- published: 07 Jun 2021
- views: 67
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Liquiñe-Ofqui Fault
The Liquiñe-Ofqui Fault is major geological fault that runs a length of roughly 1000 km in a north-south direction and exhibits current seismicity. It is located in the Chilean Northern Patagonian Andes. It is a dextral intra-arc transform fault. When considered a fault zone, the Liquiñe-Ofqui Fault Zone (LOFZ) might include other neighboring faults such as Reigolil-Pirihueico Fault.
As the name implies it runs from the Liquiñe Valley hot springs in the north to the Ofqui Isthmus in the south, where the Antarctic Plate meets the Nazca Plate and the South American Plate in Chile Triple Junction. A large part of the fault runs along the Moraleda Channel. North of Liquiñe the fault is gradually converted into a compression area. At Quetrupillán volcano the fault is crossed by the Gastre Fault Zone. It may be classified as a dextral intra-arc transform fault.
The fault name was coined by Francisco Hervé, I. Fuenzalida, E. Araya and A. Solano in 1979. The fault itself was first inferred by Chilean government agent Hans Steffen around 1900 who referred to it as a "tectonic furrow" (Spanish: surco tectónico).
This page contains text from Wikipedia, the Free Encyclopedia - https://wn.com/Liquiñe-Ofqui_Fault
Liquiñe
Liquiñe is a town in Liquiñe Valley, in Panguipulli commune, Valdivia Province, Chile. The area around the village is home to South America's densest collection of hot springs. There are literally hundred of sites where geothermal waters flow up out of the earth. The water emerges from the ground at roughly 176°F (80°C). Therefore, the water must be cooled before being fed into pools for bathing.
The Liquiñe Hot Springs feature geothermally-heated mineral water. Geologically it lies at the north end of the Liquiñe-Ofqui Fault.
The road to Carirriñe Pass goes through Liquiñe, allowing transit to and from Junín de los Andes in Argentina. However, this mountain pass is only open during the summer months of January and February.
See also
External links
This page contains text from Wikipedia, the Free Encyclopedia - https://wn.com/Liquiñe
Radio Stations - Liquiñe
SEARCH FOR RADIOS
Podcasts:
-
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System (LOFS) between 38°S and 40.5°S: Implications fo the Assessment of the Seismic Assessment.
published: 07 Jun 2021 -
Falla Liquiñe-Ofqui - Geparque Patagonia Verde
published: 13 Jun 2023 -
Falla tectónica Liquiñe
En Chile hay varias fallas tectónicas, esto se incrementó en algunos lugares por el terremoto de 9.5 ( grabado en el canal) en Valdivia. Lo que muestro hoy es una de las tantas y se llama .. Falla Liquiñe Ofqui. Enero 2024.
published: 08 Jan 2024 -
Biobío-Aluminé Fault Zone | Wikipedia audio article
This is an audio version of the Wikipedia Article: https://en.wikipedia.org/wiki/Biob%C3%ADo-Alumin%C3%A9_Fault_Zone Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago. Learning by listening is a great way to: - increases imagination and understanding - improves your listening skills - improves your own spoken accent - learn while on the move - reduce eye strain Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an ...
published: 07 Jun 2019 -
Liquiñe cascada
Cascada de liquiñe comuna de panguipulli
published: 13 Oct 2016 -
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault.
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault (Linares, Maule Region) Through a local seismic network.
published: 07 Jun 2021 -
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle.
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle: Unraveling the Liquiñe-Ofqui Fault System Case.
published: 07 Jun 2021 -
“Conversatorio nº1 en Beauchef 2021”, "Descubrimiento del Volcán Mate Grande, Patagonia Chilena"
La Escuela de Postgrado y Educación Continua EPEC, les invita a un nuevo ciclo de “Conversatorios en Beauchef 2021”, con la charla "Descubrimiento del Volcán Mate Grande a lo largo de la Zona de Fallas Liquiñe-Ofqui, Patagonia Chilena", del académico del Departamento de Geología Gregory De Pascale.
