We review petrological and geochemical features of silicic pyroclastic deposits of dominantly
low to moderate (0–25%) crystallinity, and volumes in the range of 5–1000 km 3, erupted …

More than 5000 km 3 of nearly compositionally homogeneous crystal-rich dacite (∼ 68 wt%
SiO 2:∼ 45% Pl+ Kfs+ Qtz+ Hbl+ Bt+ Spn+ Mag+ Ilm+ Ap+ Zrn+ Po) erupted from the Fish …

Abstract Recent inference that Mesozoic Cordilleran plutons grew incrementally during> 106
yr intervals, without the presence of voluminous eruptible magma at any stage, minimizes …

Multistage histories of incremental accumulation, fractionation, and solidification during
construction of large subvolcanic magma bodies that remained sufficiently liquid to erupt are …

In continental-margin subduction zones, basalt magmas spawned in the mantle interact with
the crust to produce a broad spectrum of volcanic arc associations. A distinct style of very …

Evolution of the local plate tectonic and volcanic system relationship at Kyushu Island is
defined by major changes in tectonics and volcanic style at ca. 15, 10, 6, and 2 Ma. Plate …

To illuminate rifting processes across the Transition Zone between the extensional Great
Basin and stable Colorado Plateau interior, we collected an east‐west profile of 117 …

Uncertainty surrounds the fate of the orogenic plateau in what is now the Great Basin in
western Utah and Nevada, which resulted from the Mesozoic and earliest Cenozoic …

The∼ 5000 km3 Fish Canyon Tuff (FCT) is an important unit for the geochronological
community because its sanidine, zircon and apatite are widely used as standards for the …

Multiple eruptions of silicic magma (dacite and rhyolites) occurred over the last~ 3 My in the
Kos-Nisyros volcanic center (eastern Aegean sea). During this period, magmas have …