Articles | Volume 12, issue 1
https://doi.org/10.5194/se-12-253-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-12-253-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The Piuquencillo fault system: a long-lived, Andean-transverse fault system and its relationship with magmatic and hydrothermal activity
José Piquer
CORRESPONDING AUTHOR
Instituto de Ciencias de la Tierra, Universidad Austral de Chile,
Valdivia, 5090000, Chile
Orlando Rivera
Minera Peñoles de Chile, Santiago, 8320000, Chile
Gonzalo Yáñez
Departamento de Ingeniería Estructural y Geotécnica,
Pontificia Universidad Católica de Chile, Santiago, 8320000, Chile
Núcleo Milenio Trazadores de Metales (NMTM), Santiago, 8320000,
Chile
Nicolás Oyarzún
Instituto de Ciencias de la Tierra, Universidad Austral de Chile,
Valdivia, 5090000, Chile
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17 citations as recorded by crossref.
- Oligocene to Miocene magmatic and hydrothermal evolution in the Maricunga belt (Región de Copiapó, Chile): A new look to a long known metallogenic belt S. Gamonal et al. 10.1016/j.jsames.2024.104901
- A Model for the Lithospheric Architecture of the Central Andes and the Localization of Giant Porphyry Copper Deposit Clusters A. Farrar et al. 10.5382/econgeo.5010
- Anatomy of a high-silica eruption as observed by a local seismic network: the June 2011 Puyehue–Cordón Caulle event (southern Andes, Chile) D. Basualto et al. 10.5194/se-14-69-2023
- Deciphering groundwater flow-paths in fault-controlled semiarid mountain front zones (Central Chile) R. Figueroa et al. 10.1016/j.scitotenv.2021.145456
- Local controls on magma fertility in the Mio-Pliocene metallogenic belt of central Chile: Exploration implications J. Piquer et al. 10.1016/j.jsames.2024.104782
- Kinematics of the Clarke River Shear Zone (northeastern Australia) and implications for the tectonic evolution of the Tasmanides R. Rodrigues et al. 10.1080/08120099.2024.2339391
- Opposite rotations in the Central Andes Bend: Tectonic scenario compared to other cases of opposite rotations and implications for long-term subduction at continental arcs A. Martin 10.1016/j.jsames.2023.104698
- Evolution of the Azufre volcano (northern Chile): Implications for the Cerro Pabellón Geothermal Field as inferred from long lasting eruptive activity B. Godoy et al. 10.1016/j.jvolgeores.2022.107472
- Cryptic trans-lithospheric fault systems at the western margin of South America: implications for the formation and localization of gold-rich deposit superclusters D. Wiemer et al. 10.3389/feart.2023.1159430
- Selective reactivation of inherited fault zones driven by stress field changes: Insights from structural and paleostress analysis of the Pocuro Fault Zone, Southern Central Andes (32.8°S) M. Taucare et al. 10.1016/j.jsames.2022.103914
- The role of intra-arc strike-slip fault systems on landslide generation at Curarrehue (Central Southern Chilean Andes) D. Basualto et al. 10.1016/j.jsames.2023.104752
- PORPHYRY COPPER RECURRENCE IN THE ANDES OF CHILE AND ARGENTINA R. Sillitoe & J. Perelló 10.5382/econgeo.5092
- Unravelling geological controls on groundwater flow and surface water-groundwater interaction in mountain systems: A multi-disciplinary approach E. Marti et al. 10.1016/j.jhydrol.2023.129786
- Rainfall-Induced Landslide Assessment under Different Precipitation Thresholds Using Remote Sensing Data: A Central Andes Case G. Maragaño-Carmona et al. 10.3390/w15142514
- One decade of b-value variations from volcano-tectonic seismicity as an early indicator of episodes of crisis in a volcano: the case of Copahue, Southern Andes C. Farías et al. 10.3389/feart.2023.1181177
- The influence of variations in crustal composition and lithospheric strength on the evolution of deformation processes in the southern Central Andes: insights from geodynamic models M. Barrionuevo et al. 10.1007/s00531-021-01982-5
- Shallow anatomy of hydrothermal systems controlled by the Liquiñe-Ofqui Fault System and the Andean Transverse Faults: Geophysical imaging of fluid pathways and practical implications for geothermal exploration N. Pérez-Estay et al. 10.1016/j.geothermics.2022.102435
15 citations as recorded by crossref.
