The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S)
The Andes located in the central Neuquén (38°-39°S), which belong to the southern Central Andes (35°-39°S), have recorded a similar chronology of uplift than the neighbor northern Patagonian Andes (39°-46°S), Both areas have been formed trough successive phases of contraction in the Late Cretaceous,...
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2005
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p742_Morabito http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p742_Morabito |
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paper:paper_00044822_v60_n4_p742_Morabito2023-06-08T14:25:58Z The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) Folguera, Andrés Copahue-pino hachado block Episodic behavior Loncopué trough Tectonic evolution Cretaceous episodic event fold and thrust belt geochronology Miocene morphostructure Oligocene orogeny Pliocene tectonic evolution trough uplift Andes Argentina Chile Copahue Hachado Pass Neuquen Neuquen Basin Patagonia South America The Andes located in the central Neuquén (38°-39°S), which belong to the southern Central Andes (35°-39°S), have recorded a similar chronology of uplift than the neighbor northern Patagonian Andes (39°-46°S), Both areas have been formed trough successive phases of contraction in the Late Cretaceous, Middle Eocene and Late Miocene respectively. However, the Neuquén Andes have experienced two discrete phases of orogenic relaxation, during the Late Oligocene and Pliocene-Quaternary, which make then distinctive respect to the area located to the south. Field studies have shown new evidences of an episodic behavior of the fold and thrust belt in Neuquen, corresponding to compressive phases followed by stages of crustal collapse, at least since the Middle Cretaceous. The study of two main morphostructural units in the arc and retroarc area at 37°-39°S, the Alto de Copahue Pino Hachado, and its continuation to the north in the Chilean Andes (Laguna de la Laja), and the Loncopué trough respectively exemplify this particular behavior. A structural and a stratigraphie study in those areas have given a new evolutionary framework for the Neuquén Andes. © 2005 Asociación Geológica Argentina. Fil:Folguera, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2005 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p742_Morabito http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p742_Morabito |
| institution |
Universidad de Buenos Aires |
| institution_str |
I-28 |
| repository_str |
R-134 |
| collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
| topic |
Copahue-pino hachado block Episodic behavior Loncopué trough Tectonic evolution Cretaceous episodic event fold and thrust belt geochronology Miocene morphostructure Oligocene orogeny Pliocene tectonic evolution trough uplift Andes Argentina Chile Copahue Hachado Pass Neuquen Neuquen Basin Patagonia South America |
| spellingShingle |
Copahue-pino hachado block Episodic behavior Loncopué trough Tectonic evolution Cretaceous episodic event fold and thrust belt geochronology Miocene morphostructure Oligocene orogeny Pliocene tectonic evolution trough uplift Andes Argentina Chile Copahue Hachado Pass Neuquen Neuquen Basin Patagonia South America Folguera, Andrés The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) |
| topic_facet |
Copahue-pino hachado block Episodic behavior Loncopué trough Tectonic evolution Cretaceous episodic event fold and thrust belt geochronology Miocene morphostructure Oligocene orogeny Pliocene tectonic evolution trough uplift Andes Argentina Chile Copahue Hachado Pass Neuquen Neuquen Basin Patagonia South America |
| description |
The Andes located in the central Neuquén (38°-39°S), which belong to the southern Central Andes (35°-39°S), have recorded a similar chronology of uplift than the neighbor northern Patagonian Andes (39°-46°S), Both areas have been formed trough successive phases of contraction in the Late Cretaceous, Middle Eocene and Late Miocene respectively. However, the Neuquén Andes have experienced two discrete phases of orogenic relaxation, during the Late Oligocene and Pliocene-Quaternary, which make then distinctive respect to the area located to the south. Field studies have shown new evidences of an episodic behavior of the fold and thrust belt in Neuquen, corresponding to compressive phases followed by stages of crustal collapse, at least since the Middle Cretaceous. The study of two main morphostructural units in the arc and retroarc area at 37°-39°S, the Alto de Copahue Pino Hachado, and its continuation to the north in the Chilean Andes (Laguna de la Laja), and the Loncopué trough respectively exemplify this particular behavior. A structural and a stratigraphie study in those areas have given a new evolutionary framework for the Neuquén Andes. © 2005 Asociación Geológica Argentina. |
| author |
Folguera, Andrés |
| author_facet |
Folguera, Andrés |
| author_sort |
Folguera, Andrés |
| title |
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) |
| title_short |
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) |
| title_full |
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) |
| title_fullStr |
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) |
| title_full_unstemmed |
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S) |
| title_sort |
copahue-pino hachado high and the loncopuè trough: an episodic tectonic behaviour, neuquén andes (37°-39°s) |
| publishDate |
2005 |
| url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n4_p742_Morabito http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p742_Morabito |
| work_keys_str_mv |
AT folgueraandres thecopahuepinohachadohighandtheloncopuetroughanepisodictectonicbehaviourneuquenandes3739s AT folgueraandres copahuepinohachadohighandtheloncopuetroughanepisodictectonicbehaviourneuquenandes3739s |
| _version_ |
1768546655200608256 |