Geochemistry of Vein Calcites Hosted in the Troodos Pillow Lavas and Their Implications for the Timing and Physicochemical Environment of Fracturing, Fluid Circulation, and Vein Mineral Growth

Calcite veins hosted in pillow lavas of the Late Cretaceous Troodos suprasubduction zone ophiolite provide insights into the timing and physicochemical environment of postmagmatic fracturing and fluid circulation through oceanic crust. This study presents rare earth element and yttrium (REE+Y) conce...

Descripción completa

Detalles Bibliográficos
Autores principales: Quandt, D., Micheuz, P., Kurz, W., Kluge, T., Boch, R., Hippler, D., Krenn, K., Hauzenberger, C.A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7004035/
https://www.ncbi.nlm.nih.gov/pubmed/32055238
http://dx.doi.org/10.1029/2019GC008369

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7004035/
https://www.ncbi.nlm.nih.gov/pubmed/32055238
http://dx.doi.org/10.1029/2019GC008369

Ejemplares similares