Cerro prieto y su correlación con los centros de dispersión del Golfo de California
Fuente:
Redalyc
Enregistré dans:
| Auteur principal: | |
|---|---|
| Format: | Artículo científico |
| Langue: | en |
| Publié: |
Universidad Autónoma de Baja California
1996
|
| Sujets: | |
| Accès en ligne: | |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
| _version_ | 1876428365817184256 |
|---|---|
| author | Francisco Suárez Vidal |
| author_facet | Francisco Suárez Vidal |
| contents | Cerro prieto y su correlación con los centros de dispersión del Golfo de California Francisco Suárez Vidal Ana Luz Quintanilla Montoya Ciencias de la Tierra heat source Cerro Prieto spreading center Gulf of California The Cerro Prieto geothermal tield is located in the Mexicali Valley, Baia California. Tectonically,this northern part of the Gulf of California has been classitied as a spreadmg center, within a transitionalarea of oceanic to continental conditions. Thermal, geologic-tectonic and magnetic evidente hasbeen used to postulate the existence of a heat source in the area that is associated with magmatic processes,similar to those that occur in a typical oceanic spreading center. Based on the petrography andgeochemistry of the volcanic rocks obtained during the drilling of the Wells in the geothermal tield,the rocks were classified as: basalts, basalt-andesites, andesites and dacites. The petrogenetic model ofthe intrusive volcanic bodies that is proposed for the area of crustal spreading at Cerro Prieto is differentfrom the one proposed tor a typicai oceanic spreading center, as is the case for the spreadingcenters located in the Gulf of California. This region of continental basaltic magmatism is complexdue to: a) chemical composition and mineralogy of the mantle source, b) partial melting of the parentmagma, c) magma segregation depth, and d) extension of the fractioned crystalhzation and the meltingprocesses during the storage of the magma in the upper levels of the magmatic chamber. 1996 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48022107 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.1 Vol.22 |
| format | Artículo científico |
| id | redalyc_48022107 |
| institution | Redalyc |
| language | en |
| publishDate | 1996 |
| publisher | Universidad Autónoma de Baja California |
| spellingShingle | Cerro prieto y su correlación con los centros de dispersión del Golfo de California Francisco Suárez Vidal Ciencias de la Tierra heat source Cerro Prieto spreading center Gulf of California Cerro prieto y su correlación con los centros de dispersión del Golfo de California Francisco Suárez Vidal Ana Luz Quintanilla Montoya Ciencias de la Tierra heat source Cerro Prieto spreading center Gulf of California The Cerro Prieto geothermal tield is located in the Mexicali Valley, Baia California. Tectonically,this northern part of the Gulf of California has been classitied as a spreadmg center, within a transitionalarea of oceanic to continental conditions. Thermal, geologic-tectonic and magnetic evidente hasbeen used to postulate the existence of a heat source in the area that is associated with magmatic processes,similar to those that occur in a typical oceanic spreading center. Based on the petrography andgeochemistry of the volcanic rocks obtained during the drilling of the Wells in the geothermal tield,the rocks were classified as: basalts, basalt-andesites, andesites and dacites. The petrogenetic model ofthe intrusive volcanic bodies that is proposed for the area of crustal spreading at Cerro Prieto is differentfrom the one proposed tor a typicai oceanic spreading center, as is the case for the spreadingcenters located in the Gulf of California. This region of continental basaltic magmatism is complexdue to: a) chemical composition and mineralogy of the mantle source, b) partial melting of the parentmagma, c) magma segregation depth, and d) extension of the fractioned crystalhzation and the meltingprocesses during the storage of the magma in the upper levels of the magmatic chamber. 1996 artículo científico 0185-3880 https://www.redalyc.org/articulo.oa?id=48022107 en http://www.redalyc.org/revista.oa?id=480 Ciencias Marinas application/pdf Universidad Autónoma de Baja California Ciencias Marinas (México) Num.1 Vol.22 |
| title | Cerro prieto y su correlación con los centros de dispersión del Golfo de California |
| topic | Ciencias de la Tierra heat source Cerro Prieto spreading center Gulf of California |
| url | https://www.redalyc.org/articulo.oa?id=48022107 |