1. Abstract International Ocean Discovery Program Expedition 385 drilled organic-rich
sediments and intruded sills in the off-axis region and axial graben of the northern spreading …

Pore-fluid pressure is an important parameter in controlling fault mechanics as it lowers the
effective normal stress, allowing fault slip at lower shear stress. It is also thought to influence …

Fault slip activity at subduction zones is governed by sediment frictional properties, which in
turn are affected by diagenetic processes. To study the spatial patterns in frictional …

Based on U‐Pb dating of zircon crystals and petrographic analysis, this study provides new
insights into the paleogeographic and accretion evolution along SW Japan. Our data are …

In order to investigate fault strength, healing and stability in the Nankai Trough accretionary
prism off Kii Peninsula, Japan, we conducted two series of triaxial friction experiments on …

Using logging data and samples collected by the four expeditions of the International Ocean
Discovery Program NanTroSEIZE drilling campaign that occupied Site C0002 in the Nankai …

The empirical relationship between the porosity and P‐wave velocity is a useful tool for
probing large‐scale underground physical properties and stress states based on P‐wave …

We conduct frictional experiments using cuttings collected at Nankai Trough IODP Site
C0002 over 980.5–3262.5 mbsf (meters below seafloor) depth interval to better understand …

International Ocean Discovery Program (IODP) Site C0024 is located near the deformation
front of the Nankai accretionary prism off the Kii Peninsula. The scientific objective of the …

Sediment lithology, especially the clay mineral fraction, is basic geologic information, which
is important for understanding faulting and evolutionary process of the accretionary prism …