Inhaltsbereich
Publication
(Co) Author: Schnurr, W.
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(2007): Twenty-five million years of felsic magmatism in the southern Central Volcanic Zone of the Andes: geochemistry and magma genesis of ignimbrites from 25-27°S, 67-72°W. Journal of Volcanology and Geothermal Research, 166, 1, 17-46.
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(2001): Geochemistry and isotope systematics of small- to medium-volume Neogene-Quaternary ignimbrites in the southern central Andes: evidence for derivation from andesitic magma sources. Chemical Geology, 171, 3-4, 213-237.| EDOC: 1778 |
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(2006): Digital Geological Map of the Southern and Central Puna Plateau, NW Argentina. - In: Oncken, O.; Chong, G.; Franz, G.; Giese, P.; Götze, H.-J.; Ramos, V. A.; Strecker, M. R.; Wigger, P. (Eds.), The Andes - Active Subduction Orogeny, Springer, 563-564.| EDOC: 9185 |
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(2004): Twenty million years of ignibrite eruptions in the south-central volcanic zone of the Andes (25-27°S): time-space variations and relationships with the large-volume 'flare-up' systems.. IAVCEI 2004 General Assembly (Pucon, Chile 2004).| EDOC: 6628 |
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(2000): Source constraints and Pre-eruptive magmatic conditions for Neogene silicic ignimbrites from the Central Andes (23-26°S). IX Congreso Geológico Chileno, 81-82.| EDOC: 1633 |
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(1999): Neogene Ignimbrites of the southern central Andes (25-27°S, 67-69°W): Interpretation of new isotopic and trace element data in terms of a fractionation model from arc andesites. Actas del XIV Congreso Geológico Argentino.| EDOC: 2876 |
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(1999): Neogene silicic magmatism in the southern central Andes (25-27°S. 67-69°W): new aspects of ignimbrite formation. 4. International Symposium on Andean Geodynamics, 686-688.| EDOC: 1630 |
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(1998): Isotopic contrasts in Neogene ignimbrites from the central Andes (23°S - 27°S): source heterogeneity or different petrogenesis?. 16. Geowissenschaftliches Lateinamerika-Kolloquium, p. 152.| EDOC: 1629 |