Trace element concentrations of calcite veins pervading the Western Pacific Izu-Bonin forearc and rear arc crust'

DOI

Volcanic rocks from the Izu-Bonin-Mariana forearc and rear arc, which were recovered during the International Ocean Discovery Program (IODP) Expeditions 352 and 351, are pervaded by calcite veins. The trace element concentrations of these calcite veins were determined using a laser ablation inductively-coupled plasma mass spectrometer.

Identifier
DOI https://doi.org/10.1594/PANGAEA.902424
Related Identifier https://doi.org/10.1594/PANGAEA.906261
Related Identifier https://doi.org/10.1029/2019GC008745
Related Identifier https://doi.org/10.1071/MF05229
Related Identifier https://doi.org/10.1016/j.chemgeo.2016.06.027
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.902424
Provenance
Creator Quandt, Dennis; Micheuz, Peter; Kurz, Walter; Bernasconi, Stefano M ORCID logo; Hippler, Dorothee; Krenn, Kurt; Hauzenberger, Christoph
Publisher PANGAEA
Publication Year 2019
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 3623 data points
Discipline Earth System Research
Spatial Coverage (134.318W, 27.384S, 142.754E, 28.450N); Amami-Sankaku basin; Izu-Bonin-Mariana fore arc
Temporal Coverage Begin 2014-06-30T09:00:00Z
Temporal Coverage End 2014-08-27T07:45:00Z