Magmatism is very common in the Okinawa Trough. However, the influence of magmatic
processes, including fractional crystallization and magma mixing, on the petrogenesis of …

The paper presents new original data on the Devonian rift-related volcanism from the Rudny
Altai, a marginal terrane of the Siberian continent (Altai-Sayan Fold Belt, western Central …

Extension within a continental back‐arc basin initiates within continental rather than oceanic
lithosphere, and the geochemical characteristics of magmatic rocks within continental back …

Abstract The Iheya Graben is a back-arc spreading centre in the middle part of the Okinawa
Trough. It is also located in the centre of an anomalous volcanic zone (volcanic arc migration …

In the southwestern Okinawa Trough, a cluster of approximate 70 submarine volcanoes is
located at the cross back‐arc volcanic trail (CBVT), with the eruptive products dominated by …

Low δ 18 O magmas (with δ 18 O values of< 5‰) are significantly volumetrically smaller
than the abundant high δ 18 O magmas in diverse tectonic settings. We report, for the first …

Studies of the element contents and isotopic characteristics of sulfide minerals from seafloor
hydrothermal sulfide deposits are a significant method of investigating seawater-fluid mixing …

Determining the influence of subduction input on back-arc basin magmatism is important for
understanding material transfer and circulation in subduction zones. Although the mantle …

Silicate melt inclusions (SMIs) in olivine, clinopyroxene, and orthopyroxene in basalt and
trachyandesite of the middle Okinawa Trough (MOT) and in basaltic andesites of the …

The in situ element concentrations and the sulfur (S), and lead (Pb) isotopic compositions in
anglesite were investigated for samples from seafloor hydrothermal fields in the Okinawa …