Biblioteca Digital

372 resultados para Park Ridge

(Table 6) Chemical composition of chrome spinelides from peridotides of the Mid-Atlantic Ridge

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(Table 2) Reconstructed primary modal compositions of representative ODP Hole 209-1274A peridotites, Mid-Atlantic Ridge

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Calculated abundance and biomass of Ophiocten gracilis at different stations on Kolbeinsey Ridge

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(Table 2) Pliocene and Pleistocene diatom biostratigraphy of ODP Site 177-1089 from the northen flank of the Agulhas Ridge, South Atlantic

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(Table Ia) Planktic foraminifera abundances in the latest Cretaceous sample interval of DSDP Hole 74-528 on the Walvish Ridge, South Atlantic

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(Table 3) Pliocene and Pleistocene diatom biostratigraphy of ODP Site 177-1090 from the southern flank of the Agulhas Ridge, South Atlantic

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(Table 10/11) Chemical composition of Fe-Mn crusts dredged at the Mid-Atlantic Ridge 5-7°N

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Geochemical analysis of sediment profile at station M57/3_203 from Walvis Ridge

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(Table 2) Estimated ages and plankronic foraminiferal biostratigraphy of the late Campanian and Maastrichtian section of DSDP Hole 74-525A from the Walvis Ridge, South Atlantic

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(Table 2.6) Rare earth element contents in metalliferous sediments of Core AMK15-1891 from the TAG Hydrothermal Field, Mid-Atlantic Ridge 26°N

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(Table AT48) Abundance of major and trace elements in basalts from Hole 525A, Leg 74 (Walvis Ridge, Atlantic Ocean)

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(Appendix) Stable carbon and oxygen isotope ratios of fine-fraction sediments across the Cretaceous/Tertiary boundary of DSDP Hole 74-525A from Walvis Ridge, South Atlantic

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(Appendix) Stable carbon and oxygen isotope ratios of fine-fraction sediments across the Cretaceous/Tertiary boundary of DSDP Hole 74-527 from Walvis Ridge, South Atlantic

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(Appendix) Stable carbon and oxygen isotope ratios of fine-fraction sediments across the Cretaceous/Tertiary boundary of DSDP Hole 74-529 from Walvis Ridge, South Atlantic

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(Table AT15) Abundance of major and trace elements in basalts from Hole 332B, Leg 37 (Deep Drill Valley, Mid-Atlantic Ridge)

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