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Chemical composition of basal bottom sediments from DSDP Hole 17-170
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Chemical composition of bottom sediments from DSDP Holes 17-165A and 17-167
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(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
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(Table 3) Rubidium and strontium concentrations and isotope ratios of DSDP ho...
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(Figure 3b) Distribution of abundance of calcareous nannofossils at Site 17-167
Quantification of species abundance is as follows: rare: <5 specimens observed; few: 5-10 specimens; common: 10-50 specimens; abundant: >50specimens observed. -
(Appendix 2) Isotopic composition of foraminifera from sediments of DSDP Legs...
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(Table 2) Survey of Pacific Ocean DSDP sites for hiatuses PH and NH 1 through...
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(Appendix 1) Biostratigraphy and Sr isotopic composition of sediments from DS...
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(Table 3) Atomic ratios of sediments from DSDP Site 17-164
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(Table 2) Chemical composition of sediments from DSDP Site 17-164
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(Table 1) Description of sediments from DSDP Site 17-164
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(Table 3) Rare earth and trace element contents in DSDP and ODP cherts
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(Table 1-2) Sample summary and major element contents in DSDP and ODP cherts
Contents are given on volatile free base -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 17 ...
The main objectives of Leg 17 were to establish the regional pattern of oceanic crustal ages in the central Pacific, to obtain cores of the entire stratigraphic succession,... -
Pacific Neogene carbonate accumulation rates
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drilling Project and Ocean Drilling Program drill sites in the Pacific in order to... -
(Table 1) Biostratigraphic zonation and core depth of microtektite occurrence...
Microtektites have been recovered from three horizons in eight middle Eocene to middle Oligocene marine sediment sequences. Five of these occurrences are coeval and of latest... -
Isotopic composition of carbon and oxygen from Paleogene deposits of some Pac...
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(Table DR1) Biogenic silica and chert in the Pacific Ocean, DSDP and ODP data
Evidence for the dissolution of biogenic silica at the base of pelagic sections supports the hypothesis that much of the chert formed in the Pacific derives from the dissolution... -
Minor-element chemical analyses of Hole 17-170
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Minor-element chemical analyses of Hole 17-169
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