The central-western Mediterranean area is a key region for understanding the complex
interaction between igneous activity and tectonics. In this review, the specific geochemical …

Abstract The Central Mediterranean region is one of the most important areas on Earth for
studying subduction-related potassic and ultrapotassic magmatism, derived from partial …

Ultrapotassic lavas having distinct geochemical compositions (K2O/Na2O> 2, K2O> 3%, and
MgO> 3%) are common and widespread on the Tibet Plateau, where they are closely linked …

Postcollisional potassium-rich magmatism in southern Tibet provides an important insight
into the deep processes inducing accelerated plateau uplift and associated geologic …

The Songpan Ganzi Fold Belt (SGFB), SW China, was developed from a passive continental
margin into an orogenic belt with the consumption of the Paleo-Tethys. During the evolution …

This paper furnishes a brief, but exhaustive, description of the tectonics and stratigraphy of
the Campania region (southern Italy). The attached geological map (Main Map) at 1 …

The central-western Mediterranean is one of the most important areas on Earth for studying
subduction-related potassic and ultrapotassic magmatism. In the circum-Tyrrhenian area …

Subduction drags a large amount of CO 2 into the Earth's interior, which is partly returned to
the atmosphere by arc volcanism. Processes involved in the recycling of subducted carbon …

We investigated the melting behavior of peridotite fluxed with 25 wt% of H 2 O-bearing
rhyolitic sediment melt (1.8 wt% bulk H 2 O), by performing experiments from 1100 to 1300° …

Abstract The Eocene and Miocene volcanic rocks between the cities of Trabzon and Giresun
in the Eastern Pontides (NE Turkey) erupted as mildly and moderately alkaline magmas …