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(Table 5) Major-elements from DSDP Holes 61-462, 61-462A and 33-315A
FeO recalculated as Fe2O3 in analyses from DSDP Site 61-462. Note the strong chemical similarity between the two sets of claystones. -
(Table 3) Geochemistry of Ontong Java Plateau basalts
For INAA data, precision was determined from eight replicate analyses of Standard BOB-1, except for Sc, for which six replicates were analyzed. Precisions, as estimated by... -
(Table AT34) Abundance of major and trace elements in basalts from Hole 317A,...
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(Table T68) Chemical composition of basalts from Hole 317A, Leg 33 (Manihiki ...
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(Table 2) Nd, Sm, Sr, Rb, and isotopic analyses of microtektites in DSDP sites
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(Table 1) Upper Eocene microtektites in DSDP sites
Sample 33-315-10-6,41-47 includes 547 microspherules from the >54 micron fraction -
(Table 2) Nd and Sr isotope ratios of oceanic crust from DSDP Hole 33-317A
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(Table 1) Pb isotope ratios of oceanic crust from DSDP Hole 33-317A
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(Table 1) Geochemistry and Sr isotopic composition of interstitial waters of ...
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(Table 1) Organic carbon content and stable carbon isotope ratios, and hydrog...
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(Appendix 3) Chemical composition of carbonate free sediments from DSDP Holes...
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(Appendix 3) Chemical composition of carbonate free sediments from DSDP Hole ...
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(Appendix 3) Chemical composition of carbonate free sediments from DSDP Hole ...
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(Appendix 2) Chemical composition of bulk sediments from DSDP Hole 33-317A
Data have been corrected for pore fluid contents -
(Table 13) Distribution of Oligocene to Miocene radiolarians in DSDP Hole 33-...
Species abundance: C = common, F = few, R = rare, + = single specimen, ? = dubious identification, - = searched for and not found -
(Table 12) Distribution of Oligocene to Miocene radiolarians in DSDP Hole 33-...
Species abundance: C = common, F = few, R = rare, + = single specimen, ? = dubious identification, - = searched for and not found, ! = reworked or downworked specimens -
Age model of DSDP Hole 33-317B
This dataset has no description
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(Table DR1) Trace element contents in basalts from ODP Hole 33-317A
Numerous large igneous provinces formed in the Pacific Ocean during Early Cretaceous time, but their origins and relations are poorly understood. We present new geochronological... -
Diversity of benthic foraminiferal faunas in Tertiary and Quaternary sediment...
A study is made of the benthic foraminifers (size fraction > 63 µm) recovered from 59 upper Eocene through Quaternary sediment samples at DSDP Site 317 (Leg 33), located at a...