At subduction zones, fluid flow, pore pressure, and tectonic processes are tightly
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …

It has been known for a long time that slip accompanying earthquakes accounts for only a
fraction of plate tectonic displacements. However, only recently has a fuller spectrum of …

We describe two transient slow slip events that occurred before the 2011 Tohoku-Oki
earthquake. The first transient crustal deformation, which occurred over a period of a week in …

Mud volcanism is an important natural source of the greenhouse gas methane to the
hydrosphere and atmosphere,. Recent investigations show that the number of active …

Subduction zone megathrust faults host Earth's largest earthquakes, along with multitudes of
smaller events that contribute to plate convergence. An understanding of the faulting …

Anaerobic oxidation of methane (AOM) mediated by anaerobic methanotrophic archaea
(ANME) is the primary process that provides energy to cold seep ecosystems by converting …

We document a sequence of simultaneous short‐term and long‐term slow slip events
(SSEs) at the Hikurangi subduction zone during the 2010/2011 period. The sequence of …

В монографии приведены результаты многолетних исследований закономерностей
деформирования нарушений сплошности массивов горных пород. На основе …

Coseismic static stress changes and dynamic stresses generated by seismic waves cause
changes in water level in wells and in stream flow and alter hydrogeologic properties such …

Abstract The Monviso ophiolite Lago Superiore Unit (LSU; Western Alps) constitutes a well-
preserved, largely coherent fragment of eclogitic upper oceanic lithosphere subducted to c …