New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna

In the southern border of Laguna de Pozuelos Basin, the Pan de Azúcar volcanic complex crops out. It consists of several dacitic volcanic dome centers of ~ 12 Ma. Previous interpretation of seismic lines and a detailed ground magnetic survey indicated the presence of buried intrusive bodies. The det...

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Autor principal: Prezzi, Claudia Beatriz
Publicado: 2010
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v66_n1-2_p282_Prezzi
http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p282_Prezzi
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spelling paper:paper_00044822_v66_n1-2_p282_Prezzi2023-06-08T14:26:23Z New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna Prezzi, Claudia Beatriz Caldera system Gravity and magnetic anomalies Middle Miocene Northern Puna Bouguer anomaly caldera dacite dome gravity anomaly magnetic anomaly magnetic survey Miocene Argentina Jujuy Pozuelos Lake Puna In the southern border of Laguna de Pozuelos Basin, the Pan de Azúcar volcanic complex crops out. It consists of several dacitic volcanic dome centers of ~ 12 Ma. Previous interpretation of seismic lines and a detailed ground magnetic survey indicated the presence of buried intrusive bodies. The determination of the existence of buried bodies has two major implications: 1) these volcanic complexes are closely associated with ore deposits (as part of the Bolivian tin ore polymetallic belt); and 2) the existence of a large ancient caldera (~12 Ma) beneath the central and southern part of the Laguna de Pozuelos Basin, covered by the infilling sediments was previously suggested. The volcanic complexes would represent the final stages of such a calderic magmatic system. In order to confirm the existence of other buried intrusives and/or a buried caldera system, detailed ground magnetic and gravity surveys were carried out. The magnetic map is dominated by positive and negative anomalies in the southern sector of the basin, associated with the dacitic domes. The residual Bouguer anomaly presents a semicircular pattern, having only positive values. We applied the curvature technique to analyse the magnetic and gravity signals and used Euler deconvolution to estimate the depth to the sources. Our results would support the hypothesis of a large caldera buried beneath the Laguna de Pozuelos Basin. The identification of such a large Middle Miocene caldera would bring new insight into the magmatic evolution of the northern Puna. Fil:Prezzi, C.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2010 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v66_n1-2_p282_Prezzi http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p282_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 Caldera system
Gravity and magnetic anomalies
Middle Miocene
Northern Puna
Bouguer anomaly
caldera
dacite
dome
gravity anomaly
magnetic anomaly
magnetic survey
Miocene
Argentina
Jujuy
Pozuelos Lake
Puna
spellingShingle Caldera system
Gravity and magnetic anomalies
Middle Miocene
Northern Puna
Bouguer anomaly
caldera
dacite
dome
gravity anomaly
magnetic anomaly
magnetic survey
Miocene
Argentina
Jujuy
Pozuelos Lake
Puna
Prezzi, Claudia Beatriz
New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna
topic_facet Caldera system
Gravity and magnetic anomalies
Middle Miocene
Northern Puna
Bouguer anomaly
caldera
dacite
dome
gravity anomaly
magnetic anomaly
magnetic survey
Miocene
Argentina
Jujuy
Pozuelos Lake
Puna
description In the southern border of Laguna de Pozuelos Basin, the Pan de Azúcar volcanic complex crops out. It consists of several dacitic volcanic dome centers of ~ 12 Ma. Previous interpretation of seismic lines and a detailed ground magnetic survey indicated the presence of buried intrusive bodies. The determination of the existence of buried bodies has two major implications: 1) these volcanic complexes are closely associated with ore deposits (as part of the Bolivian tin ore polymetallic belt); and 2) the existence of a large ancient caldera (~12 Ma) beneath the central and southern part of the Laguna de Pozuelos Basin, covered by the infilling sediments was previously suggested. The volcanic complexes would represent the final stages of such a calderic magmatic system. In order to confirm the existence of other buried intrusives and/or a buried caldera system, detailed ground magnetic and gravity surveys were carried out. The magnetic map is dominated by positive and negative anomalies in the southern sector of the basin, associated with the dacitic domes. The residual Bouguer anomaly presents a semicircular pattern, having only positive values. We applied the curvature technique to analyse the magnetic and gravity signals and used Euler deconvolution to estimate the depth to the sources. Our results would support the hypothesis of a large caldera buried beneath the Laguna de Pozuelos Basin. The identification of such a large Middle Miocene caldera would bring new insight into the magmatic evolution of the northern Puna.
author Prezzi, Claudia Beatriz
author_facet Prezzi, Claudia Beatriz
author_sort Prezzi, Claudia Beatriz
title New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna
title_short New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna
title_full New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna
title_fullStr New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna
title_full_unstemmed New geophysical evidences of the presence of a buried caldera in Laguna Pozuelos, Northern Puna
title_sort new geophysical evidences of the presence of a buried caldera in laguna pozuelos, northern puna
publishDate 2010
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v66_n1-2_p282_Prezzi
http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p282_Prezzi
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