Jing-jing, Zhu; Rui-zhong, Hu; Xian-wu, Bi; Hong, Zhong; Heng, Chen (2011): Appendix B: Zircon oxygen isotopic analysis of the Beiwu, Linong and Lunong intrusions [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.763240, In supplement to: Jing-jing, Z et al. (2011): Zircon U-Pb ages, Hf-O isotopes and whole-rock Sr-Nd-Pb isotopic geochemistry of granitoids in the Jinshajiang suture zone, SW China: constraints on petrogenesis and tectonic evolution of the Paleo-Tethys Ocean. Lithos, https://doi.org/10.1016/j.lithos.2011.07.003
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Coverage:
Median Latitude: 28.919792 * Median Longitude: 99.092060 * South-bound Latitude: 28.889667 * West-bound Longitude: 99.084111 * North-bound Latitude: 28.960139 * East-bound Longitude: 99.102806
Event(s):
BW-1 * Latitude: 28.960139 * Longitude: 99.093583 * Location: Beiwu intrusion, Hajiang suture zone, southwest China * Method/Device: Rock sample (ROCK)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Sample code/label | Sample label | Jing-jing, Zhu | |||
| 3 | δ18O | δ18O | ‰ | Jing-jing, Zhu | ||
| 4 | δ18O, standard deviation | δ18O std dev | ± | Jing-jing, Zhu | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
366 data points
Data
| 1 Event | 2 Sample label | 3 δ18O [‰] | 4 δ18O std dev [±] |
|---|---|---|---|
| LiN-1 | LiN01-1 | 8.0 | 0.4 |
| LiN-1 | LiN01-2 | 8.1 | 0.3 |
| LiN-1 | LiN01-3 | 7.6 | 0.4 |
| LiN-1 | LiN01-4 | 7.9 | 0.4 |
| LiN-1 | LiN01-5 | 7.8 | 0.3 |
| LiN-1 | LiN01-6 | 7.9 | 0.3 |
| LiN-1 | LiN01-7 | 7.8 | 0.3 |
| LiN-1 | LiN01-8 | 8.2 | 0.4 |
| LiN-1 | LiN01-9 | 8.3 | 0.3 |
| LiN-1 | LiN01-10 | 8.1 | 0.3 |
| LiN-1 | LiN01-11 | 7.6 | 0.3 |
| LiN-1 | LiN01-12 | 8.6 | 0.3 |
| LiN-1 | LiN01-13 | 8.2 | 0.3 |
| LiN-1 | LiN01-14 | 8.0 | 0.3 |
| LiN-1 | LiN01-15 | 7.8 | 0.4 |
| LiN-1 | LiN01-16 | 8.0 | 0.3 |
| LiN-1 | LiN01-17 | 8.9 | 0.3 |
| LiN-1 | LiN01-18 | 8.4 | 0.3 |
| LiN-1 | LiN01-19 | 8.3 | 0.3 |
| LiN-1 | LiN01-20 | 7.3 | 0.4 |
| LiN-2 | LiN02-1 | 7.6 | 0.3 |
| LiN-2 | LiN02-2 | 7.8 | 0.2 |
| LiN-2 | LiN02-3 | 8.0 | 0.3 |
| LiN-2 | LiN02-4 | 7.9 | 0.3 |
| LiN-2 | LiN02-5 | 8.3 | 0.3 |
| LiN-2 | LiN02-6 | 8.5 | 0.3 |
| LiN-2 | LiN02-7 | 8.8 | 0.3 |
| LiN-2 | LiN02-8 | 8.3 | 0.3 |
| LiN-2 | LiN02-9 | 8.3 | 0.3 |
| LiN-2 | LiN02-10 | 8.5 | 0.4 |
| LiN-2 | LiN02-11 | 8.2 | 0.4 |
| LiN-2 | LiN02-12 | 8.1 | 0.3 |
| LiN-2 | LiN02-13 | 8.5 | 0.3 |
| LiN-2 | LiN02-14 | 7.3 | 0.5 |
| LiN-2 | LiN02-15 | 8.0 | 0.3 |
| LiN-2 | LiN02-16 | 8.4 | 0.2 |
| LiN-2 | LiN02-17 | 8.1 | 0.4 |
| LiN-2 | LiN02-18 | 7.7 | 0.4 |
| LiN-2 | LiN02-19 | 7.6 | 0.3 |
| LiN-2 | LiN02-20 | 7.4 | 0.3 |
| LuN-2 | LuN02-1 | 8.6 | 0.3 |
