Results 181 to 190 of about 7,715 (221)

Pore-pressure diffusion controls upper-plate aftershocks of the 2014 Iquique earthquake. [PDF]

Nat Commun
Peña C, Heidbach O, Metzger S, Schurr B, Moreno M, Bedford J, Oncken O, Faccenna C.   +7 more
europepmc   +1 more source

Long-term history of continental weathering and particle transport to the sea. [PDF]

Proc Natl Acad Sci U S A
Canfield DE, Zhang S, Mitchell RN, Wang X, Naemi A, Spencer CJ, Zhang P.   +6 more
europepmc   +1 more source

Evolving Southern Ocean overturning in warming climates. [PDF]

Nat Commun
Zhu T, Liu W.
europepmc   +1 more source

Seismic imaging reveals a strain-partitioned sliver and nascent megathrust at an incipient subduction zone in the northeast Pacific. [PDF]

Sci Adv
Brandl CC, Worthington LL, Roland EC, Walton MAL, Nedimović MR, Gase AC, Adedeji O, Castellanos JC, Phrampus BJ, Bostock MG, Wang K, Oliva SJ.   +11 more
europepmc   +1 more source

Rapid fault healing from cementation controls the dynamics of deep slow slip and tremor. [PDF]

Sci Adv
Thomas AM, Watkins JM, Beeler N, French ME, Behr WM, Reed MH.   +5 more
europepmc   +1 more source

Subduction Zone

, 2014
openaire   +3 more sources

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SUBDUCTION

2014
Subduction
  +5 more sources

Devolatilization During Subduction

2014
Subducted crust refertilizes the subarc mantle wedge as well as the deep convecting mantle. In the subarc region, mass transfer occurs mainly through fluids, melts, or supercritical liquids. Experiments show that devolatilization reactions may occur at almost any depth in the chemically complex subducting lithosphere.
M. Schmidt, S. Poli
openaire   +1 more source

Subduction Zones Parameters ☆

2017
Subduction zones are characterized by multiple behaviors, dynamics, or geometries. Most of them results from the complex interplay between various parameters. In this article, we define the most common parameters used by scientists and then mention the studies where (set of) parameters are tested empirically, or experimentally.
Lallemand, Serge, Heuret, Arnauld
openaire   +1 more source

SUBDUCTION ZONES

Reviews of Geophysics, 2002
Subduction zones are where sediments, oceanic crust, and mantle lithosphere return to and reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's 55,000 km of convergent plate margins and are the geodynamic system that builds island arcs.
openaire   +1 more source