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By P. R. Hooper (auth.), J. D. Macdougall (eds.)

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MacDonald and Katsura, 1964), and low values near those of the average kimberlite. Though there is much overlap among the various groups, Ti0zIP20S does show some tendency to separate the various units. Groups with high Ti0zIP20S include the Imnaha, Picture Gorge, HAOT, and all Grande Ronde lavas except for the rare, very high-Mg group. At low (<5) Ti0tp20S are the SROT and Wanapum compositional types. As the magnitude of these differences are difficult to generate either through partial melting or fractional crystallization, the observed variation in Ti0zIP20S presumably relates to differences in the bulk composition of the source materials involved in the genesis of the different lavas.

1977). Geology and petrology of the Strawberry Volcanics, northeast Oregon. D. , Univ. of Oregon, Eugene, 197 p. C. (1893). A geological reconnaissance in central Washington. s. Geol. Surv. Bull. 108, 108 p. R. A. Swanson (1970). Eruption and flow rates of flood basalts. H. , Proc. 2nd Columbia River Basalt Symp. Eastern Washington State College Press. Cheney, 271-297. A. (1986). Stratigraphy, sedimentology, and petrology of Neogene rocks in the Deschutes Basin, central Oregon: A record of continental margin volcanism and its influence on fluvial sedimentation in an arc-adjacent basin.

Ceol. Soc. Amer. Bull. 92, 669-678. E. R. Hooper (1981). Geologic studies of the Columbia Plateau: Part I. Late Cenozoic evolution of the southeast part of the Columbia River Basalt Province. Ceol. Soc. Amer. Bull. 92, 659-668. M. P. Reidel (1978). Descriptive summary of the Grande Ronde Basalt type section, Columbia River Basalt Group. ' I Informal Rept. RHO-BWI-LD-15, Richland, WA. W. (1984). Isotopic constraints on Columbia River flood basalt genesis and the nature of the subcontinental mantle.

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