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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... -
(Table 2) Trace element concentrations of selected Cocos Plate samples
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Geochemistry of interstitial water of ODP Hole 206-1256C
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Geochemistry of interstitial water of ODP Hole 206-1256B
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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... -
C and H geochemistry of altered oceanic crus of ODP/IODP Hole 1256D
Carbon and hydrogen concentrations and isotopic compositions were measured in 19 samples from altered oceanic crust cored in ODP/IODP Hole 1256D through lavas, dikes down to the... -
Nannofossil biostratigraphy of ODP Hole 206-1256B sediments
Site 1256 of Ocean Drilling Program Leg 206 to the Guatemala Basin on the eastern flank of the East Pacific Rise yielded a near-complete, middle Miocene-Quaternary... -
Chemical composition of secondary minerals from ODP Site 206-1256
Two basement holes were drilled during Ocean Drilling Program (ODP) Leg 206. Hole 1256C penetrates 88.5 m into basement and Hole 1256D, ~30 m to the south, penetrates 502 m into... -
Chemical composition of hydrogarnet and celadonite from ODP Hole 206-1256D
Mid-ocean-ridge basalts recovered from Hole 1256D during Ocean Drilling Program Leg 206 exhibit the effects of various low-temperature (<100°C) alteration processes,... -
Major element oxides of minerals from a lava pond at ODP Site 206-1256
At Ocean Drilling Program Site 1256 (6°44.2'N, 91°56.1'W), during Leg 206, a thick massive unit was cored in two neighboring penetrations of the uppermost basement, Holes 1256C... -
Grain sizes and mineral composition of the basement of ODP Site 206-1256
Hole 1256C was cored 88.5 m into basement, and Hole 1256D, the deep reentry hole, was cored 502 m into basement during Ocean Drilling Program Leg 206. Hole 1256D is located ~30... -
Sediment geochemistry of ODP Holes 206-1256B and 206-1256C
We measured the chemical composition of 100 samples from the 250-m sediment sequence retrieved from Ocean Drilling Program Site 1256 in the Guatemala Basin using a newly... -
Geochemistry of oceanic crust of the Cocos Plate
New geochemical data from the Cocos Plate constrain the composition of the input into the Central American subduction zone and demonstrate the extent of influence of the... -
Element concentrations of aluminosilicate components from ODP sites in the Pa...
We measured major and trace element concentrations in the operationally defined, chemically extracted, residual aluminosilicate component of sediment from Ocean Drilling Program... -
P-wave velocity (PWS split-core system) on ODP Hole 206-1256D
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P-wave velocity (PWS split-core system) on ODP Hole 206-1256C
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P-wave velocity (PWS split-core system) on ODP Hole 206-1256B
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P-wave velocity (PWS split-core system) on ODP Hole 206-1256A
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Thermal conductivity of ODP Hole 206-1256D
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Thermal conductivity of ODP Hole 206-1256C
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