Three distinct tectonic regimes were identified for felsic and intermediate volcanic rocks
using published datasets from twenty-six different geographical locations around the world …

Major and trace element and Sr–Nd–Pb isotopic variations in mafic volcanic rocks hve been
studied in a 220 km transect across the Kamchatka arc from the Eastern Volcanic Front, over …

We present the results of a regional study of oxygen and Sr-Nd-Pb isotopes of Pleistocene to
Recent arc volcanism in the Kamchatka Peninsula and the Kuriles, with emphasis on the …

Trace element concentrations and B isotope compositions were determined for lavas from
the Eastern Volcanic Front (EVF), the Central Kamchatka Depression (CKD), and the …

Abstract New 40 Ar/39 Ar and published 14 C ages constrain voluminous mafic volcanism of
the Kamchatka back-arc to Miocene (3–6 Ma) and Late Pleistocene to Holocene (< 1 Ma) …

A data base for the composition and emission rates of more than 100 thermal manifestations
including boiling geothermal systems and 23 volcanoes along the 1900km long Kamchatka …

Post-collisional mafic magmas are melts of mixed sources formed by the interaction between
crust and mantle. We report the first identification of metasomatic sources formed at> 200 km …

Late Pleistocene-Holocene volcanism in Kamchatka results from the subduction of the
Pacific Plate under the peninsula and forms three volcanic belts arranged in en echelon …

Data on the geology, petrography, and geochemistry of Middle–Late-Pleistocene rocks from
the Tolbachik volcanic massif (Kamchatka, Klyuchevskaya group of volcanoes) are …

The tectonic evolution of the Shuanghu Paleo-Tethys Ocean is an important but poorly
understood issue in the geology of the Tibetan Plateau and Tethys. Here we present a new …