Influence of high marine Ca/SO4 ratio on alteration of submarine basalts at 2.41 Ga documented by triple O and Sr isotopes of epidote

Author:

Zakharov D.O.,Lundstrom C.C.,Laurent O.,Reed M.H.,Bindeman I.N.

Funder

National Geographic Society

Evolving Earth Foundation

NSF

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference122 articles.

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

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

3. Isotopic composition of gypsum in the Macquarie Island ophiolite: Implications for the sulfur cycle and the subsurface biosphere in oceanic crust;Alt;Geology,2003

4. Alt, J.C., Teagle D.A.H. 2000. Hydrothermal alteration and fluid fluxes in ophiolites and oceanic crust. In Ophiolites and oceanic crust: new insights from field studies and the Ocean Drilling Program Geological Society of America. Available at: https://pubs.geoscienceworld.org/books/book/501/chapter/3800685 [Accessed February 17, 2020].

5. Alt, J.C., Teagle, D.A.H., Bach, W., Halliday, A.N., Erzinger, J., 1996a. Stable and strontium isotopic profiles through hydrothermally altered upper oceanic crust, Hole 504B. Proceedings of the Ocean Drilling Program Scientific Results 148, 57–69.

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