EXTENSIONAL STRUCTURES IN ANISOTROPIC ROCKS

[1] [Anonymous], 1976, J GEOL SOC LONDON, DOI DOI 10.1144/GSJGS.132.2.0155

[2] ORTHOGNEISS, MYLONITE AND NON COAXIAL DEFORMATION OF GRANITES - EXAMPLE OF THE SOUTH-ARMORICAN-SHEAR-ZONE [J]. JOURNAL OF STRUCTURAL GEOLOGY, 1979, 1 (01) : 31 - 42

[3] BIOT A, 1965, MECHANICS INCREMENTA

[4] SP-MYLONITES - ORIGIN OF SOME MYLONITES BY SUPERPLASTIC FLOW [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1975, 50 (02) : 93 - 104

[5] DESCRIPTION AND ORIGIN OF BANDED DEFORMATION STRUCTURES .1. REGIONAL STRAIN, LOCAL PERTURBATIONS, AND DEFORMATION BANDS [J]. CANADIAN JOURNAL OF EARTH SCIENCES, 1977, 14 (08) : 1721 - 1731

[6] DEVELOPMENT OF INTERNAL STRUCTURES IN DEFORMED ANISOTROPIC ROCKS [J]. TECTONOPHYSICS, 1971, 12 (01) : 23 - &

[7] FOLD SHAPES AS FUNCTIONS OF PROGRESSIVE STRAIN [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1976, 283 (1312): : 129 - +

[8] DESCRIPTION AND ORIGIN OF BANDED DEFORMATION STRUCTURES .2. RHEOLOGY AND GROWTH OF BANDED PERTURBATIONS [J]. CANADIAN JOURNAL OF EARTH SCIENCES, 1977, 14 (11) : 2510 - 2523

[9] COMPATIBILITY EQUATIONS AND INTEGRATION OF FINITE STRAINS IN 2 DIMENSIONS [J]. TECTONOPHYSICS, 1977, 39 (04) : T1 - T6

[10] COBBOLD PR, 1976, B SOC GEOL FR, V18, P1497

[1] [Anonymous], 1976, J GEOL SOC LONDON, DOI DOI 10.1144/GSJGS.132.2.0155

[2] ORTHOGNEISS, MYLONITE AND NON COAXIAL DEFORMATION OF GRANITES - EXAMPLE OF THE SOUTH-ARMORICAN-SHEAR-ZONE [J]. JOURNAL OF STRUCTURAL GEOLOGY, 1979, 1 (01) : 31 - 42

[3] BIOT A, 1965, MECHANICS INCREMENTA

[4] SP-MYLONITES - ORIGIN OF SOME MYLONITES BY SUPERPLASTIC FLOW [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1975, 50 (02) : 93 - 104

[5] DESCRIPTION AND ORIGIN OF BANDED DEFORMATION STRUCTURES .1. REGIONAL STRAIN, LOCAL PERTURBATIONS, AND DEFORMATION BANDS [J]. CANADIAN JOURNAL OF EARTH SCIENCES, 1977, 14 (08) : 1721 - 1731

[6] DEVELOPMENT OF INTERNAL STRUCTURES IN DEFORMED ANISOTROPIC ROCKS [J]. TECTONOPHYSICS, 1971, 12 (01) : 23 - &

[7] FOLD SHAPES AS FUNCTIONS OF PROGRESSIVE STRAIN [J]. PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1976, 283 (1312): : 129 - +

[8] DESCRIPTION AND ORIGIN OF BANDED DEFORMATION STRUCTURES .2. RHEOLOGY AND GROWTH OF BANDED PERTURBATIONS [J]. CANADIAN JOURNAL OF EARTH SCIENCES, 1977, 14 (11) : 2510 - 2523

[9] COMPATIBILITY EQUATIONS AND INTEGRATION OF FINITE STRAINS IN 2 DIMENSIONS [J]. TECTONOPHYSICS, 1977, 39 (04) : T1 - T6

[10] COBBOLD PR, 1976, B SOC GEOL FR, V18, P1497