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Exemplary behaviour of red palaeosol (RP) samples by alternating field demagn...
This dataset has no description
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Principal component analyses of surface sediment from the Canadian Beaufort S...
This dataset has no description
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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... -
(Table 17) ChRM inclinations and paleolatitudes of discrete samples from ODP ...
This dataset has no description
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(Table 16) ChRM inclinations and paleolatitudes of discrete samples from ODP ...
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(Table T3) Paleomagnetic properties of igneous samples from DSDP Hole 86-581 ...
Sediment depth is given in mbsf. Note that for 88-581B negative inclinations assumed reversed polarity. -
(Table T5) Paleomagnetic properties of igneous samples from ODP Site 129-800,...
Sediment depth is given in mbsf. Note that for 129-800-57R polarity assumed normal; for Cores 129-800-58R and 129-800-60R polarity assumed reversed. -
(Table T1) Paleomagnetic properties of igneous samples from DSDP Leg 17 sites
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(Appendix 4B) Varimax factor loading matrix for benthic foraminifera in easte...
This dataset has no description
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(Appendix 4A) Principal factor loading matrix for benthic foraminifera in eas...
This dataset has no description
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(Appendix 3B) Varimax factor score matrix for benthic foraminifera in eastern...
This dataset has no description
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(Appendix 3A) Principal factor score matrix for benthic foraminifera in easte...
This dataset has no description
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Paleomagnetic of sediment core DVDP-11
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Paleomagnetic of sediment core DVDP-10
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Paleomagnetic of sediment core CIROS-2
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(Appendix 5) Principal Component Scores of benthic foraminifera Q-mode assemb...
This dataset has no description
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XRF analysis of sediment core from Asea (Peloponnese, Greece) for the Late Ho...
The sediment core Asea-1 was retrieved from the Asea Valley, Peloponnese Greece, in 2010 using a vibra corer. The upper 5 m were scanned at 0.5 cm resolution with... -
Paleosecular geomagnetic variation for the Holocene measured from U-channels ...
Inclination, declination, and relative palaeointensity calculated as a composite (WINPSV-12K) of four sediment cores (+54-03/57PC, +54-03/64PC, +54-03/67PC, +54-03/68PC) from... -
(Table T1) Paleomagnetic properties of ODP Hole 191-1179D basalts
During Ocean Drilling Program Leg 191, ~100 m of mid-Cretaceous igneous crust was cored at Site 1179 (41.08°N, 159.96°E), located within magnetic Anomaly M8 on the abyssal plain... -
(Table T1) Paleomagnetic characterization of sedimentary rocks from ODP Hole ...
Coring in Hole 1213B on the south flank of Shatsky Rise recovered sedimentary rocks (chalk and claystone) of earliest Cretaceous (Berriasian) age. Because few samples of this...
