about
Fracture propagation to the base of the Greenland Ice Sheet during supraglacial lake drainage.Intermittent plate tectonics?Trench-parallel anisotropy produced by foundering of arc lower crust.Grain-size dynamics beneath mid-ocean ridges: Implications for permeability and melt extractionFoundering of lower island-arc crust as an explanation for the origin of the continental Moho.Spreading rate dependence of gravity anomalies along oceanic transform faults.Automated analysis of electrospray ionization fourier transform ion cyclotron resonance mass spectra of natural organic matter.Response to Comment on "Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply".Greenland supraglacial lake drainages triggered by hydrologically induced basal slip.Response to Comment on "Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply"Corrigendum: Greenland supraglacial lake drainages triggered by hydrologically induced basal slipSensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supplyMorphology and segmentation of the western Galápagos Spreading Center, 90.5°-98°W: Plume-ridge interaction at an intermediate spreading ridgeCorrelated geophysical, geochemical, and volcanological manifestations of plume-ridge interaction along the Galápagos Spreading CenterA three-dimensional gravity model of the southern contact of the Sebago pluton, Maine
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P50
description
researcher
@en
wetenschapper
@nl
հետազոտող
@hy
name
Mark D Behn
@nl
Mark D Behn
@sl
Mark D. Behn
@en
Mark D. Behn
@es
type
label
Mark D Behn
@nl
Mark D Behn
@sl
Mark D. Behn
@en
Mark D. Behn
@es
prefLabel
Mark D Behn
@nl
Mark D Behn
@sl
Mark D. Behn
@en
Mark D. Behn
@es
P1053
F-5813-2012
P106
P1153
6602078294
P31
P3829
P496
0000-0002-2001-1335