TY  - GEN 
AU  - Coltat, Rémi
AU  - Andreani, M.
AU  - Patten, C. G. C.
AU  - Godard, Marguerite
AU  - Debret, Baptiste
AU  - Escartin, Javier
PY  - 2023
UR  - https://hdl.handle.net/10481/85248
AB  - At Mid-Ocean Ridges, hot, reduced, acidic, and metal-rich fluids are responsible for the formation of ultramafic-hosted seafloor massive sulfide deposits (UM-SMSs), where mantle exhumation efficiently operates. As UM-SMSs display great structural,...
LA  - eng
PB  - Wiley
KW  - Mid-Atlantic Ridge
KW  - Mantle exhumation
KW  - Fluid-rock interactions
KW  - Element geochemistry
KW  - Metals
KW  - Seafloor massive
KW  - Sulfide deposits
TI  - Origin of Fe-Ca-Metasomatism in Exhumed Mantle Rocks at the MARK Area (23°N, ODP Leg 153) and Implications on the Formation of Ultramafic-Hosted Seafloor Massive Sulfide Deposits
DO  - 10.1029/2023GC010894
ER  -