By A. Henk (auth.), O. Oncken, C. Janssen (eds.)
The 11th foreign convention on Basement Tectonics used to be 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 hot political adjustments in jap Europe. hence, the most subject of the assembly focussed at the constitution and heritage of the full ecu continent. extra issues have been grouped round issues of present curiosity. Keynote lectures on those subject matters got via A. Berthelsen, St. Mueller, A. eco-friendly, and D. Fountain. The technical periods have been prepared with aid of the clinical Committee at the following themes: 1. Continental scale gains of basement rocks of phanerozoic cratons - with emphasis on Europe 2. Extrapolation and correlation of geological and geophysical information from basement rocks: an review 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 although all been amassed in a single half in view that them all take care of assorted elements of deformation of the continental basement. A moment half features a entire record of all papers and posters provided on the assembly. box journeys to review the various above pointed out facets within the Harz mountains, the Granulite Massif, and the Erzgebirge have been geared up via P. Bankwitz, P. Frischbutter, 1. Rotzler, okay. 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
3. Inyo Batholith The Inyo batholith forms part of a Jura-Triassic, locally alkali-rich arc extending at least from British Columbia to Mexico (Miller, 1978). This batholith is an approximately 70 by 25 km, rectangular-shaped, NW-SE oriented body consisting of several different phases (Fig. 3): the Eureka Valley monzonite, the Marble Canyon monzodiorite, the Joshua Flat monzonite, and the Beer Creek granodiorite. , 1965; McKee & Nash, 1967; Evernden & Kistler, 1970) show 2 distinct time spans from 179168 Ma (hbl) and from 170-162 Ma (bio).
8b) and no ribbons sensu stricto. The lenticular aggregates usually have symmetrical tails on sections normal to the mylonitic foliation. In some cases asymmetrical tails are also found. Analysis of the orientations of tails reveals a scattered distribution. The ribbons exhibit dynamic recrystallization textures, with the growth of new grains over subjoints normal to the mylonitic foliation, and also over grain edges (Fig. 8A, sample T-21). The distribution of orientations of new grains is usually weakly orthorhombic with a c-axis maximum close to Y.
1994) Using geological maps to constrain pluton emplacement mechanisms, Geological Society of America Abstracts with Programs, 26, 52. G. (1979) U-Pb and Pb-Pb ages of primary and detritical zircons from the White Mountains, eastern California, Geological Society of America Abstracts with Programs, 11, 79. Hanson, RB. D. Thesis], University of California Los Angeles, 231 p. B. (1987) Superimposed deformations in the development of a shear zone: An example from the northern White Mountains, California, Geological Society of America Abstracts with Programs, 18/2, 113.
Basement Tectonics 11 Europe and Other Regions: Proceedings of the Eleventh International Conference on Basement Tectonics, held in Potsdam, Germany, July 1994 by A. Henk (auth.), O. Oncken, C. Janssen (eds.)