(Table S1) Age determination of Emperor Seamounts basement

DOI

The Hawaiian-Emperor hotspot track has a prominent bend, which has served as the basis for the theory that the Hawaiian hotspot, fixed in the deep mantle, traced a change in plate motion. However, paleomagnetic and radiometric age data from samples recovered by ocean drilling define an age-progressive paleolatitude history, indicating that the Emperor Seamount trend was principally formed by the rapid motion (over 40 millimeters per year) of the Hawaiian hotspot plume during Late Cretaceous to early-Tertiary times (81 to 47 million years ago). Evidence for motion of the Hawaiian plume affects models of mantle convection and plate tectonics, changing our understanding of terrestrial dynamics.

Ages calculated using biotite monitor FCT-3 (28.04 Ma) and the following decay constants:lambda-epsilon = 0.581E-10/yr, lambda-epsiolon = 4.963E-10/yr.

Supplement to: Tarduno, John A; Duncan, Robert A; Scholl, David W; Cottrell, Rory D; Steinberger, Bernhard; Thordarson, Thorvaldur; Kerr, Bryan C; Neal, Clive R; Frey, Frederick A; Torii, Masayuki; Carvallo, Claire (2003): The Emperor Seamounts: Southward motion of the Hawaiian hotspot plume in earth's mantle. Science, 301(5636), 1064-1069

Identifier
DOI https://doi.org/10.1594/PANGAEA.772113
Related Identifier https://doi.org/10.1126/science.1086442
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.772113
Provenance
Creator Tarduno, John A ORCID logo; Duncan, Robert A; Scholl, David W; Cottrell, Rory D ORCID logo; Steinberger, Bernhard ORCID logo; Thordarson, Thorvaldur ORCID logo; Kerr, Bryan C; Neal, Clive R; Frey, Frederick A ORCID logo; Torii, Masayuki; Carvallo, Claire
Publisher PANGAEA
Publication Year 2003
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 222 data points
Discipline Earth System Research
Spatial Coverage (164.714W, 34.926S, 172.146E, 53.010N); North Pacific/GUYOT; North Pacific Ocean
Temporal Coverage Begin 1971-08-30T00:00:00Z
Temporal Coverage End 2001-08-13T00:00:00Z