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Titlebook: Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung; Proceedings of the I Peter Paulitsch Conferen

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书目名称Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung
副标题Proceedings of the I
编辑Peter Paulitsch
视频video
图书封面Titlebook: Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung; Proceedings of the I Peter Paulitsch Conferen
描述Ten years have passed since the last symposium on "Rock Deformation" was held in Los Angeles. The intervening period has seen striking advances in X-ray and experimental structural petrology. The Symposium of the Working Group on X-Ray and Experimental Structural Petrology, held at the invitation of the Deutsche Forschungsgemeinschaft on 17 and 18 February, 1969, in the Mineralogy Institute of the Technische Hochschule Darmstadt, was intended to display the progress made in this field. A meeting on the same had been held in 1968 at the Mineralogy Institute of the Technische Hochschule Aachen. The outcome of many years of effort has been the development of new, automated in­ struments for the X-ray processing of specimens. The X-ray and optical data so obtained are processed by computer to give complete texture diagrams; it is also possible to rotate the coordinates, and to make an indirect determination of data which have not been measured. In experimental structural petrology, the temperature and pressure dependence of the translational system has been studied in minerals from various types of rock formation which had not previously been investigated, and deductions were made conc
出版日期Conference proceedings 1970
关键词Deformation; Gestein; formation; mineral; mineralogy; petrology
版次1
doihttps://doi.org/10.1007/978-3-642-95187-9
isbn_softcover978-3-642-95189-3
isbn_ebook978-3-642-95187-9
copyrightSpringer-Verlag, Berlin/Heidelberg 1970
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Über die Verwendbarkeit der Anisotropie der Magnetischen Suszeptibilität zur Bestimmung der MagnetitThe present paper deals with using of anisotropy of magnetic susceptibility to the determination of dimensional orientation of magnetite in rocks. As an example of practical application of this method some results for Blansko — type granodiorite from Brno massif are presented.
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Regelungseigenschaften Monomineralischer Gesteine bei Gerichteter BeanspruchungIn a hydrostatic stressfield mineral grains do not show any preferred orientation. In uniaxial stress we will expect preferred orientation for the crystallites. With optical and electrical methods the preferred orientation of experimental deformed calcite and quartz were determined.
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https://doi.org/10.1007/978-3-642-95187-9Deformation; Gestein; formation; mineral; mineralogy; petrology
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