published: 29 Apr 2021 -
Jose Piquer - Fundamental basement faults, magmas and hydrothermal fluids
José Piquer is the Director of the Institute of Earth Sciences at Universidad Austral de Chile and he'll be coming by tomorrow to chat about fundamental basement faults, magmas and hydrothermal fluids with recent advances from the Andes. Several authors have recognized the relevant role played by fundamental basement faults in controlling the distribution and geometry of magmatic-hydrothermal systems. The talk begins with a discussion about the concept of fundamental basement fault, its relevance for mineral exploration and the difficulties involved in properly recognizing them, particularly in active orogenic systems. This is followed by a presentation of recent advances in the study of fundamental basement faults in the Andes of Chile and Argentina, with an emphasis on studies based on...
published: 31 Aug 2021 -
Charla 1 GeoCharlas T3 - Miguel Sáez
En la primera charla de nuestro ciclo GeoCharlas T3, el candidado a Doctor, Miguel Sáez del Departamento de Geofísica de la Universidad de Chile, nos trae la charla: Terremotos lentos en Chile, ¿cómo, dónde y cuándo? (Slow earthquakes in Chile, how, where and when?) En esta charla, Miguel resume el estado del arte del estudio de terremotos lentos en el mundo, su reciente descubrimiento, su generación y ocurrencia en diferentes ambientes tectónicos. Acotando el área de estudio nos muestra las diferentes señales sísmicas y geodésicas observadas a lo largo de Chile. En particular nos comparte sus recientes estudios de tremors no volcánicos en el Punto Triple chileno y sismicidad lenta asociada a la falla Liquiñe-Ofqui, en la región de Aysén.
published: 07 May 2020
5:49
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System
- Order: Reorder
- Duration: 5:49
- Uploaded Date: 07 Jun 2021
- views: 67
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System (LOFS) between 38°S and 40.5°S: Implications fo the Assessment of t...
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System (LOFS) between 38°S and 40.5°S: Implications fo the Assessment of the Seismic Assessment.
https://wn.com/Luis_Astudillo_Sotomayor_Research_Line_Rl3_Neotectonics_Of_The_Liquiñe_Ofqui_Fault_System
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System (LOFS) between 38°S and 40.5°S: Implications fo the Assessment of the Seismic Assessment.
0:20
Falla Liquiñe-Ofqui - Geparque Patagonia Verde
- Order: Reorder
- Duration: 0:20
- Uploaded Date: 13 Jun 2023
- views: 200
- published: 13 Jun 2023
- views: 200
0:15
Falla tectónica Liquiñe
- Order: Reorder
- Duration: 0:15
- Uploaded Date: 08 Jan 2024
- views: 2513
En Chile hay varias fallas tectónicas, esto se incrementó en algunos lugares por el terremoto de 9.5 ( grabado en el canal) en Valdivia.
Lo que muestro hoy es u...
En Chile hay varias fallas tectónicas, esto se incrementó en algunos lugares por el terremoto de 9.5 ( grabado en el canal) en Valdivia.
Lo que muestro hoy es una de las tantas y se llama .. Falla Liquiñe Ofqui.
Enero 2024.
https://wn.com/Falla_Tectónica_Liquiñe
En Chile hay varias fallas tectónicas, esto se incrementó en algunos lugares por el terremoto de 9.5 ( grabado en el canal) en Valdivia.
Lo que muestro hoy es una de las tantas y se llama .. Falla Liquiñe Ofqui.
Enero 2024.
- published: 08 Jan 2024
- views: 2513
0:27
Biobío-Aluminé Fault Zone | Wikipedia audio article
- Order: Reorder
- Duration: 0:27
- Uploaded Date: 07 Jun 2019
- views: 3
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Biob%C3%ADo-Alumin%C3%A9_Fault_Zone
Listening is a more natural way...
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Biob%C3%ADo-Alumin%C3%A9_Fault_Zone
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
https://assistant.google.com/services/invoke/uid/0000001a130b3f91
Other Wikipedia audio articles at:
https://www.youtube.com/results?search_query=wikipedia+tts
Upload your own Wikipedia articles through:
https://github.com/nodef/wikipedia-tts
Speaking Rate: 0.9044353972429492
Voice name: en-GB-Wavenet-C
"I cannot teach anybody anything, I can only make them think."
