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THE COLD BAY VOLCANIC CENTER, ALEUTIAN VOLCANIC ARC: 1, IMPLICATIONS FOR THE ORIGIN OF HI-ALUMINA ARC BASALT
Brophy, J. G., 1986, The Cold Bay volcanic center, Aleutian volcanic arc: 1, Implications for the origin of Hi-alumina arc basalt: Contributions to Mineralogy and Petrology, v. 93, n. 3, p. 368-380.

DATA TABLES *Not all tables in a publication may be listed. Not all tables from a publication have data entered in the database.
52: Whole rock and modal compositions
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* (super a) Mg-# assumes all iron as FeO. Major element and V, Cr, Co, Ni, Sr and Ba abundances analyzed by ICP at Indiana University. Analyst: James Brophy. Estimated errors (1sigma, relative %) are: Si (<1), Ti (<0.5), Al (<1), Fe (<0.5), Mn (<2), Mg (<0.5), Ca (<0.5), Na (<2), K (<1.5), P (<10), V (<4), Cr (30), Co (<2), Ni (<15), Rb (<3), Sr (<2.5), Zr (<2.5), and Ba (<2). *
53: Representative plagioclase core compositions

54: Representative olivine core compositions
* (super a) Whole rock FeO contents recalculated (Sack et al. 1980) for T-fo2 conditions of 1,110 C and NNO+0.6 log units *
55: Representative clinopyroxene core compositions

56: Representative titanomagnetic core compositions

57: HAB and tholeiite compositions referred to in this study
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58: log (fO2/(fO2)NNO) T=1,110 degrees C

59: Olivine tholeiite fractionation calculations

60: Trace element distribution coefficients

61: Summary of quartz eclogite modeling


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