Triple oxygen and hydrogen isotopic study of hydrothermally altered rocks from the 2.43–2.41 Ga Vetreny belt, Russia: An insight into the early Paleoproterozoic seawater

Author:

Zakharov D.O.,Bindeman I.N.ORCID

Funder

NSF

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference111 articles.

1. Oceanic faulting and fault-controlled subseafloor hydrothermal alteration in the sheeted dike complex of the Josephine ophiolite;Alexander;J. Geophys. Res. Earth,1993

2. Oxygen isotope composition of a section of lower oceanic crust, ODP Hole 735B;Alt;Geochem. Geophys. Geosyst.,2006

3. An oxygen isotopic profile through the upper kilometer of the oceanic crust, DSDP Hole 504B;Alt;Earth Planet. Sci. Lett.,1986

4. Mineralogy and stable isotopic compositions of the hydrothermally altered lower sheeted dike complex, hole 504B, leg 140;Alt;Proc. Ocean Drill. Progr. Sci. Results,1995

5. Hydrothermal alteration of a section of upper oceanic crust in the easter equatorial Pacific: a synthesis of results from Site 504 (DSDP Legs 69, 70, and 83, and ODP Legs 111, 137, 140, and 148);Alt;Proc. Ocean Drill. Program Sci. Results,1996

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