation, tending to zero around the footwall block.To compare the stages of the analog model with the trishear method, the apical angle was tested at intervals of 5°, ranging from 10° to 100°. The difference between the velocity field of the analog model and the theoretical trishear model was calculated to determine the trishear apical angle that best approximates the analog kinematic field in the experiment. Subsequently, the angular differences between the trishear method and the analog experiment were computed after scaling the vectors. The best approximation was obtained with an angle of 30°.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
American Geophysical Union  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Kinematics  
dc.subject
Numerical model  
dc.subject
Fault-propagation  
dc.subject
Folds  
dc.subject.classification
Geología  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
Analog Models and Trishear Kinematics: A Sandbox Experiment  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.type
info:eu-repo/semantics/conferenceObject  
dc.type
info:ar-repo/semantics/documento de conferencia  
dc.date.updated
2024-11-26T14:39:57Z  
dc.journal.pagination
1-2  
dc.journal.pais
Estados Unidos  
dc.journal.ciudad
Washington  
dc.description.fil
Fil: Gutierrez, Cecilia Inés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional del Sur; Argentina  
dc.description.fil
Fil: Plotek, Berenice Lia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
dc.description.fil
Fil: Likerman, Jeremias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
dc.description.fil
Fil: Cristallini, Ernesto Osvaldo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1732568  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.agu.org/annual-meeting  
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Autor  
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Autor  
dc.conicet.rol
Autor  
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Autor  
dc.coverage
Internacional  
dc.type.subtype
Reunión  
dc.description.nombreEvento
American Geophysical Union 2024 meeting  
dc.date.evento
2024-12-09  
dc.description.ciudadEvento
Washington  
dc.description.paisEvento
Estados Unidos  
dc.type.publicacion
Book  
dc.description.institucionOrganizadora
American Geophysical Union  
dc.source.libro
American Geophysical Union (AGU) 2024 meeting  
dc.date.eventoHasta
2024-12-13  
dc.type
Reunión