This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …

Ultramafic soils are in equal parts fascinating and dangerous. Developed on rocks derived
predominately from the Earth's mantle and metamorphosed at the ocean floors, ultramafic …

Granitoids are a major component of the continental crust. They play a pivotal role in its
evolution, either by adding new material (continental growth), or by reworking older …

The strong resilience of the mineral zircon and its ability to host a wealth of isotopic
information make it the best deep-time archive of Earth's continental crust. Zircon is found in …

The Himalayan orogeny, a result of the collision of India and Eurasia, provides direct
evidence of strain accommodation and large-scale rheological behavior of the continental …

Despite several decades of investigations, inferences on the timing and nature of collisions
along the Mesozoic–Cenozoic Eurasian margin remain controversial. We assimilate …

Continental arcs in Cordilleran orogenic systems display episodic changes in magma
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …

We review igneous experimental data designed to understand fractionation processes in the
roots of magmatic arcs, focusing on fractional crystallization experiments in dry and hydrous …

The intraoceanic Kohistan arc, northern Pakistan, exposes a complete crustal section
composed of infracrustal basal cumulates formed at≤ 55km depth, a broadly …

We review data and recent research on arc composition, focusing on the relatively complete
arc crustal sections in the Jurassic Talkeetna arc (south central Alaska) and the Cretaceous …