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Titlebook: Basement Tectonics 7; Proceedings of the S Robert Mason Conference proceedings 1992 Springer Science+Business Media Dordrecht 1992 Deformat

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Counterclockwise Converging Basement Fracturing Patterns Across the Arabian Peninsula and Eastern Irifficult to detect in the field because the feeble surface expressions of the individual lineaments are commonly camouflaged by surface features such as linear sand dunes and yardangs. Their tectonic origin and rejuvenating nature are suggested by several indications: 1) their smooth passage across
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Evidence of Large Horizontal Earth Movements features in the U.S. and Canada. A . versus . graph of these features strongly resembles the similarly plotted curves of Lunar and Martian impact craters of the same size range, indicating that these large Earth features may have a similar origin and history. The one hundred-plus features mapped ar
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Rift Related Magmatism and the Petrogenesis of Lavas from the Kiejo Eruptive, Rungwe Volcanic Provinction. Structural trends inferred from volcanological features display a dominantly north to north-westerly alignment within the province. Volcanic episodes date from late Tertiary (10 Ma) through to Recent, with the last eruption occurring approximately 190 years ago from the Kiejo eruptive..Compos
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Deformation and Intrusion in Deeply Buried Rocks: Creep, High-Angle Ductile and Brittle Shear, and Cractures and brittle-ductile or ductile shear zones that form at low or high angles (less than or more than 45°) to the axis of greatest compressive stress (σ.). A new Continuum criterion for deformation allows us to graph the stresses that result in flow (including creep), and virtually any orienta
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Western Himalaya Basement Reactivationrtiary structures superimposed over the Precambrian fabric. The outer belt of epigra de metamorphics and granites comprising the Chail Unit was upthrust in a wedge shape along the steeply dipping Chail Thrust in the Western foothills. This thrust flattens eastward and gives rise to the south-vergent
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