Rare-earth-element (REE) concentrations of hydrothermally altered basaltic rocks in IODP Hole U1502B (Dataset S3)


a Eu anomaly is calculated using Eu/Eu* = EuN / (SmN 2 + GdN 2) 1/2; the subscript N denotes normalized to chondrite (Anders and Grevesse, 1989).b Normalized to chondrite (Anders and Grevesse, 1989), the ratio of LREE (light REE, La–Sm) to HREE (heavy REE, Gd–Lu) (i.e. L/HREE), and often approximated by the ratio of La to Yb (i.e. LaN/YbN).Values in mg/kg given in ppm.

DOI https://doi.org/10.1594/PANGAEA.946082
Related Identifier https://doi.org/10.1594/PANGAEA.946146
Related Identifier https://doi.org/10.1016/j.chemgeo.2021.120569
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.946082
Creator Wu, Jiawang; Liu, Zhifei; Yu, Xun
Publisher PANGAEA
Publication Year 2022
Funding Reference China Postdoctoral Science Foundation, 2018M640418; China Postdoctoral Science Foundation, 2019T120352; National Natural Science Foundation of China, 2018YFE0202402; National Natural Science Foundation of China, 41530964; National Natural Science Foundation of China, 41806064; National Natural Science Foundation of China, 41906051; Shanghai Association for Science and Technology, 20590780200
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 945 data points
Discipline Earth System Research
Spatial Coverage (116.231 LON, 18.465 LAT)
Temporal Coverage Begin 2017-04-29T19:30:00Z
Temporal Coverage End 2017-05-13T20:50:00Z