Results 241 to 250 of about 46,716 (290)
Dynamics of longitudinal Hawaiian hotspot motion and the formation of the Hawaiian-Emperor Bend. [PDF]
Proc Natl Acad Sci U S AZhang J, Hu J.
europepmc +1 more source
Mode of intracontinental mountain building controlled by lower crustal composition and mantle lithosphere depletion. [PDF]
Nat CommunXu X +14 more
europepmc +1 more source
Some of the next articles are maybe not open access.
Related searches:
Related searches:
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.
Robert J Stern
exaly +2 more sources
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.
Robert J Stern
exaly +2 more sources
, 1994 This book is devoted to the quantitative physical modeling of subduction and subduction-related processes. It presents a coherent description of the modeling method (including similarity criteria, and a novel applied experimental technique), results from
Alexander I. Shemenda +1 more
openaire +2 more sources
Subduction invasion of the Atlantic by Mediterranean subduction zones
2022<p>Subduction invasion has been referred to as the process by which subduction zones from a subducting ocean invade or trigger subduction initiation in a contiguous ocean. This can, in principle, happen in different ways that can vary from a direct migration by rollback along an oceanic corridor connecting the two oceans (e.g., the ...
João C. Duarte +3 more
openaire +1 more source
Devolatilization During Subduction
2014Subducted 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
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 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
Sediment subduction and frictional sliding in a subduction zone
Geology, 1980New experimental data for the mechanical and thermodynamic properties of clays at high pressure and high temperature are applied to model the frictional sliding in a subduction zone. The model is believed applicable because of the large volume of pelagic sediments that appear to have been subducted with the oceanic plate along active Pacific margins ...
openaire +1 more source
To Subduct or not to Subduct? that is the Archaean Question…
2015info:eu-repo/semantics ...
Debaille, Vinciane +2 more
openaire +1 more source