R. Omarini

发表

An overview of the Mesozoic-Cenozoic magmatism and tectonics in Eastern Paraguay and central Andes (western Gondwana): implications for the composition of mantle sources.

Â. Min, M. Gasparon, P. Comin-Chiaramonti, 2016 .

Puncoviscana folded belt in northwestern Argentina: testimony of Late Proterozoic Rodinia fragmentation and pre-Gondwana collisional episodes

A. Seilacher, H. Götze, R. Omarini, 1999 .

Combined U–Pb and Lu–Hf isotope data on turbidites of the Paleozoic basement of NW Argentina and petrology of associated igneous rocks: Implications for the tectonic evolution of western Gondwana between 560 and 460 Ma

M. Matteini, M. Pimentel, N. Hauser, 2011 .

Pliocene intraplate-type volcanism in the Andean foreland at 26°10′S, 64°40′W (NW Argentina): Implications for magmatic and structural evolution of the Central Andes

L. Vezzoli, R. Mazzuoli, H. Guillou, 2010 .

The Quaternary calc-alkaline volcanism of the Patagonian Andes close to the Chile triple junction: geochemistry and petrogenesis of volcanic rocks from the Cay and Maca volcanoes (̃45°S, Chile)

A. Lahsen, F. Innocenti, P. Manetti, 2003 .

The geochemical variations of the upper cenozoic volcanism along the Calama–Olacapato–El Toro transversal fault system in central Andes (~24°S): petrogenetic and geodynamic implications

M. Matteini, R. Mazzuoli, R. Cas, 2002 .

Mingling and mixing features in basaltic andesites of the Eastern Cordillera (Central Andes, 24°S): a petrographic and microanalytical study

M. Matteini, R. Mazzuoli, N. Hauser, 2006 .

Miocene magmatism and tectonics of the easternmost sector of the Calama–Olacapato–El Toro fault system in Central Andes at ~24°S: Insights into the evolution of the Eastern Cordillera

M. Matteini, L. Vezzoli, R. Mazzuoli, 2008 .

Geodynamical evolution of Central Andes at 24°S as inferred by magma composition along the Calama–Olacapato–El Toro transversal volcanic belt

M. Matteini, R. Mazzuoli, R. Cas, 2002 .

The Aguilar pluton (23°12′ S-65°40′ W; NW Argentina): Petrological implications on the origin of the Late Jurassic intraplate magmatism in the Central Andes

L. Vezzoli, R. Mazzuoli, A. Gioncada, 2013 .

Topaz magmatic crystallization in rhyolites of the Central Andes (Chivinar volcanic complex, NW Argentina): Constraints from texture, mineralogy and rock chemistry

P. Orlandi, L. Vezzoli, R. Mazzuoli, 2014 .

Pre-Mesozoic evolution of the central Andes; The basement revisited

R. Harmon, S. Kelley, W. Todt, 1990 .

Geological evolution and pre-Gond wanic nomenclatur e in Northwest Ar gentina (1800 - 160 Ma)

R. Omarini, R. Sureda, 1999 .

Tectonomagmatic characteristics of the back‐arc portion of the Calama–Olacapato–El Toro Fault Zone, Central Andes

U. Riller, L. Vezzoli, R. Mazzuoli, 2011 .

Geological Development and Structures

R. Omarini, T. Bogdanic, K. Reutter, 2013 .

Central Andean Transect: Nazca Plate to Chaco Plains, Southwestern Pacific Ocean, Northern Chile, and Northern Argentina

H. Götze, R. Omarini, 1991 .

Reply to comment on “Kinematic variations across Eastern Cordillera at 24°S (Central Andes): Tectonic and magmatic implications”

M. Matteini, L. Vezzoli, R. Mazzuoli, 2009 .

Kinematic variations across Eastern Cordillera at 24°S (Central Andes): Tectonic and magmatic implications

M. Matteini, R. Mazzuoli, V. Acocella, 2007 .

KinematicvariationsacrossEasternCordilleraat24°S(CentralAndes): Tectonic and magmatic implications

M. Matteini, L. Vezzoli, R. Mazzuoli, 2007 .