By A. Henk (auth.), O. Oncken, C. Janssen (eds.)
The 11th foreign convention on Basement Tectonics was once held on the GeoForschungsZentrum Potsdam in Germany 25-29 July 1994. It was once the 1st time assembly of this sequence came about within the centre of Europe and the 1st such assembly during this quarter after the new political alterations in japanese Europe. accordingly, the most topic of the assembly focussed at the constitution and heritage of the total ecu continent. extra topics have been grouped round themes of present curiosity. Keynote lectures on those themes got by way of A. Berthelsen, St. Mueller, A. eco-friendly, and D. Fountain. The technical classes have been prepared with aid of the medical Committee at the following subject matters: 1. Continental scale good points of basement rocks of phanerozoic cratons - with emphasis on Europe 2. Extrapolation and correlation of geological and geophysical info from basement rocks: an overview three. Mechanisms of basement exhumation within the evolution of orogenic belts four. constitution and intraplate deformation of the North-American craton Papers submitted to this quantity have even if all been gathered in a single half given that them all take care of assorted facets of deformation of the continental basement. A moment half incorporates a whole record of all papers and posters awarded on the assembly. box journeys to check many of the above pointed out points within the Harz mountains, the Granulite Massif, and the Erzgebirge have been equipped through P. Bankwitz, P. Frischbutter, 1. Rotzler, ok. Rotzler, and B. Mingram. Their help is gratefully acknowledged.
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Extra info for Basement Tectonics 11 Europe and Other Regions: Proceedings of the Eleventh International Conference on Basement Tectonics, held in Potsdam, Germany, July 1994
The distribution of orientations of new grains is usually weakly orthorhombic with a c-axis maximum close to Y. This suggests that prismatic slip was activated in the small grains. The values of differential stress, obtained from the recrystallized grain size of quartz vary from 10 to 70 MPa. These values are lower than expected for rocks of this type (White, 1979) and suggests widespread overgrowing. ::: 0.. 3 E « . -0.. 0-.. 00 o~o 0 ° A /\ o~o 4 Amplitudes Folds l ,. B 0 Fold. I 0 Fold. II • Folds III 5 B ,.
6. Emplacement Mechanisms Supported by the results from the S edge of the Joshua Flat pluton, downward return flow of country rock is interpreted as the earliest, and one of the more important material transfer mechanisms during emplacement of the Joshua Flat pluton. The inward-bending of formations within the structural aureole all around the pluton and the systematic decreasing age of the stratigraphy within the aureole toward the pluton clearly document an increasing amount of downward movement of country rock as the pluton is approached.
T. (1973) Microstructures and preferred orientations of experimentally deformed quartzites,Geol. Soc. Amer. Bull.. 297-314. Vogel, D. E. (1967) Petrology of an eclogite- and pyrigarnite-bearing polymetamorphic rock complex at Cabo Ortegal, NW Spain, Leidse Geol. Meded.. 40, 123-213. White, S. H. (1979) Paleostress estimates in the Moine thrust zone, Nature. 280, 222-223. COUNTRY ROCK DISPLACEMENT DURING EMPLACEMENT OF THE JOSHUA FLAT PLUTON, WHITE-INYO MOUNTAINS, CALIFORNIA ECKARDT STEIN Institute for Mineralogy, TH Darmstadt D-64287 Darmstadt SCOTT R.