Results 21 to 30 of about 1,920 (208)

Serpentinites and serpentinites within a fossil subduction channel: La Corea mélange, eastern Cuba [PDF]

open access: yesGeologica Acta, 2011
A variety of metaultramafic (serpentinite) rocks in La Corea mélange, Sierra de Cristal, eastern Cuba, show differences in chemical, textural and mineralogical characteristics demonstrating a variety of protoliths.
I.F. BLANCO QUINTERO   +4 more
doaj   +2 more sources

Accretion versus erosion and sediment transfer balance near the subduction interface [PDF]

open access: yesComptes Rendus. Géoscience
The nature and amount of sediment transferred from one plate to the other near the subduction interface partly determines the tectonic and seismogenic regime of a margin.
Lallemand, Serge   +3 more
doaj   +2 more sources

Evolving temperature field in a fossil subduction channel during the transition from subduction to collision (Tauern Window, Eastern Alps) [PDF]

open access: yesJournal of Metamorphic Geology, 2020
We investigate the evolution of the three‐dimensional thermal structure of a palaeo‐subduction channel exposed in the Penninic units of the central Tauern Window (Eastern Alps).
Pleuger, Jan; 1Institut für Geologische Wissenschaften Freie Universität Berlin Berlin Germany   +8 more
core   +4 more sources

Ophiolite mélange zone records exhumation in a fossil subduction channel

open access: yesGeology, 2007
Recent models propose that the exhumation of high-pressure rocks occurs by means of return flow inside a low-viscosity channel of serpentinite situated between the plates.
FEDERICO, LAURA   +3 more
core   +2 more sources

Large Igneous Province Record Through Time and Implications for Secular Environmental Changes and Geological Time‐Scale Boundaries

open access: yesGeophysical Monograph Series, Page 1-26., 2021

Exploring the links between Large Igneous Provinces and dramatic environmental impact

An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Richard E. Ernst   +8 more
wiley  

+2 more sources

Transient Permeability of a Deep‐Seated Subduction Interface Shear Zone

open access: yesGeophysical Research Letters, 2023
Slow slip and tremor is observed along many subduction margins and is commonly linked to fluid pressure variations and migration. Accurate estimates of porosity and permeability around subduction megathrust shear zones are vital for understanding fluid ...
J. Muñoz‐Montecinos, W. M. Behr
doaj   +1 more source

A likely geological record of deep tremor and slow slip events from a subducted continental broken formation

open access: yesScientific Reports, 2022
Fluids in subduction zones play a key role in controlling seismic activity, drastically affecting the rheology of rocks, triggering mineral reactions, and lowering the effective stress.
Francesco Giuntoli, Giulio Viola
doaj   +1 more source

Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas [PDF]

open access: yesSolid Earth, 2018
The Himalayas are the archetype of continental collision, where a number of long-standing fundamental problems persist in the Greater Himalayan Sequence (GHS): (1) contemporaneous reverse and normal faulting, (2) inversion of metamorphic grade, (3 ...
F. O. Marques   +4 more
doaj   +1 more source

Long-term slow slip events along the Nankai trough delayed by the 2016 Kumamoto earthquake, Japan

open access: yesEarth, Planets and Space, 2020
The Global Navigation Satellite System network in Japan detected transient crustal deformation along the Nankai trough, Japan, from June 2018. Time-dependent inversion analysis shows that a long-term slow slip event in northern Hyuga-nada Sea along the ...
Shinzaburo Ozawa   +3 more
doaj   +1 more source

Recent Crustal Deformation in West-Central South America [PDF]

open access: yes, 2003
I use interferometric synthetic aperture radar (InSAR) to create maps of crustal deformation along the coast and within the volcanic arc of central South America. I image deformation associated with six subduction zone earthquakes, four volcanic centers,
Pritchard, Matthew Earl
core   +1 more source

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