Titlebook: Basement Tectonics 12; Central North Americ John P. Hogan,M. Charles Gilbert Book 1998 Springer Science+Business Media Dordrecht 1998 Cambr

美學(xué)

Abduct

Insubordinate

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魯莽

The Absolute Religion: Christianity,onics. For the most part, these tectonic features are the result of regional stress on pre-existing basement fractures causing activity that interrupts the regional stratigraphic record. Facies and local absence of sedimentary units provide evidence for delineating the time and extent of these basem

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Petrologic Constraints on the Tectonic Evolution of the Llano Upliftvents. Early dynamothermal metamorphism took place at moderate to high pressures and decreased in intensity from southwest to northeast across the uplift. Late largely static metamorphism at lower pressures resulted from a thermal event linked to regionally widespread emplacement of granitic intrusi

Cholesterol

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萬(wàn)花筒

Surface and Near-Surface Investigation of the Alteration of the Mount Scott Granite and Geometry of ndy Creek Gabbro in the Hale Spring Area of the Wichita Mountains, shows that the upper portion of the Sandy Creek gabbro pluton is largely steep-walled, with a blunt irregular subhorizontal roof capped by Mount Scott Granite. In the subsurface, the near vertical sidewalls of the gabbro are presumed

襲擊

Multiple Reactivations of Rigid Basement Block Margins: Examples in the Northern Reading Prong, USActivated multiple times during subsequent tectonic events. The rocks in these fault zones contain complexly overprinted mylonites, cataclasites, and breccias with distinct kinematics and mineralizations. By studying the similarities and differences of rocks from three different fault zones across th