-
(Table T40) Chemical composition of grain size fraction <0.001 mm sampled fro...
This dataset has no description
-
(Table T39) Parameter b of clay minerals sampled from basalts of alkaline and...
This dataset has no description
-
(Table T38) Secondary minerals in fine fraction sampled from alkaline series ...
This dataset has no description
-
(Table T37) Chemical composition of hawaiites from Hole 430A, Leg 55 (Ojin se...
This dataset has no description
-
(Table 2) Survey of Pacific Ocean DSDP sites for hiatuses PH and NH 1 through...
This dataset has no description
-
(Table 3) Projected ages of radiolarian events of DSDP Hole 55-433A in the we...
Ages were obtained from age/depth plots based on diatom, foraminifer, calcareous nannofossil and magnetostratigraphic events -
Age model of DSDP Hole 55-433A
This dataset has no description
-
Annotated record of the detailed examination of Mn deposits from DSDP Leg 55 ...
Leg 55 was conceived as part of the decade-long experiment to test the kinematic hot-spot hypothesis and several of its more imporant corollaries for the origin of the... -
(Table 4) Mineralogy at DSDP Leg 55 Holes
On Leg 55, cores were takenfrom three seamounts in the Emperor Seamount chain: Ojin, Nintoku, and Suiko Seamounts. At the drilling sites the water depth was 1300 to 1700 meters;... -
(Table 1) Bulk geochemistry of some lavas at DSDP Hole 55-433C
According to Wilson's (1963a, b) hypothesis, the volcanoes of the Hawaiian-Emperor Chain are formed as the Pacific lithospheric plate moves over a source of magma in the mantle.... -
(Table 1) Chemistry of two samples of the red weathered layer at DSDP Hole 55...
One argument for the subaerial formation of Nintoku Seamount in the Emperor chain is the occurrence of a red claystone interlayered between two basalt flows in Hole 432A.... -
(Table 1) Stabile isotopes at DSDP Leg 55 Holes
Deep sea drilling on four seamounts in the Emperor Seamount chain revealed that Paleogene shallow-water carbonate sediments of the "bryozoan-algal" facies crown the basalt... -
(Table S1) Diatom species richness from the Early Pleistocene to present
The extent to which the spatial distribution of marine planktonic microbes is controlled by local environmental selection or dispersal is poorly understood. Our ability to... -
(Table 1) Isotopic and trace-element ratios of Emperor Seamount basalts
When a mantle plume interacts with a mid-ocean ridge, both are noticeably affected. The mid-ocean ridge can display anomalously shallow bathymetry, excess volcanism, thickened... -
Global shallow sediment diagenesis survey results based on all available IODP...
Global shallow sediment diagenesis survey results based on all available IODP sediment core images.
