This archived dataset accompanies the article "Paleobathymetry of submarine lavas in the Samail and Troodos ophiolites: insights from volatiles in glasses and implications for hydrothermal systems" in the Journal of Geophysical Research: Solid Earth (Belgrano et al. 2021). Comprehensive details on the aquisition and selection of this data are given in the accompanying article. This dataset archive consists of a multi-sheet Excel file containing: (1) Newly measured major element and H2O (± CO2) compositions for volcanic glasses recovered from the Samail ophiolite, respectively determined by electron microprobe analysis (EMPA) and Fourier Transform infrared spectroscopy (FTIR). (2) The raw Beer-Lambert equation parameters as used to determin...
Fourier transform infrared spectroscopy (FTIR) is an analytical technique utilized to measure the co...
Water and molecular carbon dioxide concentrations, the speciation of water, and hydrogen isotope rat...
The analysis of volatile traces such as H2O and CO2 in volcanic minerals may provide significant con...
Hydrostatic pressure exerted by the ocean water column fundamentally influences magmatic and hydroth...
Hydrostatic pressure exerted by the ocean water column fundamentally influences magmatic and hydroth...
ISOTOPE ratios and concentrations of incompatible trace elements are remarkably successful in discri...
Fresh volcanic glasses from the extrusive section of the Troodos Ophiolite in Akaki Canyon are thole...
Knowledge of the isotopic evolution of volcanic eruptions is essential to volcanologists, geochemist...
Thermogravimetric analysis-mass spectrometry (TGA-MS) is potentially a powerful tool for measurement...
The North Arch volcanic field is a submarine suite of alkali basaltic to nephelinitic lavas of the s...
The chemical compositions of tephra shards are widely utilised in a myriad of disciplines, including...
This paper reports new FTIR data on the H2O and CO2 concentrations in glasses of 26 naturally quench...
The major magmatic volatile components—H2O, CO2, S, Cl, and F— play an important role in the formati...
Volcanic glasses are an amorphous phyllosilicates formed by the fast cooling of the magma. The physi...
Volcanic ash (<2mm) erupted from the Aeolian Islands is reported distally as layers in sedimentar...
Fourier transform infrared spectroscopy (FTIR) is an analytical technique utilized to measure the co...
Water and molecular carbon dioxide concentrations, the speciation of water, and hydrogen isotope rat...
The analysis of volatile traces such as H2O and CO2 in volcanic minerals may provide significant con...
Hydrostatic pressure exerted by the ocean water column fundamentally influences magmatic and hydroth...
Hydrostatic pressure exerted by the ocean water column fundamentally influences magmatic and hydroth...
ISOTOPE ratios and concentrations of incompatible trace elements are remarkably successful in discri...
Fresh volcanic glasses from the extrusive section of the Troodos Ophiolite in Akaki Canyon are thole...
Knowledge of the isotopic evolution of volcanic eruptions is essential to volcanologists, geochemist...
Thermogravimetric analysis-mass spectrometry (TGA-MS) is potentially a powerful tool for measurement...
The North Arch volcanic field is a submarine suite of alkali basaltic to nephelinitic lavas of the s...
The chemical compositions of tephra shards are widely utilised in a myriad of disciplines, including...
This paper reports new FTIR data on the H2O and CO2 concentrations in glasses of 26 naturally quench...
The major magmatic volatile components—H2O, CO2, S, Cl, and F— play an important role in the formati...
Volcanic glasses are an amorphous phyllosilicates formed by the fast cooling of the magma. The physi...
Volcanic ash (<2mm) erupted from the Aeolian Islands is reported distally as layers in sedimentar...
Fourier transform infrared spectroscopy (FTIR) is an analytical technique utilized to measure the co...
Water and molecular carbon dioxide concentrations, the speciation of water, and hydrogen isotope rat...
The analysis of volatile traces such as H2O and CO2 in volcanic minerals may provide significant con...