(Q58041825)

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The Somuncura Large Igneous Province in Patagonia: Interaction of a Transient Mantle Thermal Anomaly with a Subducting Slab

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The Somuncura Large Igneous Province in Patagonia: Interaction of a Transient Mantle Thermal Anomaly with a Subducting Slab (English)

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S. Mahlburg Kay

1

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A. A. Ardolino

series ordinal

2

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M. L. Gorring

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3

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V. A. Ramos

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4

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publication date

21 September 2006

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published in

Journal of Petrology

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volume

48

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issue

1

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page(s)

43-77

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Is the African plate stationary?

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https://api.crossref.org/works/10.1093%2FPETROLOGY%2FEGL053

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21 January 2018

Late Cenozoic tectonics of the Southern Chile Trench

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21 January 2018

Large igneous provinces: Crustal structure, dimensions, and external consequences

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https://api.crossref.org/works/10.1093%2FPETROLOGY%2FEGL053

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21 January 2018

Mantle Processes and Sources of Neogene Slab Window Magmas from Southern Patagonia, Argentina

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https://api.crossref.org/works/10.1093%2FPETROLOGY%2FEGL053

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21 January 2018

Episodic arc migration, crustal thickening, subduction erosion, and magmatism in the south-central Andes

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21 January 2018

The IUGS systematics of igneous rocks

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21 January 2018

Southern Patagonian plateau basalts and deformation: Backarc testimony of ridge collisions

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21 January 2018

Nature and composition of the continental crust: A lower crustal perspective

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retrieved

21 January 2018

Coupling of South American and African Plate Motion and Plate Deformation

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https://api.crossref.org/works/10.1093%2FPETROLOGY%2FEGL053

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21 January 2018

A large-scale isotope anomaly in the Southern Hemisphere mantle

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21 January 2018

Ocean-ridge basalts with convergent-margin geochemical affinities from the Chile Ridge

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reference URL

https://api.crossref.org/works/10.1093%2FPETROLOGY%2FEGL053

retrieved

21 January 2018

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DOI

10.1093/PETROLOGY/EGL053

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(Q58041825)

The Somuncura Large Igneous Province in Patagonia: Interaction of a Transient Mantle Thermal Anomaly with a Subducting Slab

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