Results 91 to 100 of about 13,990 (220)

Impact of Mantle Velocity Uncertainty on Receiver‐Function Imaging of the Transition Zone

Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract Seismological estimates of the 400‐km and 670‐km mantle discontinuities (d400 and d670) are crucial for understanding the thermochemical structure and dynamics of the mantle transition zone (MTZ). However, artifacts from using ray theory and uncertainties in mantle velocity structure can affect topographic mapping of these boundaries.
Carlos A. M. Chaves, Felipe P. Corral, Jeroen Ritsema   +2 more
wiley   +1 more source

Impulsive supply of volatile-rich magmas in the shallow plumbing system of Mt. Etna volcano [PDF]

, 2018
Magma dynamics at Mt. Etna volcano are frequently recognized as the result of complex crystallization regimes that, at shallow crustal levels, unexpectedly change from H2O -undersaturated to H2O-saturated conditions, due to the impulsive and irregular ...
Gaeta, Mario, Mollo, Silvio, Palladino, Danilo Mauro, Perinelli, Cristina, Pia De Cristofaro, Serena, Scarlato, Piergiorgio   +5 more
core   +1 more source

Seismic Attenuation Reveals Fault and Forearc Structure Across the Subduction‐Collision Transition in Southern Taiwan

Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract The Southern Array for the Lithosphere and Uplift of Taiwan Experiment (SALUTE) provides a new window into the subduction‐collision transition zone in southern Taiwan, where the Eurasian Plate‐Luzon Arc convergence drives intense orogeny and crustal deformation. Using dense P‐ and S‐wave spectral amplitude data recorded by SALUTE and a quality
Yu‐Pin Lin, Shu‐Huei Hung, Tai‐Lin Tseng, Pei‐Ying Patty Lin, Eh Tan, Ying‐Nien Chen   +5 more
wiley   +1 more source

Moho Depth Variations in Central Italy

, 2013
[1] Along the Italian peninsula adjoin two crustal domains, peri-Tyrrhenian and Adriatic, whose boundary is not univocal in central Italy. In this area, we attempt to map the extent of the Moho in the two terrains from variations of the travel time difference between the direct P wave and the P-to-S wave converted at the crust-mantle boundary, called ...
Emiliano Di Luzio, Giuliana Mele, Cristina Di Salvo   +2 more
openaire   +1 more source

U and Th content in the Central Apennines continental crust: a contribution to the determination of the geo-neutrinos flux at LNGS

, 2011
The regional contribution to the geo-neutrino signal at Gran Sasso National Laboratory (LNGS) was determined based on a detailed geological, geochemical and geophysical study of the region.
A. Riva, Agostinelli, Anderson, Araki, Argnani, Arpesella, Babbucci, Barchi, Bassin, Battaglia, Beccaluva, Behn, Bellini, Bellotti, Bernoulli, Bernoulli, Bigi, Billi, Billi, Borghi, Boriani, Boriani, C. Tomei, Calamita, Carminati, Carruba, Cassinis, Cavazza, Cavinato, Cermak, Channel, Christensen, Ciarapica, Cipollari, Coltorti, Coltorti, Conticelli, Crescenti, Dal Piaz, De Marchi, Della Vedova, Dewey, Di Luzio, Dziewonski, D’Amico, Eder, Elter, Enomoto, F. Mantovani, Finetti, Finetti, Finetti, Finetti, Fiorentini, Fiorentini, Fogli, Franz, G. Di Carlo, G. Fiorentini, G. Rusciadelli, Gao, Ghisetti, Govindaraju, Holbrook, Hunziker, Hurtig, Jenkyns, Jochum, Jolivet, Lachance, Lucente, M. Coltorti, M. Morsilli, Mantovani, Mantovani, Martinis, Marx, Mazzucchelli, McDonough, Mele, Oldow, Palme, Panza, Patacca, Patacca, Patacca, Plank, Ponziani, Quick, Quick, R. Boraso, R. Tassinari, Raghavan, Rivalenti, Rothschild, Rudnick, Rudnick, Salter, Sani, Santantonio, Sassi, Schnetger, Scisciani, Scisciani, Scrocca, Speranza, Telford, V. Chubakov, Vai, Viti, Wedepohl, Workman, Wortel, Yegorova, Zappaterra, Zartman   +115 more
core   +1 more source

The Detection of Transient Subduction Zone Interface Properties Using Teleseismic Data

Geophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract The physical properties of subduction zone interfaces govern the transition between stable aseismic slip, episodic slow slip events (SSEs), and large earthquakes. Ultraslow velocity layers (USVLs) along the megathrust are commonly interpreted as indicators of elevated pore‐fluid pressures that promote slow slip, but their temporal variability ...
F. Rappisi, T. J. Craig, S. Rost
wiley   +1 more source

Three‐dimensional Moho topography in Italy: New constraints from receiver functions and controlled source seismology

Geochemistry, Geophysics, Geosystems, 2011
In complex tectonics regions, seismological, geophysical, and geodynamic modeling require accurate definition of the Moho geometry. Various active and passive seismic experiments performed in the central Mediterranean region revealed local information on
R. Di Stefano, I. Bianchi, M. G. Ciaccio, G. Carrara, E. Kissling   +4 more
doaj   +1 more source

PENENTUAN PATAHAN DAN TOPOGRAFI MOHO PADA DATA NOAA-FA BERBASIS FFT

Jurnal Neutrino: Jurnal Fisika dan Aplikasinya, 2012
Regional Gravity NOAA-FA data analysis using several gradient methods has been conducted to determine the fracture and direction fault based on FFT.
Sungkono, Bagus Jaya Santosa
doaj   +1 more source

Moho Interface Modeling Beneath the Himalayas, Tibet and Central Siberia Using GOCO02S and DTM2006.0

Terrestrial, Atmospheric and Oceanic Sciences, 2013
We apply a newly developed method to estimate the Moho depths and density contrast beneath the Himalayas, Tibet and Central Siberia. This method utilizes the combined least-squares approach based on solving the inverse problem of isostasy and using the ...
Robert Tenzer, Mohammad Bagherbandi, Cheinway Hwang, Emmy Tsui-Yu Chang   +3 more
doaj   +1 more source

Tectonic evolution of a continental collision zone: A thermomechanical numerical model [PDF]

, 2004
We model evolution of a continent-continent collision and draw some parallels with the tectonic evolution of the Himalaya. We use a large-scale visco-plasto-elastic thermomechanical model that has a free upper surface, accounts for erosion and deposition
Avouac, J.-P., Burov, E., Toussaint, G.
core