Cargando…
Paradoxically lowered oxygen isotopes of hydrothermally altered minerals by an evolved magmatic water
It has been well known that the influxing meteoric water can hydrothermally lower oxygen and hydrogen isotopes of rocks and/or minerals during continental magmatic or metamorphic processes in certain appropriate cases. Its opposite, however, is not implicitly true and needs independent testing. In t...
Autores principales: | Wei, Chun-Sheng, Zhao, Zi-Fu |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9519577/ https://www.ncbi.nlm.nih.gov/pubmed/36171246 http://dx.doi.org/10.1038/s41598-022-19921-y |
Ejemplares similares
-
Lithium isotope traces magmatic fluid in a seafloor hydrothermal system
por: Yang, Dan, et al.
Publicado: (2015) -
A nonlinear controlling function of geological features on magmatic–hydrothermal mineralization
por: Zuo, Renguang
Publicado: (2016) -
Monitoring of magmatic–hydrothermal system by noble gas and carbon isotopic compositions of fumarolic gases
por: Obase, Tomoya, et al.
Publicado: (2022) -
Oxygen controls on magmatism in rocky exoplanets
por: Lin, Yanhao, et al.
Publicado: (2021) -
Garnet secondary ion mass spectrometry oxygen isotopes reveal crucial roles of pulsed magmatic fluid and its mixing with meteoric water in lode gold genesis
por: Fan, Gao-Hua, et al.
Publicado: (2022)