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Titlebook: Basement Tectonics 11 Europe and Other Regions; Proceedings of the E O. Oncken,C. Janssen Conference proceedings 1996 Springer Science+Busi

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Country Rock Displacement during Emplacement of the Joshua Flat Pluton, White-Inyo Mountains, Califom monzonite to granodiorite. This batholith intruded upper Proterozoic to lower Paleozoic anchizonal to greenschist facies, multiply deformed metasediments during which a narrow (.004 to.16 batholith radii) structural aureole formed in the country rock. The structural characteristics of this aureole
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Lower Continental Crust Exhumed: Granulite Grade Terranes and Amphibolite Grade Shear Zones in the Aites with seismic velocities as high as P.=6.35–7.05 km/s, densities of 2.85–3.08 g/cm. (Meissner, 1986) and radioactive heat productions of A=0.48–0.53 µW/m. (Rudnick, 1992, Kremenetsky et al., 1986). In contrast the upper crust is enriched with highly radioactive granite batholiths and granite-mig
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Multifractal Analysis of Fault Structures in Basement Rocksrocks (Hirata et al, 1987; Sammis and Biegel, 1989) because it provides the simplest nontrivial description of scale invariance of physical systems. Computer simulation of quasi-static fracture in solids that incorporates lattice models (Louis and Guinea, 1989; Hassold and Srolovitz, 1989) also gene
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Seismic Data of the Carpathian Foredeep Basement (Romania)seismic reflection/ refraction profiles as well as gravity and thermal studies carried out in the foredeep area of the southern and eastern Carpathians provide information on the crustal structure of the study region. The variability in the reflectivity pattern and crustal thickness shown by the dif
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Pre-Paleozoic Crustal Tectonics Controlling Paleozoic and Tertiary Metallogenies in the Central Regiile ore deposits identified a 500 km long and 50 km wide belt where old and modern ore deposits coexist..The NNE belt, which is accompanied by important Paleozoic granites and Tertiary volcanics, has strong Bouguer gravity anomalies. This belt includes a block of crust with anomalous thicknesses tha
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