Rock magnetic properties and titanomagnetite oxydation state of ODP Hole 109-648B (Table 1)

Petersen, Nikolai P;Vali, Hojatollah

Description

The titanomagnetite oxidation state of "zero age" ocean floor basalts was investigated. For this purpose the oxidation parameter, z, of Hole 648B basalts was determined by SEM observation of "shrinkage cracks" in individual titanomagnetite grains and by Curie temperature measurements. A mean z-value of 0.1 has been deduced for the Hole 648B basalts.Assuming a linear relationship between titanomagnetite low-temperature oxidation state and age of the oceanic basalt, an age of 0.7 m.y. is deduced for Hole 648B.

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Mentions (0)

Metrics

Dataset Index

0.7

FAIR Score

94%

Citations

1

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

PANGAEA

License

Creative Commons Attribution 3.0 Unported

Assigned Domain

Subfield

Geochemistry and Petrology

Field

Earth and Planetary Sciences

Domain

Physical Sciences

Confidence Score

42%

Source

Scholar Data Model

Keywords

Sample code/labelSpecific saturation magnetizationNRM, IntensityNRM, Median destructive field of natural remanent magnetizationCurie temperatureOxidation parameterDrilling/drill rigDSDP/ODP/IODP sample designationLeg109Joides ResolutionOcean Drilling Program (ODP)

Normalization Factors

FT

94.23

CTw

1.00

MTw

1.00