The belt boundary thrust within the Cretaceous–Neogene accretionary complex of the
Shimanto Belt, southwestern Japan, extends for more than~ 1 000 km along the Japanese …

A zircon fission track-annealing model is calculated on the basis of annealing experiments
from the literature with induced tracks in α-decay event damage-free zircon samples …

An assemblage of quantitative data sets is examined to evaluate tectonic mélange as a plate
boundary fault rocks in subduction zone. The research object is the latest Cretaceous Mugi …

Tectonic mélange has a key role in subduction zones because its thick pile forms the plate
boundary itself; therefore, the plate boundary process is nearly identical to the mélange …

The Nankai accretionary prism is divided into three segments: outer and inner wedges and
their transition zone. These wedges reflect different aspects of wedge taper, internal …

Актуальность работы. Изучение тектонических процессов, происходивших в областях
конвергенции литосферных плит, является фундаментальной научной проблемой …

The Mugi Mélange located in western Shikoku of the Shimanto Belt shows systematic Y‐P
deformation fabrics formed by microshear and pressure solution that penetrate throughout …

Pseudotachylyte is present in the Shimanto accretionary complex in Shikoku, Japan. The
pseudotachylyte occurs as a vein in a fault zone and displays flow structure, TiO2 microlites …

Nobeoka Thrust in Kyushu, southwest Japan, was investigated to understand the
relationship between the seismogenic out‐of‐sequence thrust (OST) and fluid flow in …

Pseudotachylyte-bearing fault zones, found in the Shimanto accretionary complex,
southwest Japan, developed during subduction or underplating at seismogenic depths. The …