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      K-feldspar megacrysts in granites — Phenocrysts, not porphyroblasts

      Earth-Science Reviews

      Elsevier BV

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          Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone

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            Phenocryst-matrix partition coefficients for K, Rb, Sr and Ba, with applications to anorthosite and basalt genesis

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              An evaluation of criteria to deduce the sense of movement in sheared rocks

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                Author and article information

                Journal
                Earth-Science Reviews
                Earth-Science Reviews
                Elsevier BV
                00128252
                February 1986
                February 1986
                : 23
                : 1
                : 1-63
                Article
                10.1016/0012-8252(86)90003-6
                © 1986

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