ORIENTATION OF MINERAL LINEATION ALONG FLOW DIRECTION IN ROCKS

[1] CAREY SW, 1954, J GEOL SOC AUST, V1, P67, DOI DOI 10.1080/14400955308527848

[2] CLOOS H, 1946, GEOL SOC AM MED, V18

[3] CLOOS H, 1928, FORTSCHR GEOL PALAON, V7, P1

[4] EIRICH FR, 1956, RHEOLOGY THEORY A ED, V1, P653

[5] The motion of ellipsoidal particles in a viscous fluid [J]. PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-CONTAINING PAPERS OF A MATHEMATICAL AND PHYSICAL CHARACTER, 1922, 102 (715) : 161 - 179

[6] PARTICLE MOTIONS IN SHEARED SUSPENSIONS .2. COLLISIONS OF UNIFORM SPHERES [J]. JOURNAL OF COLLOID SCIENCE, 1952, 7 (04): : 354 - 369

[7] MASON SG, 1959, SUSPENDED PARTICLES

[8] Oldroyd J.G., 1956, RHEOLOGY, P653

[9] CONTINENTAL DRIFT + ORIGIN OF MOUNTAINS - HOT CREEP + CREEP FRACTURE ARE CRUCIAL FACTORS IN FORMATION OF CONTINENTS + MOUNTAINS [J]. SCIENCE, 1964, 146 (364) : 1003 - &

[10] SCHMIDT W, 1932, TEKTONIK VERFORMUNGS

[1] CAREY SW, 1954, J GEOL SOC AUST, V1, P67, DOI DOI 10.1080/14400955308527848

[2] CLOOS H, 1946, GEOL SOC AM MED, V18

[3] CLOOS H, 1928, FORTSCHR GEOL PALAON, V7, P1

[4] EIRICH FR, 1956, RHEOLOGY THEORY A ED, V1, P653

[5] The motion of ellipsoidal particles in a viscous fluid [J]. PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-CONTAINING PAPERS OF A MATHEMATICAL AND PHYSICAL CHARACTER, 1922, 102 (715) : 161 - 179

[6] PARTICLE MOTIONS IN SHEARED SUSPENSIONS .2. COLLISIONS OF UNIFORM SPHERES [J]. JOURNAL OF COLLOID SCIENCE, 1952, 7 (04): : 354 - 369

[7] MASON SG, 1959, SUSPENDED PARTICLES

[8] Oldroyd J.G., 1956, RHEOLOGY, P653

[9] CONTINENTAL DRIFT + ORIGIN OF MOUNTAINS - HOT CREEP + CREEP FRACTURE ARE CRUCIAL FACTORS IN FORMATION OF CONTINENTS + MOUNTAINS [J]. SCIENCE, 1964, 146 (364) : 1003 - &

[10] SCHMIDT W, 1932, TEKTONIK VERFORMUNGS