Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins = Caractéristiques des éléments traces des grauwackes et détermination de la localisation tectonique des bassins sédimentairesBHATIA, M. R; CROOK, K. A. W.Contributions to mineralogy and petrology. 1986, Vol 92, Num 2, pp 181-193, issn 0010-7999Article

A DEFORMED POLYMICTIC CONGLOMERATE; THE INFLUENCE OF GRAIN SIZE AND COMPOSITION ON THE MECHANISM AND RATE OF DEFORMATION = UN CONGLOMERAT POLYGENIQUE DEFORME; L'INFLUENCE DE LA DIMENSION DE GRAIN ET DE LA COMPOSITION SUR LE MECANISME ET LA VITESSE DE DEFORMATIONETHERIDGE MA; VERNON RH.1981; TECTONOPHYSICS; ISSN 0040-1951; USA; DA. 1981; VOL. 79; NO 3-4; PP. 237-254Article

TIMING OF REGIONAL DEFORMATION IN THE HILL END TROUGH: DISCUSSION AND REPLYPACKHAM GH; POWELL CM; JONES JG et al.1978; J. GEOL. SOC. AUSTRAL.; AUS; DA. 1978; VOL. 25; NO 5-6; PP. 361-364; BIBL. 1 P.; 1 ILL.Article

HILL END TROUGH: NEW RADIOMETRIC AGES.CAS RAF; SHAW SE.1976; SEARCH; AUSTRAL.; DA. 1976; VOL. 7; NO 5; PP. 205-207; BIBL. 18 REF.; 10 ANAL.Article

A CRITICAL APPRAISAL OF THE TECTONIC HISTORY OF THE HILL END TROUGH AND ITS MARGINSPOWELL CM.1976; AUSTRAL. SOC. EXPLOR. GEOPHYSICSTS, BULL.; AUSTRAL.; DA. 1976; VOL. 7; NO 1; PP. 14-18; 2 ILL.; (CONF. GEOL. SOC. AUST., SPEC. GROUP INVEST. GENESIS ORE DEPOSITS; MACQUARIE UNIV., NORTH RYDE; 1975)Conference Paper

THE HILL END TROUGH: AN EMPIRICAL APPROACH.CAS R.1976; AUSTRAL. SOC. EXPLOR. GEOPHYSICISTS, BULL.; AUSTRAL.; DA. 1976; VOL. 7; NO 1; PP. 18; (CONF. GEOL. SOC. AUST., SPEC. GROUP INVEST. GENESIS ORE DEPOSITS; MACQUARIE UNIV., NORTH RYDE; 1975)Conference Paper

MICROSTRUCTURAL EVIDENCE OF TIME-RELATIONSHIPS BETWEEN METAMORPHISM AND DEFORMATION IN THE METASEDIMENTARY SEQUENCE OF THE NORTHERN HILL END TROUGH, NEW SOUTH WALES, AUSTRALIAVERNON RH; FLOOD RH.1979; TECHTONOPHYSICS; NLD; DA. 1979; VOL. 58; NO 1-2; PP. 127-137; BIBL. 9 REF.; 7 ILL.Article

PALEOZOIC INTERARC BASIN IN EASTERN AUSTRALIA AND A MODERN NEW ZEALAND ANALOGUECAS RAF; JONES JG.1979; NEW ZEAL. J. GEOL. GEOPHYS.; NZL; DA. 1979; VOL. 22; NO 1; PP. 71-85; BIBL. 3 P.; 10 ILL.Article

SILICIC LAVAS IN PALEOZOIC FLYSCHLIKE DEPOSITS IN NEW SOUTH WALES, AUSTRALIA: BEHAVIOR OF DEEP SUBAQUEOUS SILICIC FLOWSCAS R.1978; GEOL. SOC. AMER., BULL.; USA; DA. 1978; VOL. 89; NO 12; PP. 1708-1714; BIBL. 28 REF.; 7 ILL.; 9 ANAL.Article

TIMING OF REGIONAL DEFORMATION OF THE HILL END TROUGH: A REASSESSMENT.POWELL CM; EDGECOMBE DR; HENRY NM et al.1976; J. GEOL. SOC. AUSTRAL.; AUSTRAL.; DA. 1976; VOL. 23; NO 4; PP. 407-421; BIBL. 1 P. 1/2; 7 ILL.Article

TRACE-ELEMENT GEOCHEMISTRY AND SEDIMENTARY PROVINCES: A STUDY FROM THE TASMAN GEOSYNCLINE, AUSTRALIA = GEOCHIMIE DES ELEMENTS TRACES ET PROVINCES SEDIMENTAIRES: UNE ETUDE DU GEOSYNCLINAL TASMAN, AUSTRALIEBHATIA MR; TAYLOR SR.1981; CHEM. GEOL.; ISSN 0009-2541; NLD; DA. 1981; VOL. 33; NO 1-2; PP. 115-125; BIBL. 22 REF.; 2 TAB. ; ILL./TABL./ESQUISSEArticle

Significance of illite crystallinity and b_o values of K-white mica in low-grade metamorphic rocks, North Hill End Synclinorium, New South Wales, Australia = Signification de la cristallinité de l'illite et valeur b₀ d'un mica blanc à potassium, dans les roches de métamorphisme de basse température, North Hill End Synclinorium, Nouvelle Galles du Sud, AustralieOFFLER, R; PRENDERGAST, E.Mineralogical Magazine. 1985, Vol 49, Num 3, pp 357-364, issn 0026-461XArticle