Research articles

The effects of meteoric diagenesis on the geochemical composition and microstructure of Pliocene fossil Terebratalia coreanica and Laqueus rubellus brachiopod shells from northeastern Japan

Fujioka H, Takayanagi H, Yamamoto K, Iryu Y

Scaling land-surface variables for landslide detection

Sîrbu F, Drăguţ L, Oguchi T, Hayakawa Y, Micu M

Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research

Itamiya H, Sugita R, Sugai T

Freeze-thaw durability of repair mortars and porous limestone: compatibility issues

Ákos Török and Balázs Szemerey-Kiss

Habitat evolution of a peat swamp forest and belowground carbon sequestration during the Holocene along the coastal lowland in Central Sumatra, Indonesia

Fujimoto K, Miura M, Kobayashi S, Simbolon H

Millennial-scale variability of East Asian summer monsoon inferred from sea surface salinity in the northern East China Sea (ECS) and its impact on the Japan Sea during Marine Isotope Stage (MIS) 3

Kubota Y, Kimoto K, Tada R, Uchida M, Ikehara K

Postseismic fluid discharge chemically recorded in altered pseudotachylyte discovered from an ancient megasplay fault: an example from the Nobeoka Thrust in the Shimanto accretionary complex, SW Japan

Hasegawa R, Yamaguchi A, Fukuchi R, Hamada Y, Ogawa N, Kitamura Y, Kimura G, Ashi J, Ishikawa T

Universat-SOCRAT multi-satellite project to study TLEs and TGFs

Panasyuk M, Klimov P, Svertilov S, Belov A, Bogomolov V, Bogomolov A, Garipov G, Iyudin A, Kaznacheeva M, Maksimov I, Minaev A, Novikov A, Minaev P, Petrov V, Pozanenko A, Shtunder Y, Yashin I

Southern Hemisphere mid- and high-latitudinal AOD, CO, NO2, and HCHO: spatiotemporal patterns revealed by satellite observations

Ahn DH, Choi T, Kim J, Park SS, Lee YG, Kim S, Koo JH

Geological record of prehistoric tsunamis in Mugi Town, facing the Nankai Trough, western Japan

Shimada Y, Fujino S, Sawai Y, Koichiro T, Matsumoto D, Momohara A, Saito-Kato M, Yamada M, Hirayama E, Suzuki T, Chagué C