Biblioteca Digital

38 resultados para DFT CALCULATION

Planktonic foraminiferal assemblages and SST calculation of sediment core TAN1106/34

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Planktonic foraminiferal assemblages and SST calculation of sediment core TAN1106/89

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Planktonic foraminiferal assemblages and SST calculation of sediment surface samples of the Solander Trough, New Zealand

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Planktonic foraminiferal assemblages and SST calculation of sediment core TAN0803/9

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Planktonic foraminiferal assemblages and SST calculation of sediment core TAN1106/43

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(Appendix C) Stable isotope ratios and paleotemperature calculation of selected planktonic foraminifera from Maastrichtian sediments of DSDP Hole 74-525A from Walvis Ridge, South Atlantic

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Stable oxygen isotope and Mg/Ca ratios of planktonic foraminifera, and SST calculation for ODP Hole 165-999A

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4.5. Principal Component Analysis calculation of best fit line for multiple demagnetization steps in order to determine the inclination and declination of SLW1 sediment cores

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(Figure 3) Alkenones, unsaturation index UK`37 and calculation of sea surface temperatures of sediment core GeoB3910-2 from the northeastern Brazil continental slope

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(Table 2) Age calculation and calcite concentration from IODP Hole 310-M0005D

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Interpolated temperature of water used for calculation of sea surface temperatures

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(Table 2) Boundary conditions used for the calculation of relative contributions from available carbon sources to the total carbon pool at Chapopote

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(Table A1) Stable isotope ratios and paleotemperature calculation of selected planktonic foraminifera from late Campanian and Maastrichtian sediments of DSDP Hole 86-577A from the Shatsky Rise, North Pacific

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(Table A1) Stable isotope ratios and paleotemperature calculation of selected planktonic foraminifera from late Campanian and Maastrichtian sediments of DSDP Hole 74-525A from the Walvis Ridge, South Atlantic

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(Supplementary Table A ) Locations employed for calculation of continental environmental conditions with WebWIMP Modelling program and values obtained as displayed in Fig. 1

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