| LuN-2 | LuN02-2 | 8.1 | 0.4 |
| LuN-2 | LuN02-3 | 8.3 | 0.3 |
| LuN-2 | LuN02-4 | 7.8 | 0.3 |
| LuN-2 | LuN02-5 | 8.6 | 0.3 |
| LuN-2 | LuN02-6 | 8.0 | 0.4 |
| LuN-2 | LuN02-7 | 7.7 | 0.3 |
| LuN-2 | LuN02-8 | 8.4 | 0.4 |
| LuN-2 | LuN02-9 | 8.1 | 0.3 |
| LuN-2 | LuN02-10 | 8.0 | 0.3 |
| LuN-2 | LuN02-11 | 8.3 | 0.3 |
| LuN-2 | LuN02-12 | 7.9 | 0.3 |
| LuN-2 | LuN02-13 | 8.0 | 0.3 |
| LuN-2 | LuN02-14 | 7.5 | 0.4 |
| LuN-2 | LuN02-15 | 7.6 | 0.3 |
| LuN-2 | LuN02-16 | 7.9 | 0.3 |
| LuN-2 | LuN02-17 | 8.0 | 0.3 |
| LuN-2 | LuN02-18 | 8.2 | 0.4 |
| LuN-2 | LuN02-19 | 7.9 | 0.4 |
| LuN-2 | LuN02-20 | 7.9 | 0.3 |
| LuN-2 | LuN02-21 | 8.3 | 0.3 |
| LuN-1 | LuN01-1 | 8.2 | 0.3 |
| LuN-1 | LuN01-2 | 8.3 | 0.3 |
| LuN-1 | LuN01-3 | 8.0 | 0.4 |
| LuN-1 | LuN01-4 | 8.3 | 0.3 |
| LuN-1 | LuN01-5 | 8.4 | 0.3 |
| LuN-1 | LuN01-6 | 7.6 | 0.2 |
| LuN-1 | LuN01-7 | 8.2 | 0.3 |
| LuN-1 | LuN01-8 | 8.2 | 0.3 |
| LuN-1 | LuN01-9 | 8.2 | 0.4 |
| LuN-1 | LuN01-10 | 8.4 | 0.3 |
| LuN-1 | LuN01-11 | 7.7 | 0.4 |
| LuN-1 | LuN01-12 | 8.4 | 0.2 |
| LuN-1 | LuN01-13 | 8.3 | 0.3 |
| LuN-1 | LuN01-14 | 8.2 | 0.2 |
| LuN-1 | LuN01-15 | 8.5 | 0.3 |
| LuN-1 | LuN01-16 | 8.7 | 0.3 |
| LuN-1 | LuN01-17 | 8.3 | 0.3 |
| LuN-1 | LuN01-18 | 8.4 | 0.4 |
| LuN-1 | LuN01-19 | 8.4 | 0.3 |
| LuN-1 | LuN01-20 | 8.2 | 0.4 |
| LuN-1 | LuN01-21 | 8.9 | 0.4 |
| BW-6 | BW0902-1 | 7.8 | 0.3 |
| BW-6 | BW0902-2 | 7.6 | 0.3 |
| BW-6 | BW0902-3 | 8.0 | 0.4 |
| BW-6 | BW0902-4 | 7.3 | 0.2 |
| BW-6 | BW0902-5 | 7.9 | 0.2 |
| BW-6 | BW0902-6 | 7.9 | 0.3 |
| BW-6 | BW0902-7 | 7.8 | 0.3 |
| BW-6 | BW0902-8 | 7.8 | 0.4 |
| BW-6 | BW0902-9 | 8.9 | 0.3 |
| BW-6 | BW0902-10 | 7.7 | 0.4 |
| BW-6 | BW0902-11 | 7.5 | 0.3 |
| BW-6 | BW0902-12 | 7.7 | 0.2 |
| BW-6 | BW0902-13 | 7.5 | 0.3 |
| BW-6 | BW0902-14 | 7.9 | 0.3 |
| BW-6 | BW0902-15 | 7.9 | 0.3 |
| BW-6 | BW0902-16 | 8.4 | 0.3 |
| BW-6 | BW0902-17 | 7.9 | 0.3 |
| BW-6 | BW0902-18 | 7.3 | 0.3 |
| BW-6 | BW0902-19 | 7.3 | 0.2 |
| BW-6 | BW0902-20 | 7.4 | 0.3 |
| BW-1 | BW0901-1 | 7.7 | 0.2 |
| BW-1 | BW0901-2 | 7.4 | 0.2 |
| BW-1 | BW0901-3 | 7.5 | 0.3 |
| BW-1 | BW0901-4 | 7.6 | 0.2 |
| BW-1 | BW0901-5 | 8.2 | 0.2 |
| BW-1 | BW0901-6 | 7.6 | 0.2 |
| BW-1 | BW0901-7 | 8.2 | 0.4 |
| BW-1 | BW0901-8 | 7.9 | 0.3 |
| BW-1 | BW0901-9 | 7.9 | 0.3 |
| BW-1 | BW0901-10 | 8.1 | 0.3 |
| BW-1 | BW0901-11 | 8.3 | 0.2 |
| BW-1 | BW0901-12 | 8.7 | 0.2 |
| BW-1 | BW0901-13 | 9.3 | 0.3 |
| BW-1 | BW0901-14 | 7.8 | 0.4 |
| BW-1 | BW0901-15 | 8.3 | 0.2 |
| BW-1 | BW0901-16 | 7.9 | 0.3 |
| BW-1 | BW0901-17 | 8.0 | 0.2 |
| BW-1 | BW0901-18 | 8.0 | 0.2 |
| BW-1 | BW0901-19 | 8.1 | 0.3 |
| BW-1 | BW0901-20 | 8.4 | 0.2 |