Meteoric water
Water of atmospheric origin: rain, snow, rivers, groundwater. Its δD and δ18O follow the global meteoric water line and become lighter towards high latitudes and altitudes, whereas magmatic water is much heavier in 18O (about 6 to 10 ‰). Their mixing shows up in ore fluids.
Composition
Global meteoric water line: δD = 8 × δ18O + 10 (Craig, 1961).
Sources
In the atlas
- Matra France
- Shuiyindong China
- Luziyuan China
- Binh Do Viêt Nam
- Haobugao China
- Xinchang-Yongjia silver belt (Haoshi, Bamao, Dalingkou, Wubu) China
- Koru (Tahtalıkuyu et Eskikışla) Turkey
- Dunde China
- Shuitoushan China
- Nebida Italy
- Seddas Moddizzis Italy
- Mount Agruxiau Italy
- Campo Pisano Italy
- San Benedetto Italy
- Montevecchio Italy
- Welkenraedt Belgique
- Theux Belgique
- Angleur Belgique
- Century Australia
- Watson's Lode Australia
- Flat Tyre Australia
- Lawn Hill discordant Zn-Pb-Ag lodes Australia
- Maoping (tungsten, Jiangxi) China
- Jiaoxi China
- Xiaoganjia China
- Piaotang China
- Lianhuashan China
- Changpu China
- Guangping China
- Jiuhuashan China