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1	Nature and Origin of Foliation and Lineation in Porphyry, Killarney, Ontario Collins, Wayne Robert 28 April 1988 (has links) <p> The Killarney Igneous Complex, composed of an intrusive granite and a hypabyssal or extrusive porphyry was implaced near and at the surface in the general locality of Killarney, Ontario. The crystallization age of the intrusive portion of the complex is approximately 1740 million years. These rocks have experienced deformation by forces which in some instances produced complicated shearing motions. Mesoscopic samples show a foliation and a lineation supporting a history of deformation. The foliation is clearly the more visible fabric and is interpreted as a plane of flattening.</p> <p> Kinematic indicators, specifically asymmetric pressure shadow wings, are present within the rocks; however the patterns are too complicated to interpret by a simple sense of shear. The geometry of these kinematic indicators does suggest an active plane of foliation.</p> / Thesis / Bachelor of Science (BSc)
2	How Can We Know The Poet from The Poem?: Cross-examining the Poetic Process Hall, Kira Ann January 2019 (has links) No description available. Literature Fine Arts Language Arts poetry poems poet imagery meter lineation spacing rhythm mental illness
3	Precambrian Geology of the Cottonwood Cliffs Area, Mohave County, Arizona Beard, Linda Sue January 1985 (has links) A belt of Early Proterozoic rocks crops out in the Cottonwood Cliffs area, northwest Arizona. The belt contains an eastern and a western assemblage separated by the Slate Mountain fault. The western assemblage consists of mafic to felsic metavolcanic rocks, metapelites, and metaconglomerates. The eastern assemblage consists of phyllites, felsic to intermediate metavolcanic rocks, metagraywackes, and metagabbro bodies. The belt is bounded to the east by foliated granodiorite. The Valentine granite intruded the belt on the west and north. Steeply-plunging lineations and fold axes, and northeast-trending vertical foliation dominate the structural fabric. The regional elongation direction is near-vertical, as indicated by mineral and pebble lineations, and is parallel to fold axes. Although only one deformational event is evident, the intensity of that event may have obliterated evidence of any earlier deformation. Tertiary basalts and the Peach Springs Tuff locally overly the metamorphic rocks. Cenozoic normal faults in the area are mostly of minor displacement. Arizona axial-plane structures Cenozoic Cottonwood Cliffs folds foliation intrusions lineation lithostratigraphy metamorphic rocks Miocene Mohave County Arizona Neogene northwestern Arizona Peach Springs Tuff Precambrian Proterozoic Slate Mountain Fault stratigraphy structural analysis Tertiary United States upper Precambrian Valentine Granite Geology, Stratigraphic -- Precambrian Geology -- Arizona -- Mohave County

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