TECTONICALLY DEFORMED PILLOW LAVA AS AN INDICATOR OF BEDDING AND WAY-UP = PILLOW LAVA TECTONIQUEMENT DEFORME COMME INDICATEUR DU SENS ET DE L'ORIENTATION DES COUCHESBORRADAILE GJ.1982; J. STRUCT. GEOL.; ISSN 0191-8141; GBR; DA. 1982; VOL. 4; NO 4; PP. 469-479; 10 P.; BIBL. 6 REF.Article

COMPACTION ESTIMATE LIMITS FROM SAND DIKE ORIENTATIONS.BORRADAILE GJ.1977; J. SEDIMENT. PETROL.; U.S.A.; DA. 1977; VOL. 47; NO 4; PP. 1598-1601; BIBL. 5 REF.; 3 ILL.Article

I. DALRADIAN STRUCTURE AND STRATIGRAPHY OF THE NORTHERN LOCK AWE DISTRICT, ARGYLLSHIREBORRADAILE GJ.1972; TRANS. R. SOC. EDINBURGH; G.B. ; 1972,1973, VOL. 69, NUM. 0001, P. 1 A 21Serial Issue

"STRUCTURAL FACING" (SHACKLETON'S RULE) AND THE PALAEOZOIC ROCKS OF THE MALAGUIDE COMPLEX NEAR VELEZ RUBIO, SE SPAIN.BORRADAILE GJ.1976; PROC. KKL. NEDERL. AKAD. WETENSCH., B; NETHERL.; DA. 1976; VOL. 79; NO 5; PP. 330-336; H.T. 4; BIBL. 15 REF.; 7 ILL.Article

PARTICULATE FLOW, FOLDS, CLEAVAGE AND MAGNETIC FABRICS = ECOULEMENT DES PARTICULES, PLIS, CLIVAGE TECTONIQUE ET STRUCTURES MAGNETIQUESBORRADAILE GJ.1982; J. STRUCT. GEOL.; ISSN 0191-8141; GBR; DA. 1982; VOL. 4; NO 2; PP. 231Conference Paper

MINIMUM STRAIN FROM CONGLOMERATES WITH DUCTILITY CONTRAST = DEFORMATION MINIMUM A PARTIR DE CONGLOMERATS PRESENTANT DES CONTRASTES DE DUCTILITEBORRADAILE GJ.1981; J. STRUCT. GEOL.; ISSN 0191-8141; GBR; DA. 1981; VOL. 3; NO 3; PP. 295-297; BIBL. 12 REF.; ILL.Article

TRANSECTED FOLDS: A STUDY ILLUSTRATED WITH EXAMPLES FROM CANADA AND SCOTLAND = PLIS DISSEQUES: UNE ETUDE ILLUSTREE D'EXEMPLES DU CANADA ET D'ECOSSEBORRADAILE GJ.1978; GEOL. SOC. AMER. BULL.; ISSN 0016-7606; USA; DA. 1978; VOL. 89; NO 4; PP. 481-493; BIBL. 1 P.; ILL./BLOC DIAGR.Article

ON CLEAVAGE AND STRAIN: RESULTS OF A STUDY IN WEST GERMANY USING TECTONICALLY DEFORMED SAND DYKES.BORRADAILE GJ.1977; J. GEOL. SOC.; G.B.; DA. 1977; VOL. 133; NO 2; PP. 146-164; BIBL. 2 P.; 15 ILL.Article

THERMAL ANISOTROPY - A FACTOR CONTRIBUTING TO THE DISTRIBUTION OF CALEDONIAN METAMORPHIC ZONES IN THE SW SCOTTISH HIGHLANDS.BORRADAILE GJ.1976; GEOL. EN MIJNBOW; NEDERL.; 1976, VOL. 55, NUM. 0001-0002, P. 41 A 45Serial Issue

VARIABLY ORIENTED CO-PLANAR PRIMARY FOLDSBORRADAILE GJ.1972; GEOL. MAG.; G.B. ; 1972, VOL. 109, NUM. 0002, P. 89 A 98Serial Issue

THE GEOLOGICAL SIGNIFICANCE OF MAGNETIC ANOMALIES IN THE REGION OF ISLAY.WESTBROOK GK; BORRADAILE GJ.1978; SCOTT. J. GEOL.; G.B.; DA. 1978; VOL. 14; NO 3; PP. 213-224; BIBL. 1 P.; 6 ILL.Article

FINITE STRAIN ESTIMATES FROM THE DABRADIAN DOLOMITIC FORMATION, ISLAY, ARGYLL, SCOTLANDBORRADAILE GJ; JOHNSON HD.1973; TECTONOPHYSICS; NETHERL ; 1973, VOL. 18, NUM. 0003-0004, P. 249 A 259Serial Issue

THE LOCH NANT AREA, ARGYLLSHIRE, AND ITS SIGNIFICANCE IN THE STRUCTURAL HISTORY OF THE LOCH AWE SYNCLINEBORRADAILE GJ; ROBERTS JL; TREAGUS JE et al.1971; SCOTT. J. GEOL.; G.B. ; 1971, VOL. 7, NUM. 0001, P. 79 A 85Serial Issue