about
Deep seismic structure of the Tonga subduction zone: Implications for mantle hydration, tectonic erosion, and arc magmatismSeismic velocity structure and deformation due to the collision of the Louisville Ridge with the Tonga-Kermadec TrenchCrustal structure and origin of the Cape Verde RiseSeismic evidence of tectonic control on the depth of water influx into incoming oceanic plates at subduction trenchesThe Alboran volcanic-arc modulated the Messinian faunal exchange and salinity crisisSeismicity and active tectonics in the Alboran Sea, Western Mediterranean: Constraints from an offshore-onshore seismological network and swath bathymetry dataCrustal thinning in the northern Tyrrhenian Rift: Insights from multichannel and wide-angle seismic data across the basinEarly-stage rifting of the northern Tyrrhenian Sea Basin: Results from a combined wide-angle and multichannel seismic studySeismic activity at Cadamosto seamount near Fogo Island, Cape Verdes-formation of a new ocean island?Hydroacoustic Measurements of the 2014 Eruption at Ahyi Volcano, 20.4°N Mariana ArcTracking Submarine Volcanic Activity at Monowai: Constraints From Long-Range Hydroacoustic MeasurementsEpisodic magmatism and serpentinized mantle exhumation at an ultraslow-spreading centreEnhanced Mantle Upwelling/Melting Caused Segment Propagation, Oceanic Core Complex Die Off, and the Death of a Transform Fault: The Mid-Atlantic Ridge at 21.5°NSpatial variations of magmatic crustal accretion during the opening of the Tyrrhenian back-arc from wide-angle seismic velocity models and seismic reflection imagesSeismic structure and segmentation of the axial valley of the Mid-Cayman Spreading CenterSeismotectonics of the Horseshoe Abyssal Plain and Gorringe Bank, eastern Atlantic Ocean: Constraints from ocean bottom seismometer dataMagmatic-tectonic conditions for hydrothermal venting on an ultraslow-spread oceanic core complexOn the relationship between structure, morphology and large coseismic slip: A case study of the M 8.8 Maule, Chile 2010 earthquakeAftershock seismicity and tectonic setting of the 2015 September 16Mw8.3 Illapel earthquake, Central ChileCrustal structure and kinematics of the TAMMAR propagating rift system on the Mid-Atlantic Ridge from seismic refraction and satellite altimetry gravityCrustal structure of the Kermadec arc from MANGO seismic refraction profilesMantle earthquakes beneath the South Iberia continental margin and Gulf of Cadiz – constraints from an onshore-offshore seismological networkMantle exhumation and sequence of magmatic events in the Magnaghi–Vavilov Basin (Central Tyrrhenian, Italy): New constraints from geological and geophysical observationsReloca Slide: an ~24 km3submarine mass-wasting event in response to over-steepening and failure of the central Chilean continental slopeUltra-long-range hydroacoustic observations of submarine volcanic activity at Monowai, Kermadec ArcSeamountsBending-related faulting of the incoming oceanic plate and its effect on lithospheric hydration and seismicity: A passive and active seismological study offshore Maule, ChileFault geometry and permeability contrast control vent temperatures at the Logatchev 1 hydrothermal field, Mid-Atlantic RidgeThe complex 3-D transition from continental crust to backarc magmatism and exhumed mantle in the Central Tyrrhenian basinInterplate seismicity at the CRISP drilling site: The 2002 Mw 6.4 Osa Earthquake at the southeastern end of the Middle America TrenchSeismic structure of the Central Tyrrhenian basin: Geophysical constraints on the nature of the main crustal domainsSplay fault activity revealed by aftershocks of the 2010 Mw 8.8 Maule earthquake, central ChileStructure and deformation of the Kermadec forearc in response to subduction of the Pacific oceanic plateVolatile (H2O, CO2, Cl, S) budget of the Central American subduction zoneCrustal thickness and mantle wedge structure from receiver functions in the Chilean Maule region at 35°SMicroseismicity of the Mid-Atlantic Ridge at 7°S-8°15′S and at the Logatchev Massif oceanic core complex at 14°40′N-14°50′NOverriding plate structure of the Nicaragua convergent margin: Relationship to the seismogenic zone of the 1992 tsunami earthquakeUplift at lithospheric swells--II: is the Cape Verde mid-plate swell supported by a lithosphere of varying mechanical strength?Abrupt change in the dip of the subducting plate beneath north ChileControls of faulting and reaction kinetics on serpentinization and double Benioff zones
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description
geoloog
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researcher
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հետազոտող
@hy
name
Ingo Grevemeyer
@ast
Ingo Grevemeyer
@en
Ingo Grevemeyer
@es
Ingo Grevemeyer
@nl
type
label
Ingo Grevemeyer
@ast
Ingo Grevemeyer
@en
Ingo Grevemeyer
@es
Ingo Grevemeyer
@nl
prefLabel
Ingo Grevemeyer
@ast
Ingo Grevemeyer
@en
Ingo Grevemeyer
@es
Ingo Grevemeyer
@nl
P214
P227
P1053
E-5162-2016
P1960
3v2bjvgAAAAJ
P21
P213
0000 0001 1814 4641
P214
P227
P31
P3829
P496
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