- Socrates
SUMMARY
=======
The Biobío-Aluminé Fault Zone is a northwest-trending geological fault zone in south-central Chile and Argentina. The fault aligns with the middle-upper course of Bío Bío River where fault traces are largely covered with fluvial gravels. The northernmost reaches of the north-south Liquiñe-Ofqui Fault intersect and displace the Biobío-Aluminé Fault Zone.
https://wn.com/Biobío_Aluminé_Fault_Zone_|_Wikipedia_Audio_Article
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Biob%C3%ADo-Alumin%C3%A9_Fault_Zone
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
https://assistant.google.com/services/invoke/uid/0000001a130b3f91
Other Wikipedia audio articles at:
https://www.youtube.com/results?search_query=wikipedia+tts
Upload your own Wikipedia articles through:
https://github.com/nodef/wikipedia-tts
Speaking Rate: 0.9044353972429492
Voice name: en-GB-Wavenet-C
"I cannot teach anybody anything, I can only make them think."
- Socrates
SUMMARY
=======
The Biobío-Aluminé Fault Zone is a northwest-trending geological fault zone in south-central Chile and Argentina. The fault aligns with the middle-upper course of Bío Bío River where fault traces are largely covered with fluvial gravels. The northernmost reaches of the north-south Liquiñe-Ofqui Fault intersect and displace the Biobío-Aluminé Fault Zone.
- published: 07 Jun 2019
- views: 3
0:40
Liquiñe cascada
- Order: Reorder
- Duration: 0:40
- Uploaded Date: 13 Oct 2016
- views: 226
Cascada de liquiñe comuna de panguipulli
Cascada de liquiñe comuna de panguipulli
https://wn.com/Liquiñe_Cascada
Cascada de liquiñe comuna de panguipulli
- published: 13 Oct 2016
- views: 226
2:40
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault.
- Order: Reorder
- Duration: 2:40
- Uploaded Date: 07 Jun 2021
- views: 29
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault (Linares, Maule Region) Through a local seismic network.
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault (Linares, Maule Region) Through a local seismic network.
https://wn.com/Martín_Riedel_Research_Line_Rl3_Micro_Seismicity_Of_The_Mesamávida_Crustal_Fault.
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault (Linares, Maule Region) Through a local seismic network.
- published: 07 Jun 2021
- views: 29
5:49
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle.
- Order: Reorder
- Duration: 5:49
- Uploaded Date: 07 Jun 2021
- views: 46
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle: Unraveling the Liquiñe-Ofqui Fault System Case.
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle: Unraveling the Liquiñe-Ofqui Fault System Case.
https://wn.com/Joaquín_Julve_Research_Line_Rl2_5_Crustal_Fault_Dynamics_Through_The_Subduction_Seismic_Cycle.
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle: Unraveling the Liquiñe-Ofqui Fault System Case.
- published: 07 Jun 2021
- views: 46
1:13:20
“Conversatorio nº1 en Beauchef 2021”, "Descubrimiento del Volcán Mate Grande, Patagonia Chilena"
- Order: Reorder
- Duration: 1:13:20
- Uploaded Date: 29 Apr 2021
- views: 129
La Escuela de Postgrado y Educación Continua EPEC, les invita a un nuevo ciclo de “Conversatorios en Beauchef 2021”, con la charla "Descubrimiento del Volcán Ma...
La Escuela de Postgrado y Educación Continua EPEC, les invita a un nuevo ciclo de “Conversatorios en Beauchef 2021”, con la charla "Descubrimiento del Volcán Mate Grande a lo largo de la Zona de Fallas Liquiñe-Ofqui, Patagonia Chilena", del académico del Departamento de Geología Gregory De Pascale.
https://wn.com/“Conversatorio_Nº1_En_Beauchef_2021”,_Descubrimiento_Del_Volcán_Mate_Grande,_Patagonia_Chilena
La Escuela de Postgrado y Educación Continua EPEC, les invita a un nuevo ciclo de “Conversatorios en Beauchef 2021”, con la charla "Descubrimiento del Volcán Mate Grande a lo largo de la Zona de Fallas Liquiñe-Ofqui, Patagonia Chilena", del académico del Departamento de Geología Gregory De Pascale.
