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NUMBER 19 13 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 (8-5)(14-l) (2-8) (4-3) (4-8) (3-8) (3-9) (5-7) (7-3) (4-1) (8-6) (14-10)(15-1)(6-1) (6-8) (15-2) (8-1) (7-1)(15-5) (15-15) 42.1 41.8 43.2 42.1 42.3 41.9 42.5 42.3 42.5 42.6 41.3 42.1 41.3 42.4 42.1 41.2 41.4 40.6 40.1 41.8 0.12
14 20 SMITHSONIAN CONTRIBUTIONS TO THE EARTH SCIENCES 20 40 60 30 FIGURE 9.—Ca-Mg-Fe diagram. X garnets from Buell Park A garnet inclusions in diamond FE
Page 1 and 2: SMITHSONIAN CONTRIBUTIONS TO THE EA
Page 3 and 4: Contents MINERALOGY COMPOSITION OF
Page 5 and 6: Constituent SiO TiO Al 0 fl 2 3 Cr
Page 7 and 8: PER CENT CBLCIUM FIGURE 3.—The ca
Page 9 and 10: Constituent TiO,, 2 2 3 FeO* MnO Mg
Page 11 and 12: 20 Cfl 40 .60 SMITHSONIAN CONTRIBUT
Page 13 and 14: 35'50' I L 6.. 3.. 2.. r FOKT DEFIA
Page 15: 12 SMITHSONIAN CONTRIBUTIONS TO THE
Page 19 and 20: 16 Constituent Si0 2 TiO2 A12O3 Cr
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Page 23 and 24: 20 40 20 SMITHSONIAN CONTRIBUTIONS
Page 25 and 26: Abyssal Basaltic Glasses as Indicat
Page 27 and 28: 24 Electron-M icroprobe Analysis An
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Page 33 and 34: 30 Hill in the NE Atlantic, and fro
Page 35 and 36: 32 cores the arrangement is stratig
Page 39 and 40: 36 ATLANTIC OCEAN LAT. LONG. DEPTH
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64 SMITHSONIAN CONTRIBUTIONS TO THE
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TABLE 1.—Chemical composition in
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82 Literature Cited Bostrom, K., an
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Geochemical Differences among Compo
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The St. Mary's County, Maryland, Ch
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100 SMITHSONIAN CONTRIBUTIONS TO TH
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Mineralogical and Chemical Composit
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108 Sampling Inclusion 1 was taken
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112 15 10 32 3.6 40 44 48 •fl-r O
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2.0- 1.5- 1.0 0.8 : 0.6: 0.4- 0.2-
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