Now showing items 51-70 of 70

    Recent faulting and active shortening of the Middle Atlas Mountains, Morocco, within the diffuse African-Eurasian plate boundary [1]
    Rheology of dacitic volcanoes: from magma chamber to eruptive style [1]
    Role of Li and B bearing fluids in crystallization and alteration of granitic pegmatites, San Diego, California [1]
    Seismic anisotropy beneath the southern Puna Plateau [1]
    Seismic attenuation of regional phases in the northern Middle East and the Tibetan Plateau [1]
    Seismic tomography and anisotropy: studies of intraplate seismic zones [1]
    Spatial, temporal, and petrogenetic relationships of basaltic and lamprophyric dikes and sills of the Raton Basin, southern Colorado and northern New Mexico [1]
    Structural analysis of basin margin laramide folding and fault reactivation in the south-central Wind River Basin, Schoettlin Mountain quadrangle, Fremont County, Wyoming [1]
    Structural geology and contact metamorphism along the northwestern thermal aureole of the Laramie anorthosite complex, Central Laramie Mountains, Wyoming [1]
    Structural geology and tectonics of the paleoproterozoic rocks of the Mount Rushmore Quadangle, Black Hills, Souh Dakota [1]
    A study of Quaternary active tectonics [1]
    Surface and deep water circulation in late Cretaceous North Atlantic greenhouse ocean [1]
    Temperature-dependent thermal transport properties of major Archean rock types and implications for the thermal evolution of Archean terranes [1]
    Two phases of extension in North China since Mesozoic : [1]
    Two-plane wave tomography and lithospheric structure beneath eastern Tibet [1]
    Unraveling the fluid-present metamorphism of schists from garnet compositions in the Black Hills, South Dakota [1]
    Upper mantle shear wave velocity structure of the east Anatolian-Caucasus region [1]
    Variation and fractionation of lithium isotopes within single tourmaline crystals in the pegmatites of the Black Hills, SD [1]
    The viscosity of dacitic liquids measured at conditions relevant to explosive arc volcanism: determing the influence of temperature, silicate composition, and dissolved volatile content [1]