The Northern Patagonia Somuncura plateau basalts: A product of slab-induced, shallow asthenospheric upwelling?

Terra Nova

Volumn 13, Issue 2, 2001, Pages 117-121

  De Ignacio, Cristina ^a   López, Ivan ^b   Oyarzun, Roberto ^a   Márquez, Alvaro ^a  

^a UNIVERSIDAD COMPLUTENSE DE MADRID   (Spain)

^b UNIVERSIDAD REY JUAN CARLOS   (Spain)

Author keywords

[No Author keywords available]

Indexed keywords

ASTHENOSPHERE; BASALT; TECTONIC EVOLUTION; TECTONIC RECONSTRUCTION; TERTIARY; UPWELLING;

ARGENTINA; PATAGONIA;

EID: 0035203460     PISSN: 09544879     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-3121.2001.00326.x     Document Type: Article

References (30)

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2. Seismicity and shape of the subducted Nazca plate
3. The 1960 Chilean earthquakes
4. The extra-Andean Patagonian volcanic plateau of Somuncura, Argentina
5. Plumes, orogenesis, and supercontinental fragmentation
6. The timing and duration of the Karoo igneous event, Southern Gondwana
7. Origin of the Columbia Plateau and Snake River Plain, deflection of the Yellowstone plume
8. Neogene Patagonian plateau lavas: Continental magmas associated with ridge collission at the Chile Triple Junction
9. Plate detachment, asthenosphere upwelling, and topography across subduction zones
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11. The relationship between alkaline magmatism, lithospheric extension and slab window formation along continental destructive plate margin
12. Delamination and delamination magmatism
13. The Somuncura plateau: An Oligo-Miocene 'baby-hotspot' in extra-Andean Patagonia (40.5° to 43.5° Latitude)
14. El origen de la meseta de Somuncura: Distribución y geoquímica de sus rocas volcánicas máficas
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