WORLD-WIDE OCCURRENCE OF HFSE-DEPLETED MANTLE

[51] APPLICATIONS OF THE ION MICRO-PROBE TO GEOCHEMISTRY AND COSMOCHEMISTRY [J]. ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, 1982, 10 : 483 - 526

[52] GEOCHEMISTRY OF TRANSITION-ELEMENTS IN GARNET LHERZOLITE NODULES IN KIMBERLITES [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1978, 67 (01) : 41 - 50

[53] SHIMIZU N, 1974, CARNEGIE I WASH YB, V73, P964

[54] SHIMIZU N, 1987, EOS, V68, P447

[55] STERN CR, 1986, REV GEOL CHILE, V27, P41

[56] GEOCHEMISTRY AND MINERALOGY OF 2 SPINEL PERIDOTITE SUITES FROM DREISER-WEIHER, WEST-GERMANY [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1980, 44 (03) : 457 - 470

[57] CHEMICAL-COMPOSITION AND ORIGIN OF THE EARTHS PRIMITIVE MANTLE [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1982, 46 (02) : 179 - 192

[58] TERA F, 1986, GEOCHIM COSMOCHIM AC, V50, P535, DOI 10.1016/0016-7037(86)90103-1

[59] Thompson R.N., 1983, CONTINENTAL BASALT M, P158

[60] EXPERIMENTAL PETROLOGY OF NORMAL MORB NEAR THE KANE FRACTURE-ZONE - 22-DEGREES-25-DEGREES N, MID-ATLANTIC RIDGE [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1987, 96 (02) : 121 - 139

[51] APPLICATIONS OF THE ION MICRO-PROBE TO GEOCHEMISTRY AND COSMOCHEMISTRY [J]. ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, 1982, 10 : 483 - 526

[52] GEOCHEMISTRY OF TRANSITION-ELEMENTS IN GARNET LHERZOLITE NODULES IN KIMBERLITES [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1978, 67 (01) : 41 - 50

[53] SHIMIZU N, 1974, CARNEGIE I WASH YB, V73, P964

[54] SHIMIZU N, 1987, EOS, V68, P447

[55] STERN CR, 1986, REV GEOL CHILE, V27, P41

[56] GEOCHEMISTRY AND MINERALOGY OF 2 SPINEL PERIDOTITE SUITES FROM DREISER-WEIHER, WEST-GERMANY [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1980, 44 (03) : 457 - 470

[57] CHEMICAL-COMPOSITION AND ORIGIN OF THE EARTHS PRIMITIVE MANTLE [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1982, 46 (02) : 179 - 192

[58] TERA F, 1986, GEOCHIM COSMOCHIM AC, V50, P535, DOI 10.1016/0016-7037(86)90103-1

[59] Thompson R.N., 1983, CONTINENTAL BASALT M, P158

[60] EXPERIMENTAL PETROLOGY OF NORMAL MORB NEAR THE KANE FRACTURE-ZONE - 22-DEGREES-25-DEGREES N, MID-ATLANTIC RIDGE [J]. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 1987, 96 (02) : 121 - 139