- Oligocene to Miocene magmatic and hydrothermal evolution in the Maricunga belt (Región de Copiapó, Chile): A new look to a long known metallogenic belt S. Gamonal et al. 10.1016/j.jsames.2024.104901
- A Model for the Lithospheric Architecture of the Central Andes and the Localization of Giant Porphyry Copper Deposit Clusters A. Farrar et al. 10.5382/econgeo.5010
- Anatomy of a high-silica eruption as observed by a local seismic network: the June 2011 Puyehue–Cordón Caulle event (southern Andes, Chile) D. Basualto et al. 10.5194/se-14-69-2023
- Deciphering groundwater flow-paths in fault-controlled semiarid mountain front zones (Central Chile) R. Figueroa et al. 10.1016/j.scitotenv.2021.145456
- Local controls on magma fertility in the Mio-Pliocene metallogenic belt of central Chile: Exploration implications J. Piquer et al. 10.1016/j.jsames.2024.104782
- Kinematics of the Clarke River Shear Zone (northeastern Australia) and implications for the tectonic evolution of the Tasmanides R. Rodrigues et al. 10.1080/08120099.2024.2339391
- Opposite rotations in the Central Andes Bend: Tectonic scenario compared to other cases of opposite rotations and implications for long-term subduction at continental arcs A. Martin 10.1016/j.jsames.2023.104698
- Evolution of the Azufre volcano (northern Chile): Implications for the Cerro Pabellón Geothermal Field as inferred from long lasting eruptive activity B. Godoy et al. 10.1016/j.jvolgeores.2022.107472
- Cryptic trans-lithospheric fault systems at the western margin of South America: implications for the formation and localization of gold-rich deposit superclusters D. Wiemer et al. 10.3389/feart.2023.1159430
- Selective reactivation of inherited fault zones driven by stress field changes: Insights from structural and paleostress analysis of the Pocuro Fault Zone, Southern Central Andes (32.8°S) M. Taucare et al. 10.1016/j.jsames.2022.103914
- The role of intra-arc strike-slip fault systems on landslide generation at Curarrehue (Central Southern Chilean Andes) D. Basualto et al. 10.1016/j.jsames.2023.104752
- PORPHYRY COPPER RECURRENCE IN THE ANDES OF CHILE AND ARGENTINA R. Sillitoe & J. Perelló 10.5382/econgeo.5092
- Unravelling geological controls on groundwater flow and surface water-groundwater interaction in mountain systems: A multi-disciplinary approach E. Marti et al. 10.1016/j.jhydrol.2023.129786
- Rainfall-Induced Landslide Assessment under Different Precipitation Thresholds Using Remote Sensing Data: A Central Andes Case G. Maragaño-Carmona et al. 10.3390/w15142514
- One decade of b-value variations from volcano-tectonic seismicity as an early indicator of episodes of crisis in a volcano: the case of Copahue, Southern Andes C. Farías et al. 10.3389/feart.2023.1181177
2 citations as recorded by crossref.
- The influence of variations in crustal composition and lithospheric strength on the evolution of deformation processes in the southern Central Andes: insights from geodynamic models M. Barrionuevo et al. 10.1007/s00531-021-01982-5
- Shallow anatomy of hydrothermal systems controlled by the Liquiñe-Ofqui Fault System and the Andean Transverse Faults: Geophysical imaging of fluid pathways and practical implications for geothermal exploration N. Pérez-Estay et al. 10.1016/j.geothermics.2022.102435
Latest update: 06 Nov 2024
Short summary
A proper recognition of deep, long-lived fault systems is very important for society. They can produce potentially dangerous earthquakes. They can also act as pathways for magmas and hydrothermal fluids, leading to the formation of volcanoes, geothermal systems and mineral deposits. However, the manifestations of these very old faults in the present-day surface can be very subtle. Here, we present a detailed, multi-disciplinary study of a fault system of this type in the Andes of central Chile.
A proper recognition of deep, long-lived fault systems is very important for society. They can...