Author Posting. © American Geophysical Union, 2005. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geochemistry Geophysics Geosystems 6 (2005): Q11001, doi:10.1029/2005GC001013.Heat flow measurements colocated with seismic data across 106 Ma seafloor of the Madeira Abyssal Plain (MAP) reveal variations in seafloor heat flow of ±10–20% that are positively correlated with basement relief buried below thick sediments. Conductive finite element models of sediments and upper basement using reasonable thermal properties are capable of generating the observed positive correlation between basement relief and seafloor heat flow, but with vari...
Three-dimensional modeling of convection in the oceanic crust at Deep Sea Drilling Project site 504B...
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of Am...
Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here ...
[1] Heat flow measurements colocated with seismic data across 106 Ma seafloor of the Madeira Abyssal...
Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of Am...
Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of Am...
Author Posting. © American Geophysical Union, 2014. This article is posted here by permission of Am...
[1] We use coupled heat and mass transport models to investigate the basement permeability distribut...
The evolution of oceanic crust plays an integral role in global heat flow, geochemical cycles, and i...
We compiled a suite of 490 heat flow measurements from the Pacific Ocean in areas with less than 85 ...
[1] Areas of the seafloor at mid‐ocean ridges where hydrothermal vents discharge are easily recogniz...
Journal ArticleSeafloor heat flow has been estimated continuously along a transect on the sedimented...
Geophysical observations and models provide important constraints on the properties of seafloor hydr...
Along with the intracrustal heat source, crustal permeability is considered as the controlling facto...
Half-space cooling and plate models of varying complexity have been proposed to account forchanges i...
Three-dimensional modeling of convection in the oceanic crust at Deep Sea Drilling Project site 504B...
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of Am...
Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here ...
[1] Heat flow measurements colocated with seismic data across 106 Ma seafloor of the Madeira Abyssal...
Author Posting. © American Geophysical Union, 2006. This article is posted here by permission of Am...
Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of Am...
Author Posting. © American Geophysical Union, 2014. This article is posted here by permission of Am...
[1] We use coupled heat and mass transport models to investigate the basement permeability distribut...
The evolution of oceanic crust plays an integral role in global heat flow, geochemical cycles, and i...
We compiled a suite of 490 heat flow measurements from the Pacific Ocean in areas with less than 85 ...
[1] Areas of the seafloor at mid‐ocean ridges where hydrothermal vents discharge are easily recogniz...
Journal ArticleSeafloor heat flow has been estimated continuously along a transect on the sedimented...
Geophysical observations and models provide important constraints on the properties of seafloor hydr...
Along with the intracrustal heat source, crustal permeability is considered as the controlling facto...
Half-space cooling and plate models of varying complexity have been proposed to account forchanges i...
Three-dimensional modeling of convection in the oceanic crust at Deep Sea Drilling Project site 504B...
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of Am...
Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here ...