H-O isotopes of vein quartz in the Yaogangxian tungsten deposit, South China

DOI

Note: the δ18O-H2O values are calculated based on the average homogenization temperature of 256 °C of quartz using the equation of Matsuisha et al. (1979): δ18O-SiO2 − δ18O-fluid = 3.34 × 106/(Th + 273.15)2 − 3.31. The results are reported relative to the Vienna Standard Mean Ocean Water (SMOW) standard.

Identifier
DOI https://doi.org/10.1594/PANGAEA.925164
Related Identifier https://doi.org/10.1594/PANGAEA.925167
Related Identifier https://doi.org/10.1016/0016-7037(79)90099-1
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.925164
Provenance
Creator Xiao, Ming ORCID logo; Qiu, Hua-Ning; Cai, Yue ORCID logo; Jiang, Ying-De; Zhang, Wan-Feng; Fang, Yuan
Publisher PANGAEA
Publication Year 2021
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 25 data points
Discipline Earth System Research
Spatial Coverage (113.319 LON, 25.661 LAT); China