- published: 29 Apr 2021
- views: 129
52:47
Jose Piquer - Fundamental basement faults, magmas and hydrothermal fluids
- Order: Reorder
- Duration: 52:47
- Uploaded Date: 31 Aug 2021
- views: 1023
José Piquer is the Director of the Institute of Earth Sciences at Universidad Austral de Chile and he'll be coming by tomorrow to chat about fundamental basemen...
José Piquer is the Director of the Institute of Earth Sciences at Universidad Austral de Chile and he'll be coming by tomorrow to chat about fundamental basement faults, magmas and hydrothermal fluids with recent advances from the Andes.
Several authors have recognized the relevant role played by fundamental basement faults in controlling the distribution and geometry of magmatic-hydrothermal systems. The talk begins with a discussion about the concept of fundamental basement fault, its relevance for mineral exploration and the difficulties involved in properly recognizing them, particularly in active orogenic systems.
This is followed by a presentation of recent advances in the study of fundamental basement faults in the Andes of Chile and Argentina, with an emphasis on studies based on structural mapping, which illustrate the expressions of this type of long-lived fault systems in the field.
https://wn.com/Jose_Piquer_Fundamental_Basement_Faults,_Magmas_And_Hydrothermal_Fluids
José Piquer is the Director of the Institute of Earth Sciences at Universidad Austral de Chile and he'll be coming by tomorrow to chat about fundamental basement faults, magmas and hydrothermal fluids with recent advances from the Andes.
Several authors have recognized the relevant role played by fundamental basement faults in controlling the distribution and geometry of magmatic-hydrothermal systems. The talk begins with a discussion about the concept of fundamental basement fault, its relevance for mineral exploration and the difficulties involved in properly recognizing them, particularly in active orogenic systems.
This is followed by a presentation of recent advances in the study of fundamental basement faults in the Andes of Chile and Argentina, with an emphasis on studies based on structural mapping, which illustrate the expressions of this type of long-lived fault systems in the field.
- published: 31 Aug 2021
- views: 1023
1:06:02
Charla 1 GeoCharlas T3 - Miguel Sáez
- Order: Reorder
- Duration: 1:06:02
- Uploaded Date: 07 May 2020
- views: 1128
En la primera charla de nuestro ciclo GeoCharlas T3, el candidado a Doctor, Miguel Sáez del Departamento de Geofísica de la Universidad de Chile, nos trae la ch...
En la primera charla de nuestro ciclo GeoCharlas T3, el candidado a Doctor, Miguel Sáez del Departamento de Geofísica de la Universidad de Chile, nos trae la charla:
Terremotos lentos en Chile, ¿cómo, dónde y cuándo?
(Slow earthquakes in Chile, how, where and when?)
En esta charla, Miguel resume el estado del arte del estudio de terremotos lentos en el mundo, su reciente descubrimiento, su generación y ocurrencia en diferentes ambientes tectónicos.
Acotando el área de estudio nos muestra las diferentes señales sísmicas y geodésicas observadas a lo largo de Chile. En particular nos comparte sus recientes estudios de tremors no volcánicos en el Punto Triple chileno y sismicidad lenta asociada a la falla Liquiñe-Ofqui, en la región de Aysén.
https://wn.com/Charla_1_Geocharlas_T3_Miguel_Sáez
En la primera charla de nuestro ciclo GeoCharlas T3, el candidado a Doctor, Miguel Sáez del Departamento de Geofísica de la Universidad de Chile, nos trae la charla:
Terremotos lentos en Chile, ¿cómo, dónde y cuándo?
(Slow earthquakes in Chile, how, where and when?)
En esta charla, Miguel resume el estado del arte del estudio de terremotos lentos en el mundo, su reciente descubrimiento, su generación y ocurrencia en diferentes ambientes tectónicos.
Acotando el área de estudio nos muestra las diferentes señales sísmicas y geodésicas observadas a lo largo de Chile. En particular nos comparte sus recientes estudios de tremors no volcánicos en el Punto Triple chileno y sismicidad lenta asociada a la falla Liquiñe-Ofqui, en la región de Aysén.
- published: 07 May 2020
- views: 1128
PLAYLIST TIME:
PLAYLIST TIME:
5:49
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault Syst...
published: 07 Jun 2021
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System
- Report rights infringement
- published: 07 Jun 2021
- views: 67
Luis Astudillo Sotomayor: Research Line RL3 - Neotectonics of the Liquiñe-Ofqui Fault System (LOFS) between 38°S and 40.5°S: Implications fo the Assessment of the Seismic Assessment.
