Navajoite is as isomorphism hosting in the lattice of hydromica which is the major hosting ore for navajoite.
水云母是钒的主要赋存体,钒是以类质同象的形式产于水云母的晶格中。
The geological and geochemical study results indicate that the metallogenetic materials came from the hydromica mudstones and shales of the Hanjiadian Group of Lower Silurian System.