The Searchlight pluton (SLP) and coeval Highland Range volcanic sequence (HRV) have
been suggested to represent intruded and erupted counterparts, and the 15 km tilted crustal …

Thermodynamic modelling shows that, although high-silica rhyolitic melts can form through
fractionation of low-silica rhyolitic magmas the complementary cumulates do not have …

Although the relationship between silicic volcanic and plutonic rocks has been extensively
studied, it remains controversial whether most plutons have volcanic counterparts and how …

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 …

Crystal-melt segregation and magma mixing are key magmatic processes that generate
compositional variabilities in igneous rocks. Distinguishing these processes can provide …

Abstract The Acoculco Caldera Complex (ACC), located in eastern Mexico, began its activity
during the Pleistocene~ 2.7 Ma. One of the most relevant and largest rhyolitic eruption in the …

S-type granitic magmas form essentially through partial melting of crustal metasedimentary
rocks, so this eliminates many possibilities for the origins of chemical variations in their …

The genesis of intermediate intrusions is highly controversial, and one of the hot topics is
whether they represent frozen melts or cumulates in the evolution of magmatic systems …

Defining the physico-chemical evolution of felsic magmatic reservoirs in the middle-upper
continental crust is crucial for understanding the connection between granitic plutons and …

The volcanic-intrusive connection is critical for understanding the formation of transcrustal
magma systems and the mechanisms driving magma eruption. Yet, the genetic links …