Early Paleocene and Late Cretaceous magnetostratigraphic assignments for Maud Rise sediments (Table 1)

DOI

A paleomagnetic investigation of the Late Cretaceous sediments of the Maud Rise, Antarctica, recovered in Holes 689B and 690C provides a fairly complete magnetostratigraphic record ranging from Chron C33N through Chron C29R. The Cretaceous/Tertiary boundary is shown to occur in Chron C29R at Site 690.

Supplement to: Hamilton, Norman (1990): Mesozoic magnetostratigraphy of Maud Rise, Antarctica. In: Barker, PF, Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 255-260

Identifier
DOI https://doi.org/10.1594/PANGAEA.746504
Related Identifier https://doi.org/10.2973/odp.proc.sr.113.179.1990
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.746504
Provenance
Creator Hamilton, Norman
Publisher PANGAEA
Publication Year 1990
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 13 data points
Discipline Earth System Research
Spatial Coverage (1.205W, -65.160S, 3.100E, -64.517N); South Atlantic Ocean
Temporal Coverage Begin 1987-01-16T08:00:00Z
Temporal Coverage End 1987-01-23T20:30:00Z