[图书][B] Rock quality, seismic velocity, attenuation and anisotropy

N Barton - 2006 - taylorfrancis.com
Seismic measurements take many forms, and appear to have a universal role in the Earth
Sciences. They are the means for most easily and economically interpreting what lies …

Channelized fluid flow in oceanic crust reconciles heat-flow and permeability data

AT Fisher, K Becker - Nature, 2000 - nature.com
Hydrothermal fluid circulation within the sea floor profoundly influences the physical,
chemical and biological state of the crust and the oceans. Circulation within ridge flanks (in …

Upper lithospheric structure of the subduction zone offshore of southern Arauco peninsula, Chile, at∼ 38 S

E Contreras‐Reyes, I Grevemeyer… - Journal of …, 2008 - Wiley Online Library
A joint interpretation of swath bathymetric, seismic refraction, wide‐angle reflection, and
multichannel seismic data was used to derive a detailed tomographic image of the Nazca …

The crustal structure of the Cocos ridge off Costa Rica

CHE Walther - Journal of Geophysical Research: Solid Earth, 2003 - Wiley Online Library
The submarine Cocos ridge in the northwestern Panamá basin, a bathymetric feature more
than 1000‐km long and 250–500 km broad, is about 2 km shallower than the adjacent …

Impact of bending related faulting on the seismic properties of the incoming oceanic plate offshore of Nicaragua

M Ivandic, I Grevemeyer, A Berhorst… - Journal of …, 2008 - Wiley Online Library
A seismic wide‐angle and refraction experiment was conducted offshore of Nicaragua in the
Middle American Trench to investigate the impact of bending‐related normal faulting on the …

Seismic investigations of the O'Higgins Seamount Group and Juan Fernández Ridge: Aseismic ridge emplacement and lithosphere hydration

H Kopp, ER Flueh, C Papenberg, D Klaeschen - Tectonics, 2004 - Wiley Online Library
The O'Higgins Seamount Group is a cluster of volcanic domes located 120 km west of the
central Chilean Trench on the crest of the Juan Fernández Ridge. This aseismic hot spot …

Variations in the distribution of magma in the lower crust and at the Moho beneath the East Pacific Rise at 9–10 N

WC Crawford, SC Webb - Earth and Planetary Science Letters, 2002 - Elsevier
Measurements of the seafloor deformation under ocean waves (compliance) reveal an
asymmetric lower crustal partial melt zone (shear velocity less than 1.8 km/s) beneath the …

Alteration of the subducting oceanic lithosphere at the southern central Chile trench–outer rise

E Contreras‐Reyes, I Grevemeyer… - Geochemistry …, 2007 - Wiley Online Library
Hydrothermal circulation and brittle faulting processes affecting the oceanic lithosphere are
usually confined to the upper crust for oceanic lithosphere created at intermediate to fast …

Seismic layer 2A: Evolution and thickness from 0‐to 70‐Ma crust in the slow‐intermediate spreading South Atlantic

J Estep, R Reece, DA Kardell… - Journal of …, 2019 - Wiley Online Library
Layer 2A, the porous and permeable uppermost igneous oceanic crust, permits the
circulation of fluid within the crust, the exchange of dissolved mineral species between the …

Marine hydrogeology: recent accomplishments and future opportunities

AT Fisher - Hydrogeology Journal, 2005 - Springer
Marine hydrogeology is a broad-ranging scientific discipline involving the exploration of fluid–
rock interactions below the seafloor. Studies have been conducted at seafloor spreading …