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Publikováno v:
Scheuermann, PP; Syverson, DD; Higgins, JA; Pester, NJ; & Seyfried, WE. (2018). Calcium isotope systematics at hydrothermal conditions: Mid-ocean ridge vent fluids and experiments in the CaSO4-NaCl-H2O system. Geochimica et Cosmochimica Acta, 226, 18-35. doi: 10.1016/j.gca.2018.01.028. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/1wt2334j
© 2018 Elsevier Ltd Two sets of hydrothermal experiments were performed to explore Ca isotope fractionation and exchange rates at hydrothermal conditions (410–450 °C, 31.0–50.0 MPa). The first set of experiments determined the magnitude of vapo
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http://www.escholarship.org/uc/item/1wt2334j
http://www.escholarship.org/uc/item/1wt2334j
Mid-ocean ridge (MOR) hydrothermal vent fluids are enriched with dissolved barium, but due to barite (BaSO4) precipitation during mixing between Ba-bearing vent fluids and SO4-bearing seawater, the magnitude of hydrothermal Ba input to the ocean rema
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https://explore.openaire.eu/search/publication?articleId=doi_________::fc23e125a39703e742b0a6b247094543