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The laboratory albitization of mid-ocean ridge basalt

March 1, 1988

Complete alteration of fresh mid-ocean ridge basalt to albite + actinolite + smectite took place in the presence of quartz and 3.4m NaCl at 350°C and 400 bars. Significant Na-metasomatism occurred in exchange for Ca + Fe + Mn. In contrast, alteration of the basalt/quartz mixture with a synthetically prepared "natural brine," and basalt with 3.4m NaCl or "natural brine" did not produce significant albitization. Based on these and previous experiments that reacted basalt with a variety of fluids, it is concluded that excess silica, a high Na/Ca ratio, and an absence of strong acidity (dissolved Mg) in the altering fluid are important for the albitization of basalt.

Publication Year 1988
Title The laboratory albitization of mid-ocean ridge basalt
DOI 10.1086/629213
Authors Robert J. Rosenbauer, James L. Bischoff, Robert A. Zierenberg
Publication Type Article
Publication Subtype Journal Article
Series Title Journal of Geology
Index ID 70231497
Record Source USGS Publications Warehouse
USGS Organization Pacific Coastal and Marine Science Center