Iran is a mosaic of continental terranes of Cadomian (520–600 Ma) age, stitched together
along sutures decorated by Paleozoic and Mesozoic ophiolites. Here we present the current …

We present a global synthesis of the geochemistry of intermediate to silicic intrusive and
volcanic rocks from 149 Phanerozoic to Archean ophiolites, and evaluate models for their …

We combine a geological, geochemical and tectonic dataset from 118 ophiolite complexes
of the major global Phanerozoic orogenic belts with similar datasets of ophiolites from 111 …

Geothermal exploration in the Central Andean Volcanic Zone (CAVZ) focuses on heat
capacities of known geothermal systems, yet the role of faults, veins, fractures and folds on …

The subduction of an active spreading center generates a clear signature in the temporal
evolution of subduction zones. It disrupts the typical arc‐type magmatism and intraplate …

The Taitao granites are distributed around the Late Miocene Taitao ophiolite (5.66±0.33 Ma
to 5.19±0.15 Ma) exposed at the western tip of the Taitao peninsula, southern Chile,~ 50 km …

Exposure of the ca. 6Ma Taitao ophiolite, Chile, located∼ 50km south of the Chile Triple
Junction, allows detailed chemical and isotopic study of rocks that were recently extracted …

We use digital elevation models and satellite imagery data completed with field observations
to develop an integrated morphotectonic analysis of the anomalous topography of the …

We present Re–Os isotopic data for widely dispersed mantle xenoliths carried to the surface
of southern South America (36°–52° S) by Eocene to recent alkaline magmatism. Our …

Determination of paleocurrent directions is a robust approach to establish the mechanism of
sediment transport and of deposition. However, in tectonically controlled (or affected) basins …