Automated Author ProfileChen, Yan
University of Orléans, CNRS, BRGM, ISTO, UMR 7327, F-45071, Orléans, France
Chen, Yan
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 3.2 (sum of 2 datasets Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
This repository contains SIMS U-Pb data of zircons from the syntectonic Mupi pluton (Table S1) and 40Ar/39Ar furnace step-heating analytical results of synmetamorphic micas (Table S2) from the Longmenshan Thrust Belt, East Tibet, China. In Table S1, six spots of zircon core are omitted from the Concordia spectra. In Table S2, all step ages are calculated by using both atmospheric argon 40Ar/36Ar of 298.56 (Lee et al., 2006, Geochimica et Cosmochimica Acta) and from the "inverse isochron". The two groups of step ages consistent within deviations.
Authors
- Zhenhua Xue ;
- Lin, Wei ;
- Chu, Yang ;
- Faure, Michel ;
- Chen, Yan ;
- Wenbin Ji ;
- Huaning Qiu
This repository contains SIMS U-Pb data of zircons from the syntectonic Mupi pluton (Table S1) and 40Ar/39Ar furnace step-heating analytical results of synmetamorphic micas (Table S2) from the Longmenshan Thrust Belt, East Tibet, China. In Table S1, six spots of zircon core are omitted from the Concordia spectra. In Table S2, all step ages are calculated by using both atmospheric argon 40Ar/36Ar of 298.56 (Lee et al., 2006, Geochimica et Cosmochimica Acta) and from the "inverse isochron". The two groups of step ages consistent within deviations.
Authors
- Zhenhua Xue ;
- Lin, Wei ;
- Chu, Yang ;
- Faure, Michel ;
- Chen, Yan ;
- Wenbin Ji ;
- Huaning Qiu