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RECOGNITION OF THE ORIGINAL VOLCANIC SUITE IN ALTERED MAFIC VOLCANIC ROCKS AT SOFALA, NEW SOUTH WALES.BARRON BJ.1976; AMER. J. SCI.; U.S.A.; 1976, VOL. 276, NUM. 0005, P. 604 A 636Serial Issue

THE USE OF COEXISTING CALCITE-ANKERITE SOLID SOLUTIONS AS A GEOTHERMOMETER.BARRON BJ.1974; CONTRIB. MINERAL. PETROL.; DEU; 1974, VOL. 47, NUM. 0001, P. 77 A 80Serial Issue

THE GEOCHEMISTRY OF AN INVARIANT POINT IN THE METAMORPHOSED BASIC VOLCANICS AT SOFALA, NEW SOUTH WALESBARRON LM; BARRON BJ.1978; CHEM. GEOL.; NLD; DA. 1978; VOL. 23; NO 3; PP. 193-213; BIBL. 25 REF.; 8 ILL.Article

AN ALGORITHM FOR THE COMPUTER ARRANGEMENT OF REACTIONS ABOUT INVARIANT POINTS.BARRON LM; BARRON BJ.1977; CONTRIB. MINERAL. PETROL.; GERM.; DA. 1977; VOL. 62; NO 1; PP. 103-107; BIBL. 7 REF.; 4 ILL.Article

A MODEL FOR GREENSCHIST FACIES EQUILIBRIA IN ALTERED MAFIC VOLCANIC ROCKS AT SOFALA, NEW SOUTH WALES.BARRON BJ; BARRON LM.1976; AMER. J. SCI.; U.S.A.; 1976, VOL. 276, NUM. 0005, P. 637 A 669Serial Issue

A DISMEMBERED OPHIOLITE SUITE AT PORT MACQUARIE, NEW SOUTH WALES.BARRON BJ; SCHEIBNER E; SLANSKY E et al.1976; REC. GEOL. SURV. NEW S. WALES; AUSTRAL.; DA. 1976; VOL. 18; NO 1; PP. 69-102; H.T. 13; BIBL. 17 REF.; 18 ILL.Article

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