Hydrothermal calcite formation in Campi Flegrei caldera, Italy: unraveling carbon sink processes in alkaline volcanic systems. [PDF]
Buono G+3 more
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Unveiling spatial variations in atmospheric CO2 sources: a case study of metropolitan area of Naples, Italy. [PDF]
Di Martino RMR+4 more
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Transient crystallisation of rare earth carbonates during the hydrothermal oxidation of siderite. [PDF]
M M, R R, A M S, L T, J D RB.
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Comparative Population Genomics Unveils Congruent Secondary Suture Zone in Southwest Pacific Hydrothermal Vents. [PDF]
Tran Lu Y A+15 more
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Population Genetics of the Deep-sea Acorn Barnacle Bathylasma hirsutum (Hoek, 1883) and the First Report of its Affiliation with a Hydrothermal Vent Field. [PDF]
Neuhaus J+4 more
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Application of Solvent-Assisted Dual-Network Hydrogel in Water-Based Drilling Fluid for Lost Circulation Treatment in Fractured Formation. [PDF]
Zheng X+5 more
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Paleoproterozoic Mississippi Valley-type mineralization at Black Angel, Greenland: evidence from sulfide δ<sup>66</sup>Zn and rhenium-osmium geochronology. [PDF]
Saintilan NJ+5 more
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Ultraslow spreading ridges: slowest but locally thickest. [PDF]
Liu CZ, Zhu RX.
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Discovery of authigenic apatite pellets in rare-earth elements-rich deep-sea sediments
Liao J+7 more
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Controls on the physics and chemistry of seafloor hydrothermal circulation
Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 1997Low temperature diffuse hydrothermal circulation is a natural consequence of the cooling of the oceanic lithosphere. Diffuse flow is expected to be ubiquitous, and will be present both within mid–ocean ridge crest axial zones of young age (0–1 Ma), and also on the older ridge crest flanks and limbs.
Henry Elderfield, Adam Schultz
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