The origin of large miarolitic (also known as “chamber”) pegmatites is not fully understood
although they may have great economic value. The formation of cavities in magmatic bodies …

In crystal-rich magma, gas bubble formation causes magma lubrication by loosening the
connected crystal framework. In contrast, if the crystal framework behaves as rigid, the gas …

Copper–gold porphyry deposits are the world's main source of copper and a significant
source of gold. They consist of vein networks and their surrounding alteration zones …

Porphyry-type deposits are the world's main source of copper and molybdenum and provide
a large proportion of gold and other metals. However, the mechanism by which mineralising …

The physical process of crystal-melt separation is responsible for the accumulation of small
to very large volumes (> 100 km3) of eruptible rhyolitic melt in the shallow crust. Granitic …

In recent years, the volcanic–plutonic relationship has been a contentious topic among
researchers. Based on this issue, they have delved deeper into the constraints of magma …

Groundmass textures of volcanic rocks provide valuable insights into the processes of
magma ascent, crystallization, and eruption. The diktytaxitic texture, characterized by a lath …

Abstract Models for the evolution of magma mush zones are of fundamental importance for
understanding magma storage, differentiation in the crust, and melt extraction processes that …

When partial melting is parametrized in numerical thermo-mechanical models in a
straightforward manner, it directly relates to variations in temperature. However, melt …

Abstract The Paleocene-Eocene Cerro Munro pluton, to the east of the North Patagonian
Batholith (NPB), is a tonalitic intrusion emplaced as a shallow, small, sub-circular tonalite …