Rare earth element mobility in the oceanic lower sheeted dyke complex: evidence from geochemical data and leaching experiments
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference46 articles.
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2. Alt, J.C., Teagle, D.A.H., 1997. Probing the TAG hydrothermal mound and stockwork: oxygen-isotopic profiles from deep ocean drilling. In: Humphris, S.E., Herzig, P.M., Miller, D.J., Zierenberg, R.A. (Eds.), Proc. ODP Sci. Results, 158, in press.
3. Alt, J.C., Laverne, C., Vanko, D., Tartarotti, P., Teagle, D.A.H., Bach, W., Zuleger, E., Erzinger, J., Honnorez, J., 1996. Hydrothermal alteration of a section of upper oceanic crust in the eastern equatorial Pacific: a synthesis of results from DSDP/ODP Legs 69, 70, 83, 111, 137, 140 and 148 at Site 504B. In: Alt, J.C., Kinoshita, H., Stokking, L.B., Michael, P.J. (Eds.), Proc. ODP Sci. Results, Vol. 148, pp. 417–434.
4. Bach, W., Erzinger, J., Alt, J.C., Teagle, D.A.H., 1996. Chemistry of the lower sheeted dike complex, ODP Hole 504B, Leg 148. The influence of magmatic differentiation and hydrothermal alteration. In: Alt, J.C., Kinoshita, H., Stokking, L.B., Michael, P.J. (Eds.), Proc. ODP Sci. Results, Vol. 148, pp. 39–55.
5. Rare-earth element mobility during hydrothermal and metamorphic fluid–rock interaction and the significance of the oxidation state of europium;Bau;Chem. Geol.,1991
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