Shock-transformation of whitlockite to merrillite and the implications for meteoritic phosphate
Quantifying the amount of water in meteorites remains challenging, with minerals the key to understanding water contents. Here, Adcocket al. perform shock experiments on H+-bearing whitlockite demonstrating that it may transform into anhydrous merrillite, which is commonly found in Martian meteorite...
Guardado en:
Autores principales: | C. T. Adcock, O. Tschauner, E. M. Hausrath, A. Udry, S. N. Luo, Y. Cai, M. Ren, A. Lanzirotti, M. Newville, M. Kunz, C. Lin |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2017
|
Materias: | |
Acceso en línea: | https://doaj.org/article/09416eb06d3d4028b4d557e993f9f079 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Clay mineral formation under oxidized conditions and implications for paleoenvironments and organic preservation on Mars
por: Seth R. Gainey, et al.
Publicado: (2017) -
Meteoritics & planetary science
Publicado: (1996) -
Comparative study of porous hydroxyapatite/chitosan and whitlockite/chitosan scaffolds for bone regeneration in calvarial defects
por: Zhou D, et al.
Publicado: (2017) -
Organometallic compounds as carriers of extraterrestrial cyanide in primitive meteorites
por: Karen E. Smith, et al.
Publicado: (2019) -
A potential hidden layer of meteorites below the ice surface of Antarctica
por: G. W. Evatt, et al.
Publicado: (2016)