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Saturday, August 1, 2020 | History

3 edition of Experimental deformation of polyphase rock analogues found in the catalog.

Experimental deformation of polyphase rock analogues

Experimental deformation of polyphase rock analogues

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  • 34 Currently reading

Published by Geologisch Instituut der Rijksuniversiteit in Utrecht .
Written in English

    Subjects:
  • Geodynamics

  • Edition Notes

    11

    The Physical Object
    Pagination207 p.
    Number of Pages207
    ID Numbers
    Open LibraryOL22023178M
    ISBN 109071577643

      The Karelia and Belomorian Provinces include a large number of generally NNW-trending greenstone belts, whose tectonic settings of origin may include an oceanic plateau, island arc and/or continental rift. The ages of volcanic rocks in these greenstone belts vary from to by:   AAPG Annual Convention and Exhibition Redefining Reservoir. June , , Calgary, Alberta, Canada.

      Modern analogues for Miocene to Pleistocene alkali basaltic phreatomagmatic fields in the Pannonian Basin: “soft-substrate” to “combined” aquifer controlled phreatomagmatism in intraplate volcanic fields Research Article Lankreijer A., Lithospheric memory and stress field controls on polyphase deformation of the Pannonian basin Cited by: Pressure-Temperature-time-Deformation paths derived from FIAs, pseudosections and zoned garnets: significance and potential for ~ Ma deformation and metamorphism in the Big Thompson region of Colorado Rockies, USA: Shank, Joel A.*; A. Guy Plint.

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Experimental deformation of polyphase rock analogues Download PDF EPUB FB2

Experimental deformation of polyphase rock analogues. [Utrecht: Faculteit Aardwetenschappen der Universiteit Utrecht, ?] (OCoLC) Material Type: Thesis/dissertation: Document Type: Book: All Authors / Contributors: Paul Dirk Bons.

Frictional slip of granite at hydrothermal conditions Experimental deformation of polyphase rock ana-logues The analysis of progressive deformation in rock analogues Jan The first approach was to do creep tests and transparent deformation cell experiments with two-phase composites of organic crystalline rock-analogues, camphor and octachloropropane (OCP).

Dome and basin folds are structures with circular or slightly elongate outcrop patterns, which can form during single- and polyphase deformation in various tectonic settings. We used power-law viscous rock analogues to simulate single-phase dome-and-basin folding of rocks undergoing dislocation by: 4.

Introduction. The first use of the terms boudin and boudinage are attributed to Marcel Lhoest during an August 31st, field trip of the Sociétè Géologique de Belgique, to the Carrière Collignon near Bastogne (Ardennes – Belgique) (Lohest et al.,Sintubin, ).The structures described by as boudins by Lohest are, in fact, mullions (Pilgers and Schmidt,Urai et al Cited by: 4.

DEFORMATION MICROSTRUCTURES IN QUARTZO-FELDSPATHIC ROCKS € PREFACE € € € TABLE OF CONTENTS € € € € In the past decade there has been enormous progress in our understanding of the deformation mechanisms and rheology of Earth materials, due to progress in experimental rock deformation studies as well as detailed studies of.

Cambridge Core - Solid Earth Geophysics - Deformation of Earth Materials - by Shun-ichiro KaratoCited by: Abstract. Geological observations, particularly of evidence for deformation, are made at scales ranging from m to 10 4 m.

Structural geologists use field relations to determine the relative timing of deformation events, and to determine their cumulative effect on structural patterns in the by: 2.

Experimental study of the evolution of fault gouge in layered sand-clay sequences. Fluid assisted rock deformation and tectonic. Symposium in honour of Florian J. Lehner, Paris, April(). The application of results from experimental rock deformation, allied to concepts from materials science, has developed a quantitative understanding of lithospheric rheology (e.g., Kohlstedt et al., ).

These insights have then been taken to provide explanations of different deformation patterns on a variety of length and time scales.

Experimental post-entrapment water loss from synthetic CO2-H2O inclusions in natural quartz. Geochim. Cosmochim. Acta, 55, Balashov, D. and Ikhenov, D. Nuclear Quadrupole Resonance in Copper (I) Oxide, Potassium Chlorate, and p-Dichlorobenzene high pressures.

The deformation and recrystallization of Biotite in the. Cambridge Core - Solid Earth Geophysics - Salt Tectonics - by Martin P. JacksonCited by: The processes that initiate and maintain prograde ductile shear zones are not well understood.

We have performed shear experiments (γ = 1 to 3) on a fine-grained (– μm) gneiss (59% quartz, 28% plagioclase, 13% aligned but not interconnected biotite) to determine the evolution of deformation mechanisms that produce dramatic strain weakening and localization, at conditions ( GPa Cited by: This book sets out the basic materials science needed for understanding the plastic deformation of rocks and minerals.

Although at atmospheric pressure or at relatively low environmental pressures, these materials tend to be brittle, that is, to fracture with little prior plastic deformation when non-hydrostatically stressed, they can undergo substantial permanent strain when stressed under.

Structural geology has developed at a very rapid pace in recent years. Evolution of Geological Structures in Micro- to Macro-Scales, covering a wide spectrum of current research in structural geology from the grain scale to the scale of orogenic belts and from the brittle to the ductile field, provides an overview of newly emerging concepts in a single volume.

The Rietveld refinement of diffraction data obtained from the polyphase rock requires the knowledge of the crystal structures of minerals composing this rock. For albite we used Downs et al.

(), amcsd No.for muscovite Catti et al. (), amcsd No. and for orthoclase Tseng et al. (), amcsd No. Cited by: 2. include polyphase and progressive ductile deformation, kinematic indicators in ductile shear zones, relationships between mesoscale and macroscale structures, micro textural analysis and fabric changes due to cataclasis, mylonitization, recrystallization and metamorphism.

A 5 days field course at the end of the semester is included. In appreciation of Hartmut Kern In appreciation of Hartmut Kern Mainprice, David; Wenk, Hans-Rudolf This special issue of Tectonophysics honors Hartmut Kern on the occasion of his retirement from teaching at the University of Kiel, Germany for his great contributions to rock deformation and petrophysics.

His experimental skills have advanced our understanding of. Bauer, P., Rosenberg, C.L, and M.R. Handy (): Deformation experiments on rock-analogue materials at controlled confining pressure: A new approach for studying strain localization at the brittle to viscous transition, Journal of Structural Geology, 22, 3, PDF.

Bauer, P., Rosenberg, C.L, and M.R. Handy (): Deformation experiments on rock-analogue materials at controlled confining pressure: A new approach for studying strain localization at the brittle to viscous transition, Journal of Structural Geology, 22, 3.

Shareable Link. Use the link below to share a full-text version of this article with your friends and colleagues. Learn more.The Zoovch Ovoo uranium deposit is located in East Gobi Basin in Mongolia. It is hosted in the Sainshand Formation, a Late Cretaceous siliciclastic reservoir, in the lower part of the post-rift infilling of the Mesozoic East Gobi Basin.

The Sainshand Formation corresponds to poorly consolidated medium-grained sandy intervals and clay layers deposited in fluvial-lacustrine by: 3.(). Experimental evidence for the dynamics of the formation of the Yinggehai basin, (). Extended models of transpression and transtension and application to tectonic setting: Continental Transtension and Transpression.

().Author: Suhaileen Shahar.