Uranopolycrase
id:
uranopolycrase-311-17042335
title:
Uranopolycrase
text:
Uranopolycrase is an oxide mineral first discovered in the Fonte del Prete vein of a pegmatite vein in San Piero in Campo, Elba Island, Tuscany, Italy. Uranopolycrase is a member of the Euxenite Group and is the uranium bearing analog of polycrase-(Y). The type specimen is almost entirely metamict. The ideal formula for uranopolycrase is (U,Y)(Ti,Nb)2O6. The mineral has been approved by the Commission on New Minerals and Mineral Names of the International Mineralogical Association to be named ur
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Uranopolycrase
date created:
date modified:
2024-01-12T06:58:11Z
main entity:
{"identifier":"Q4006326","url":"https://www.wikidata.org/entity/Q4006326"}
image:
fields total:
13
integrity:
13