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Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
Nannofossil abundance of Hole 66-493B
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-493A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-493
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-492
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-491
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-490
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-489A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-489
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-488
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-487
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-486A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 66-486
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Supplement EA2) Hafnium isotope ratios and major elements from Central Mexic...
Isotope ratio normalizations are outlined in Table (Supplement EA1). Pb-Nd-Sr isotope ratios, major and trace element concentrations are reported in LaGatta (2003) and LaGatta... -
(Table 3) Trace elements at DSDP Hole 66-487
Empty cells mean no data. -
(Table 2) Geochemistry of minerals from DSDP Sample 66-487-20-1,55-58
Concentrations lower than 0.1% are not considered representative. Empty cells mean no data. -
(Table 1) Basalt from DSDP Hole 66-487: Major elements and minerals
The CIPW norms are calculated with 85% of total iron as FeO and 15% as Fe2O3 (total Fe analysis is given as Fe2O3). Empty cells mean no data. -
(Table 5) Radiometric K-Ar analyses at DSDP Hole 66-493
This dataset has no description
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(Table 4) Major oxides in the dioritic pluton at DSDP Hole 66-493
Analysts are R. Duret and A. Pantaloni. -
(Table 3) Geochemistry of feldspar at DSDP Sample 66-493-59-1A
TiO2 and MgO contents have been found equal to zero in all the cases.
