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Paleontological investigation on diatoms of ODP Hole 151-908A
This dataset has no description
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Biostratigraphy and magnetostratigraphy of ODP Leg 124 sites
During ODP Leg 124, late middle Eocene to Quaternary sediment sequences were recovered from 13 holes drilled at five sites in the Celebes and Sulu basins. Paleomagnetic... -
Miocene radiolarians of the Sulu Sea
Radiolarians are sporadic in sediments collected in the Sulu Sea during ODP Leg 124. Due to the generally poor preservation and low abundance of radiolarians in Sulu Sea... -
Radiolarians of the Celebes Sea
Two sites were drilled in the Celebes Sea as part of Ocean Drilling Program Leg 124; Site 767 and Site 770. Radiolarians are preserved in Paleogene pelagic claystones with minor... -
Age model of the ANDRILL AND1-1B drill core, 382.38 to 459.19 m
Age model developed for samples analyzed in: Monien, Donata and Kuhn, Gerhard (2008, doi:10.1594/PANGAEA.708148) -
Physical properties of the ANDRILL AND1-1B drill core, 382.26 to 459.76 m
Wet bulk density and porosity data taken from: Niessen, F., D. Magens, and A. C. Gebhardt (2007, hdl:10013/epic.30000.d001). See doi:10.1594/PANGAEA.676905 for data. Dry bulk... -
Physical properties and abundance of diatoms of the ANDRILL AND1-1B drill core
In the austral summer of 2006/7 the ANDRILL MIS (ANtarctic geological DRILLing- McMurdo Ice Shelf) project recovered a 1285 m sediment core from beneath the Ross Ice Shelf near... -
Chronostratigraphy of sediment core CRP-2/2A (Table 1)
The 624.15 m glaciomarine sedimentary succession recovered in the CRP-2/2A drillcore comprises lower Oligocene (1000 m/m.y.). Between 306.65 mbsf and the bottom of the drillcore... -
Occurence of diatoms in sediment core CRP-1 (Table 1)
This dataset has no description
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Diatom abundance in sediment core CRP-2/2A (Table1)
Depth is top of 1 cm thick sample; B=Barren: no diatom valves or fragments present. T = Trace/reworked: rare fragments present. R = Rare: 1 complete valve in 5-30 fields of... -
4.2. Bulk density and magnetic susceptibility of sediment core SLW1_SLW_MC1A
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.1. High resolution XRF elemental composition of sediment core SLW1_SLW_MC3A
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.1. High resolution XRF elemental composition of sediment core SLW1_SLW_MC1A
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.1. High resolution XRF elemental composition of sediment core SLW1_PC1
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.3. Particle size distributions of SLW1 sediment cores
5 grams of sediment was crushed and dry-sieved to remove gravel (>2 mm). Depending on grain size of the sediment, 0.2 to 5 grams of sieved sample was transferred into a glass... -
4.5. Anisotropy of magnetic susceptibility of SLW1 sediment cores
AMS results. Columns K1, K2, K3 are all dimensionless ratios that describe the magnitude of each axis of the magnetic susceptibility ellipsoid. D1, D2, D3, I1, I2, I3 are all... -
4.2. Bulk density and magnetic susceptibility of sediment core SLW1_SLW_MC3A
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.2. Bulk density and magnetic susceptibility of sediment core SLW1_PEC1
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.2. Bulk density and magnetic susceptibility of sediment core SLW1_PC1
Gamma ray attenuation bulk density and magnetic susceptibility logged using a Geotek multi-sensor core logger at the Hartshorne Quaternary Lab at University of Massachusetts,... -
4.5. Principal Component Analysis calculation of best fit line for multiple d...
Principal Component Analysis (PCA) calculation of best fit line for multiple demagnetization steps in order to determine the inclination and declination. 20, 30, 40, and 50 mT...
