Lithospheric structure of the Central Andes based on a 3D gravimetric model
We developed a 3D density model of the conti nental crust, the subducted plate and the upper mantle of the Central Andes between 20-29°S and 74-61°W through the forward modelling of Bouguer anomaly. The goal of this contribution is to gain insight on the lithospheric structure of the area, integrati...
Guardado en:
Autores principales: | , |
---|---|
Formato: | JOUR |
Materias: | |
Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00044822_v65_n1_p81_Prezzi |
Aporte de: |
id |
todo:paper_00044822_v65_n1_p81_Prezzi |
---|---|
record_format |
dspace |
spelling |
todo:paper_00044822_v65_n1_p81_Prezzi2023-10-03T13:58:33Z Lithospheric structure of the Central Andes based on a 3D gravimetric model Prezzi, C.B. Götze, H.-J. Central Andes Convergent continental margins Gavity anomalies Lithospheric structure Bouguer anomaly continental crust continental margin convergent margin forward modeling gravimetry lithospheric structure Moho three-dimensional modeling Andes We developed a 3D density model of the conti nental crust, the subducted plate and the upper mantle of the Central Andes between 20-29°S and 74-61°W through the forward modelling of Bouguer anomaly. The goal of this contribution is to gain insight on the lithospheric structure of the area, integrating the available information (geophysical, geologic, petrologic, and geochemical) in a single model. The geometry of our model is defined and constrained by hypocenters location, reflection and refraction seismic lines, travel time and attenuation tomography, receiver function analysis, magnetotelluric studies, thermal models and structural cross sections. The densities allocated to the different bodies were calculated considering petrologic and geochemical data and pressure and temperature conditions. The model consists of 31 parallel E-W vertical planes, where the continental crust comprises distinct bodies, which represent the different morphotectonic units of the Central Andes. Contour maps of the depth to the top of the subducted plate, the depth of the continental Moho and the depth to the top of the asthenosphere below South America were produced. The residual anomaly was calculated by subtracting from the Bouguer anomaly the gravimetric effect of the modelled subducted slab and of the modelled Moho. This study demonstrates how 3D gravity modelling, integrating geophysical, geologic and petrologic information, can help to reveal the lithospheric structure of the Central Andes. Fil:Prezzi, C.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v65_n1_p81_Prezzi |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Central Andes Convergent continental margins Gavity anomalies Lithospheric structure Bouguer anomaly continental crust continental margin convergent margin forward modeling gravimetry lithospheric structure Moho three-dimensional modeling Andes |
spellingShingle |
Central Andes Convergent continental margins Gavity anomalies Lithospheric structure Bouguer anomaly continental crust continental margin convergent margin forward modeling gravimetry lithospheric structure Moho three-dimensional modeling Andes Prezzi, C.B. Götze, H.-J. Lithospheric structure of the Central Andes based on a 3D gravimetric model |
topic_facet |
Central Andes Convergent continental margins Gavity anomalies Lithospheric structure Bouguer anomaly continental crust continental margin convergent margin forward modeling gravimetry lithospheric structure Moho three-dimensional modeling Andes |
description |
We developed a 3D density model of the conti nental crust, the subducted plate and the upper mantle of the Central Andes between 20-29°S and 74-61°W through the forward modelling of Bouguer anomaly. The goal of this contribution is to gain insight on the lithospheric structure of the area, integrating the available information (geophysical, geologic, petrologic, and geochemical) in a single model. The geometry of our model is defined and constrained by hypocenters location, reflection and refraction seismic lines, travel time and attenuation tomography, receiver function analysis, magnetotelluric studies, thermal models and structural cross sections. The densities allocated to the different bodies were calculated considering petrologic and geochemical data and pressure and temperature conditions. The model consists of 31 parallel E-W vertical planes, where the continental crust comprises distinct bodies, which represent the different morphotectonic units of the Central Andes. Contour maps of the depth to the top of the subducted plate, the depth of the continental Moho and the depth to the top of the asthenosphere below South America were produced. The residual anomaly was calculated by subtracting from the Bouguer anomaly the gravimetric effect of the modelled subducted slab and of the modelled Moho. This study demonstrates how 3D gravity modelling, integrating geophysical, geologic and petrologic information, can help to reveal the lithospheric structure of the Central Andes. |
format |
JOUR |
author |
Prezzi, C.B. Götze, H.-J. |
author_facet |
Prezzi, C.B. Götze, H.-J. |
author_sort |
Prezzi, C.B. |
title |
Lithospheric structure of the Central Andes based on a 3D gravimetric model |
title_short |
Lithospheric structure of the Central Andes based on a 3D gravimetric model |
title_full |
Lithospheric structure of the Central Andes based on a 3D gravimetric model |
title_fullStr |
Lithospheric structure of the Central Andes based on a 3D gravimetric model |
title_full_unstemmed |
Lithospheric structure of the Central Andes based on a 3D gravimetric model |
title_sort |
lithospheric structure of the central andes based on a 3d gravimetric model |
url |
http://hdl.handle.net/20.500.12110/paper_00044822_v65_n1_p81_Prezzi |
work_keys_str_mv |
AT prezzicb lithosphericstructureofthecentralandesbasedona3dgravimetricmodel AT gotzehj lithosphericstructureofthecentralandesbasedona3dgravimetricmodel |
_version_ |
1807314938110148608 |