Deconvolving low-temperature alteration and post-sampling oxidation in submarine pumice from active hydrothermal fields of the middle Okinawa Trough

Surface peat accumulation rates estimated by the multiple radionuclides in the wetland on the plateau in eastern Hokkaido, Japan

Concentrations and isotope ratios of Mo and W in Okinawa Trough hydrothermal fluids: Novel probes for hydrothermal processes in a back-arc basin

Magnesium silicate hydrate regulates the dissolution of natural ultramafic rocks and associated hydrogen generation at low temperatures

Glimmerite and melteigite xenoliths from the Early Cretaceous Campto-tinguaite dyke, Nongchram Fault Zone (East Garo Hills), Shillong Plateau, North East India: Evidence for magma mixing and involvement of subducted as well as plume related mantle sources

Large disequilibrium of ²³⁴U/²³⁸U isotope ratios in deep groundwater and its potential application as a groundwater mixing indicator

Deconvolving low-temperature alteration and post-sampling oxidation in submarine pumice from active hydrothermal fields of the middle Okinawa Trough

Surface peat accumulation rates estimated by the multiple radionuclides in the wetland on the plateau in eastern Hokkaido, Japan

Concentrations and isotope ratios of Mo and W in Okinawa Trough hydrothermal fluids: Novel probes for hydrothermal processes in a back-arc basin

Magnesium silicate hydrate regulates the dissolution of natural ultramafic rocks and associated hydrogen generation at low temperatures

Glimmerite and melteigite xenoliths from the Early Cretaceous Campto-tinguaite dyke, Nongchram Fault Zone (East Garo Hills), Shillong Plateau, North East India: Evidence for magma mixing and involvement of subducted as well as plume related mantle sources

Large disequilibrium of ²³⁴U/²³⁸U isotope ratios in deep groundwater and its potential application as a groundwater mixing indicator