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You are here: Home > Library > Mid-Pleistocene lavas from the Seguam volcanic center, central Aleutian arc: closed-system fractional crystallization of a basalt to rhyodacite eruptive suite

MID-PLEISTOCENE LAVAS FROM THE SEGUAM VOLCANIC CENTER, CENTRAL ALEUTIAN ARC: CLOSED-SYSTEM FRACTIONAL CRYSTALLIZATION OF A BASALT TO RHYODACITE ERUPTIVE SUITE
citation imageSinger, B. S., Myers, J. D., and Frost, C. D., 1992, Mid-Pleistocene lavas from the Seguam volcanic center, central Aleutian arc: closed-system fractional crystallization of a basalt to rhyodacite eruptive suite: Contributions to Mineralogy and Petrology, v. 110, p. 87-112.

DATA TABLES *Not all tables in a publication may be listed. Not all tables from a publication have data entered in the database.
481: Whole-rock major and trace element compositions and petrography of Turf Point Formation samples. Major elements in wt.%, trace elements in ppm. B87-57 to B87-56 are from the western TPF; B87-36 to B87-38 from the east
View table data :: Download table data (.csv)

491: Rare earth element and Pb concentrations in ppm and Sr, Nd, and Pb isotope compositions of selected TPF samples.
View table data :: Download table data (.csv)


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