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- W2124659912 abstract "The exposure of 1300 meters of upper oceanic crust at the Blanco Fracture Zone allows near-bottom gravity measurements to determine the in situ density of the seafloor as a function of depth. Gravity measurements along the north wall of the Blanco Depression indicate an outcrop density of 2530 ± Kg/m³ for the upper 800 meters of crust and a calculated porosity of 23%. The lower 500 meters of crust (800 to 1300 meters below the sea floor) has a measured density of 2710 ± 130 Kg/m³ and a porosity of 14%. These data indicate that most of the extrusive volcanic oceanic crust is highly porous and can act as an aquifer and large-scale reservoir for hydrothermal fluids. These direct crustal density measurements also support previous interpretations that low seismic velocities observed in Layer 2 are due to the high porosity of the upper extrusive section." @default.
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- W2124659912 date "2000-04-01" @default.
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- W2124659912 title "Density and porosity of the upper oceanic crust from seafloor gravity measurements" @default.
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- W2124659912 doi "https://doi.org/10.1029/1999gl011130" @default.
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