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EVIDENCE FOR CYCLIC REACTIONS BETWEEN ANDALUSITE, "SERICITE" AND SILLIMANITE, MOUNT FRANKS AREA, WILLYAMA COMPLEX, N.S.W.GLEN RA.1979; TECHTONOPHYSIKS; NLD; DA. 1979; VOL. 58; NO 1-2; PP. 97-112; BIBL. 15 REF.; 11 ILL.Article

REORIENTATION OF EARLY BIOTITES DURING SCHISTOSITY FORMATION IN ANDALUSITE SCHISTS, MOUNT FRANKS AREA, BROKEN HILL, N.S.W. = REORIENTATION DES BIOTITES PRECOCES DURANT LA FORMATION DE LA SCHISTOSITE DANS LES SCHISTES A ANDALOUSITE DE LA ZONE DU MONT FRANKS, BROKEN HILL, NOUVELLE GALLES DU SUDGLEN RA.1980; TECTONOPHYSICS; ISSN 0040-1951; NLD; DA. 1980; VOL. 68; NO 3-4; PP. 213-232; BIBL. 2 P.; 1 TAB. ; ILL./ESQUISSE/TABL.Article

THE STRUCTURE OF THE MT. FRANKS AREA, WILLYAMA COMPLEX, NEW SOUTH WALES.GLEN RA.sdIN: PROTEROZOIC GEOL. 1ST AUST. GEOL. CONV. ABSTR.; ADELAIDE; 1975; S.L.; , P. 30 A 31Miscellaneous

COMPONENT MIGRATION PATTERNS DURING THE FORMATION OF A METAMORPHIC LAYERING, MOUNT FRANKS AREA, WILLYAMA COMPLEX, N.S.W., AUSTRALIA = RESEAUX DE MIGRATION DES COMPOSANTS AU COURS DE LA STRATIFICATION METAMORPHIQUE, REGION MONT FRANKS, COMPLEXE WILLYAMA, NOUVELLE-GALLES DU SUD, AUSTRALIAGLEN RA.1982; J. STRUCT. GEOL.; ISSN 0191-8141; GBR; DA. 1982; VOL. 4; NO 4; PP. 457-467; BIBL. 16 REF.Article

LARGE-SCALE EARLY FOLDING AND TECTONIC LEVELS IN THE NORTHWESTERN PART OF THE WILLYAMA COMPLEX, NEW SOUTH WALESCORBETT GJ; GLEN RA.1979; GEOL. SURV. NEW SOUTH WALES, DEPT MINES, QUART. NOTES; AUS; DA. 1979; NO 34; PP. 1-5; BIBL. 4 REF.; 1 ILL.Article

CHRYSOTILE ASBESTOS AT WOODSREEF, NEW SOUTH WALES = LE CHRYSOTILE DE WOODSREEF, EN NOUVELLE GALLES DU SUDGLEN RA; BUTT BC.1981; ECON. GEOL. BULL. SOC. ECON. GEOL.; ISSN 0361-0128; USA; DA. 1981-08; VOL. 76; NO 5; PP. 1153-1169; BIBL. 36 REF.; 1 TAB. ; ILL.Article

NEPTUNITE FROM THE WOODSREEF SERPENTINITE, NEW SOUTH WALES: A NEW OCCURRENCESLANSKY E; GLEN RA.1982; TMPM. TSCHERMAKS MINERALOGISCHE UND PETROGRAPHISCHE MITTEILUNGEN; ISSN 0041-3763; AUT; DA. 1982; VOL. 30; NO 4; PP. 237-247; ABS. GER; BIBL. 2 P.Article

NEPTUNITE FROM THE WOODSREEF SERPENTINITE, NEW SOUTH WALES, AUSTRALIA: A NEW OCCURRENCE = NEPTUNITE DE LA SERPENTINITE DE WOODSREEF, NOUVELLE GALLES DU SUD, AUSTRALIE: UN NOUVEAU GISEMENTSLANSKY E; GLEN RA.1981; FORTSCHR. MINERAL., BEIH.; ISSN 0375-8931; DEU; DA. 1981; VOL. 59; NO 1; PP. 184-185; BIBL. 1 REF.Conference Paper

THE SIGNIFICANCE OF SEDIMENTARY STRUCTURES IN THE WILLYAMA COMPLEX, NEW SOUTH WALES.GLEN RA; LAING WP.1975; AUSTRALAS. INST. MING METALLURGY, PROC.; AUSTRAL.; 1975, NUM. 0256, P. 15 A 20Serial Issue

THE STRUCTURE AND TECTONIC EVOLUTION OF THE BROKEN HILL REGION, AUSTRALIA = STRUCTURE ET EVOLUTION TECTONIQUE DE LA REGION BROKEN HILL, AUSTRALIEMARJORIBANKS RW; RUTLAND RWR; GLEN RA et al.1980; PRECAMBRIAN RES.; ISSN 0301-9268; NLD; DA. 1980; VOL. 13; NO 2-3; PP. 209-240; BIBL. 2 P.Article

TECTONIC RELATIONSHIP BETWEEN THE PROTEROZOIC GAWLER AND WILLYAMA OROGENIC DOMAINS, AUSTRALIA.GLEN RA; LAING WP; PARKER AJ et al.1977; J. GEOL. SOC. AUSTRAL.; AUSTRAL.; DA. 1977; VOL. 24; NO 3; PP. 125-150; BIBL. 3 P.; 11 ILL.Article

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