0:20
Falla Liquiñe-Ofqui - Geparque Patagonia Verde
published: 13 Jun 2023
Falla Liquiñe-Ofqui - Geparque Patagonia Verde
Falla Liquiñe-Ofqui - Geparque Patagonia Verde
- Report rights infringement
- published: 13 Jun 2023
- views: 200
0:15
Falla tectónica Liquiñe
En Chile hay varias fallas tectónicas, esto se incrementó en algunos lugares por el terrem...
published: 08 Jan 2024
Falla tectónica Liquiñe
Falla tectónica Liquiñe
- Report rights infringement
- published: 08 Jan 2024
- views: 2513
En Chile hay varias fallas tectónicas, esto se incrementó en algunos lugares por el terremoto de 9.5 ( grabado en el canal) en Valdivia.
Lo que muestro hoy es una de las tantas y se llama .. Falla Liquiñe Ofqui.
Enero 2024.
0:27
Biobío-Aluminé Fault Zone | Wikipedia audio article
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Biob%C3%...
published: 07 Jun 2019
Biobío-Aluminé Fault Zone | Wikipedia audio article
Biobío-Aluminé Fault Zone | Wikipedia audio article
- Report rights infringement
- published: 07 Jun 2019
- views: 3
This is an audio version of the Wikipedia Article:
https://en.wikipedia.org/wiki/Biob%C3%ADo-Alumin%C3%A9_Fault_Zone
Listening is a more natural way of learning, when compared to reading. Written language only began at around 3200 BC, but spoken language has existed long ago.
Learning by listening is a great way to:
- increases imagination and understanding
- improves your listening skills
- improves your own spoken accent
- learn while on the move
- reduce eye strain
Now learn the vast amount of general knowledge available on Wikipedia through audio (audio article). You could even learn subconsciously by playing the audio while you are sleeping! If you are planning to listen a lot, you could try using a bone conduction headphone, or a standard speaker instead of an earphone.
Listen on Google Assistant through Extra Audio:
https://assistant.google.com/services/invoke/uid/0000001a130b3f91
Other Wikipedia audio articles at:
https://www.youtube.com/results?search_query=wikipedia+tts
Upload your own Wikipedia articles through:
https://github.com/nodef/wikipedia-tts
Speaking Rate: 0.9044353972429492
Voice name: en-GB-Wavenet-C
"I cannot teach anybody anything, I can only make them think."
- Socrates
SUMMARY
=======
The Biobío-Aluminé Fault Zone is a northwest-trending geological fault zone in south-central Chile and Argentina. The fault aligns with the middle-upper course of Bío Bío River where fault traces are largely covered with fluvial gravels. The northernmost reaches of the north-south Liquiñe-Ofqui Fault intersect and displace the Biobío-Aluminé Fault Zone.
0:40
Liquiñe cascada
Cascada de liquiñe comuna de panguipulli
published: 13 Oct 2016
Liquiñe cascada
Liquiñe cascada
- Report rights infringement
- published: 13 Oct 2016
- views: 226
Cascada de liquiñe comuna de panguipulli
2:40
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault.
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault (Linar...
published: 07 Jun 2021
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault.
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault.
- Report rights infringement
- published: 07 Jun 2021
- views: 29
Martín Riedel: Research Line RL3 - Micro-seismicity of the Mesamávida Crustal Fault (Linares, Maule Region) Through a local seismic network.
5:49
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle.
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic...
published: 07 Jun 2021
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle.
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle.
- Report rights infringement
- published: 07 Jun 2021
- views: 46
Joaquín Julve: Research Line RL2-5 - Crustal Fault Dynamics Through the Subduction Seismic Cycle: Unraveling the Liquiñe-Ofqui Fault System Case.
