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(Table 1) Carbon and lipids at DSDP Hole 61-462
The lipids of a Pliocene and a Cretaceous sample from Site 462 were analyzed to assess their source and diagenetic history. Judging from the distributions of the n-alkanes,... -
(Table 1) Interstitial-water chemistry at DSDP Hole 61-462
Concentration gradients of Ca, Mg, K, Sr, and Li at Site 462, Leg 61, are linear with depth; large changes occur in the unsampled, low-porosity limestone-chert zone between 375... -
Interstitial water chemistry of Hole 61-462, raw data
Values are taken directly from the chemistry technicians shipboard notebook. -
(Table 2) Nitrogen concentrations and isotopic compositions of samples from D...
This dataset has no description
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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... -
Cadmium contents in bottom sediments and sedimentary rocks from DSDP Holes 3-...
This dataset has no description
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(Table 2) Survey of Pacific Ocean DSDP sites for hiatuses PH and NH 1 through...
This dataset has no description
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Magnetic properties of the oceanic igneous rocks (Table 1)
Hysteresis measurements have been carried out on a suite of ocean-floor basalts with ages ranging from Quaternary to Cretaceous. Approximately linear, yet separate,... -
Chemical composition of bottom sediments and rocks from DSDP Holes 3-14 throu...
Data on analyses of chemical composition of DSDP samples of bottom sediments and rocks carried out in P.P. Shirshov Institute of Oceanology are reported. Basal sediments and... -
Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes
Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of... -
Magnetic properties of Cenozoic MORB and Cretaceous MORB from DSDP and ODP holes
The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt (MORB) samples shows systematic variations as a function of age has long been... -
Nitrogen isotopic composition and chemical composition of altered oceanic cru...
Knowledge of the subduction input flux of nitrogen (N) in altered oceanic crust (AOC) is critical in any attempt to mass-balance N across arc-trench systems on a global or... -
(Table 1) Isotopic Ar and ages at DSDP Holes 61-462 and 61-462A
Empty cells = no data. -
(Table 2b) Isotopic composition of Xe of pillow lava in DSDP sites
This dataset has no description
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(Table 2a) Isotopic composition of He, Ne, Ar and Kr of pillow lava in DSDP s...
This dataset has no description
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Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
(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... -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 61 ...
The goal of Site 462 was to study the paleontologic, sedimentary, petrologic, tectonic, and magnetic histories of that area through Recent to Late Jurassic time by drilling a... -
Chemical composition of sedimentary rocks from DSDP Hole 61-462
This dataset has no description
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(Table 1) Sr isotopes and chemical composition of DSDP Hole 61-462A basalts
Sixteen elemental abundances and 87Sr/86Sr ratio of the Nauru Basin basalt (Cores 75 to 90: sub-bottom depths 950 m to 1050 m) from Hole 462A have been determined by inductively...
