Add to ORKG[1] The alteration of subseafloor volcanic glass from three locations is qualitatively attributed to biological (biotic) or chemical (abiotic) reactions on the basis of microscopic morphology of the boundary between the unaltered and altered glass. Eleven-element composition of fresh basalt glass (sideromelane) and its alteration products were determined by electron microprobe. Principal component analysis (PCA) usin
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major e...
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major e...
International audienceChemical alteration of basalt glasses in seawater ranks as one of the most imp...
Volcanic glass altered by microorganisms exhibits distinctive textures differing significantly from ...
Graduation date: 2006In the early 1980's the first evidence of biological alteration of basalt glass...
Submarine basaltic glass constitutes a major part of the oceanic crust and contains a number of bio-...
The majority of the Earth's shallow crust is composed of basalt that erupted on the seafloor an...
The majority of the Earth's shallow crust is composed of basalt that erupted on the seafloor and was...
This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published arti...
Within the altered parts of the glass rim of pillow lavas of Hole 896A, at depths at least 432 m bel...
International audienceFrequent observations of tubular to vermicular microchannels in altered basalt...
Alteration textures were examined in subglacial (hyaloclastite) deposits at Valafell, Southern Icela...
A detailed microbiological and geochemical study related to the alteration of basaltic glass of pill...
The abundances of 60 elements in 616 Ocean Floor Basaltic (OFB) glasses from the Abyssal Volcanic Gl...
International audienceChemical alteration of basalt glasses in seawater ranks as one of the most imp...
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major e...
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major e...
International audienceChemical alteration of basalt glasses in seawater ranks as one of the most imp...
Volcanic glass altered by microorganisms exhibits distinctive textures differing significantly from ...
Graduation date: 2006In the early 1980's the first evidence of biological alteration of basalt glass...
Submarine basaltic glass constitutes a major part of the oceanic crust and contains a number of bio-...
The majority of the Earth's shallow crust is composed of basalt that erupted on the seafloor an...
The majority of the Earth's shallow crust is composed of basalt that erupted on the seafloor and was...
This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published arti...
Within the altered parts of the glass rim of pillow lavas of Hole 896A, at depths at least 432 m bel...
International audienceFrequent observations of tubular to vermicular microchannels in altered basalt...
Alteration textures were examined in subglacial (hyaloclastite) deposits at Valafell, Southern Icela...
A detailed microbiological and geochemical study related to the alteration of basaltic glass of pill...
The abundances of 60 elements in 616 Ocean Floor Basaltic (OFB) glasses from the Abyssal Volcanic Gl...
International audienceChemical alteration of basalt glasses in seawater ranks as one of the most imp...
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major e...
International Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.Major e...
International audienceChemical alteration of basalt glasses in seawater ranks as one of the most imp...