ARE STRONGLY PERALUMINOUS MAGMAS DERIVED FROM PELITIC SEDIMENTARY SOURCES

[1] Abbott RN, 1981, CAN MINERAL, V19, P103

[2] ABBOTT RN, 1982, AM MINERAL, V67, P865

[3] ABBOTT RN, 1979, CAN MINERAL, V17, P549

[4] THE GROWTH OF THE CONTINENT THROUGH GEOLOGICAL TIME STUDIED BY ND ISOTOPE ANALYSIS OF SHALES [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1984, 67 (01) : 19 - 34

[5] ND-SR ISOTOPIC RELATIONSHIP IN GRANITOID ROCKS AND CONTINENTAL-CRUST DEVELOPMENT - A CHEMICAL APPROACH TO OROGENESIS [J]. NATURE, 1980, 286 (5771) : 335 - 342

[6] Anderson JL, 1981, CAN MINERAL, V19, P83

[7] [Anonymous], 1977, J GEOL SOC LOND, DOI DOI 10.1144/GSJGS.133.6.0559

[8] [Anonymous], 1968, CONTRIB MINERAL PETR, DOI DOI 10.1007/BF00371729

[9] CONTRASTING O-18-ENRICHMENT AND ORIGINS OF HIGH HIMALAYAN AND TRANSHIMALAYAN INTRUSIVES [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1983, 65 (02) : 276 - 286

[10] BROWN GC, 1984, J GEOL SOC LONDON, V141, P411

[1] Abbott RN, 1981, CAN MINERAL, V19, P103

[2] ABBOTT RN, 1982, AM MINERAL, V67, P865

[3] ABBOTT RN, 1979, CAN MINERAL, V17, P549

[4] THE GROWTH OF THE CONTINENT THROUGH GEOLOGICAL TIME STUDIED BY ND ISOTOPE ANALYSIS OF SHALES [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1984, 67 (01) : 19 - 34

[5] ND-SR ISOTOPIC RELATIONSHIP IN GRANITOID ROCKS AND CONTINENTAL-CRUST DEVELOPMENT - A CHEMICAL APPROACH TO OROGENESIS [J]. NATURE, 1980, 286 (5771) : 335 - 342

[6] Anderson JL, 1981, CAN MINERAL, V19, P83

[7] [Anonymous], 1977, J GEOL SOC LOND, DOI DOI 10.1144/GSJGS.133.6.0559

[8] [Anonymous], 1968, CONTRIB MINERAL PETR, DOI DOI 10.1007/BF00371729

[9] CONTRASTING O-18-ENRICHMENT AND ORIGINS OF HIGH HIMALAYAN AND TRANSHIMALAYAN INTRUSIVES [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1983, 65 (02) : 276 - 286

[10] BROWN GC, 1984, J GEOL SOC LONDON, V141, P411