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• W2085776977 abstract "Research Article| January 01, 2000 Mesoscopic Twin Patterns in Ferroelastic and Co-Elastic Minerals Ekhard K. H. Salje Ekhard K. H. Salje Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ U.K. Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2000) 39 (1): 65–84. https://doi.org/10.2138/rmg.2000.39.03 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Ekhard K. H. Salje; Mesoscopic Twin Patterns in Ferroelastic and Co-Elastic Minerals. Reviews in Mineralogy and Geochemistry 2000;; 39 (1): 65–84. doi: https://doi.org/10.2138/rmg.2000.39.03 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Minerals are often riddled with microstructures when observed under the electron microscope. Although the observation and classification of microstructures such as twin boundaries, anti-phase boundaries, exsolution lamellae etc., has been a longstanding activity of mineralogists and crystallographers it has only been very recently that we started to understand the enormous importance of microstructures for the physical and chemical behaviour of minerals. Let us take a twin boundary as an example. Illustrations of twinned minerals have decorated books on mineralogy for more than a century. A first major step forward was made when Burger (1945) noticed that twinning can have different... You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2085776977 date "2000-01-01" @default.
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• W2085776977 title "Mesoscopic Twin Patterns in Ferroelastic and Co-Elastic Minerals" @default.
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