1:13:20
“Conversatorio nº1 en Beauchef 2021”, "Descubrimiento del Volcán Mate Grande, Patagonia Chilena"
La Escuela de Postgrado y Educación Continua EPEC, les invita a un nuevo ciclo de “Convers...
published: 29 Apr 2021
“Conversatorio nº1 en Beauchef 2021”, "Descubrimiento del Volcán Mate Grande, Patagonia Chilena"
“Conversatorio nº1 en Beauchef 2021”, "Descubrimiento del Volcán Mate Grande, Patagonia Chilena"
- Report rights infringement
- published: 29 Apr 2021
- views: 129
La Escuela de Postgrado y Educación Continua EPEC, les invita a un nuevo ciclo de “Conversatorios en Beauchef 2021”, con la charla "Descubrimiento del Volcán Mate Grande a lo largo de la Zona de Fallas Liquiñe-Ofqui, Patagonia Chilena", del académico del Departamento de Geología Gregory De Pascale.
52:47
Jose Piquer - Fundamental basement faults, magmas and hydrothermal fluids
José Piquer is the Director of the Institute of Earth Sciences at Universidad Austral de C...
published: 31 Aug 2021
Jose Piquer - Fundamental basement faults, magmas and hydrothermal fluids
Jose Piquer - Fundamental basement faults, magmas and hydrothermal fluids
- Report rights infringement
- published: 31 Aug 2021
- views: 1023
José Piquer is the Director of the Institute of Earth Sciences at Universidad Austral de Chile and he'll be coming by tomorrow to chat about fundamental basement faults, magmas and hydrothermal fluids with recent advances from the Andes.
Several authors have recognized the relevant role played by fundamental basement faults in controlling the distribution and geometry of magmatic-hydrothermal systems. The talk begins with a discussion about the concept of fundamental basement fault, its relevance for mineral exploration and the difficulties involved in properly recognizing them, particularly in active orogenic systems.
This is followed by a presentation of recent advances in the study of fundamental basement faults in the Andes of Chile and Argentina, with an emphasis on studies based on structural mapping, which illustrate the expressions of this type of long-lived fault systems in the field.
1:06:02
Charla 1 GeoCharlas T3 - Miguel Sáez
En la primera charla de nuestro ciclo GeoCharlas T3, el candidado a Doctor, Miguel Sáez de...
published: 07 May 2020
Charla 1 GeoCharlas T3 - Miguel Sáez
Charla 1 GeoCharlas T3 - Miguel Sáez
- Report rights infringement
- published: 07 May 2020
- views: 1128
En la primera charla de nuestro ciclo GeoCharlas T3, el candidado a Doctor, Miguel Sáez del Departamento de Geofísica de la Universidad de Chile, nos trae la charla:
Terremotos lentos en Chile, ¿cómo, dónde y cuándo?
(Slow earthquakes in Chile, how, where and when?)
En esta charla, Miguel resume el estado del arte del estudio de terremotos lentos en el mundo, su reciente descubrimiento, su generación y ocurrencia en diferentes ambientes tectónicos.
Acotando el área de estudio nos muestra las diferentes señales sísmicas y geodésicas observadas a lo largo de Chile. En particular nos comparte sus recientes estudios de tremors no volcánicos en el Punto Triple chileno y sismicidad lenta asociada a la falla Liquiñe-Ofqui, en la región de Aysén.
Liquiñe-Ofqui Fault
The Liquiñe-Ofqui Fault is major geological fault that runs a length of roughly 1000 km in a north-south direction and exhibits current seismicity. It is located in the Chilean Northern Patagonian Andes. It is a dextral intra-arc transform fault. When considered a fault zone, the Liquiñe-Ofqui Fault Zone (LOFZ) might include other neighboring faults such as Reigolil-Pirihueico Fault.
As the name implies it runs from the Liquiñe Valley hot springs in the north to the Ofqui Isthmus in the south, where the Antarctic Plate meets the Nazca Plate and the South American Plate in Chile Triple Junction. A large part of the fault runs along the Moraleda Channel. North of Liquiñe the fault is gradually converted into a compression area. At Quetrupillán volcano the fault is crossed by the Gastre Fault Zone. It may be classified as a dextral intra-arc transform fault.
The fault name was coined by Francisco Hervé, I. Fuenzalida, E. Araya and A. Solano in 1979. The fault itself was first inferred by Chilean government agent Hans Steffen around 1900 who referred to it as a "tectonic furrow" (Spanish: surco tectónico).
This page contains text from Wikipedia, the Free Encyclopedia - https://wn.com/Liquiñe-Ofqui_Fault
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