Cite
MLA Citation
C. Schmidt et al.. “Origin of High Mg and SO4 Fluids in Sediments of the Terceira Rift, Azores‐Indications for Caminite Dissolution in a Waning Hydrothermal System.” Geochemistry, geophysics, geosystems, vol. 20, 2019, pp. 6078–6094. http://access.bl.uk/ark:/81055/vdc_100099415307.0x000023