Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …

Many workers accept a metamorphic model for orogenic gold ore formation, where a gold-
bearing aqueous-carbonic fluid is an inherent product of devolatilization across the …

Although the capacity for water to lower the solidus during crustal melting is well recognised,
a modern consensus is that most granitic magmas are generated under fluid-absent melting …

Fluid–rock interaction has profound effects on the dynamics of the lithosphere. This
Perspectives article describes the catalytic effects of water on the kinetics of mineral …

Magmatic regions are typically viewed as vertical systems, with magma coming in the bottom
and either freezing in the crust to form plutons or erupting to form volcanic rocks. Maintaining …

We modeled water exsolution from a growing and crystalizing felsic magma body using a
conductive thermal model with simplified physical mechanisms of volatile transport. Magma …

We present a 2D thermo‐elastic model of a magma body formation in a granitic crust by
injection of rhyolitic or basaltic dikes and sills. Elastic analytical solutions enable the …

In this paper, we analyse the seismic noise at Ischia Island (Italy) with the objective of
detecting the hydrothermal source signals taking advantage of the Covid-19 quiescence due …

Upper-crustal granitoids are a late-stage product of crustal differentiation. This last stage in
the evolution has been proposed to be the key interval that governs volcanic eruptions, ore …

We characterize the alteration of the Saint-Jean-du-Doigt mafic-dominated, bimodal
intrusive complex in the Armorican Massif by means of petrographic investigation and …