Canavesite is a secondary mineral that occurs due to the weathering of ludwigite-magnetite skarn on the surface of mine walls.
42.
Secondary minerals consist of lead minerals like anglesite, cerussite, pyromorphite and wulfenite, and of iron sulfides like marcasite and pyrite.
43.
It is an uncommon secondary mineral in the oxidized zone of arsenic bearing zinc deposits and occurs rarely in granite pegmatite.
44.
Because zemannite is secondary mineral, its crystals usually on other rocks and retain the hexagonal shape corresponding to their crystal symmetry.
45.
Lanthanites are frequently found as secondary minerals formed by the weathering of other minerals and occur as scales or tabular crystals.
46.
These secondary minerals show several hundred times lower concentration of plutonium and several times higher concentration of uranium than the lava itself.
47.
It occurs as a secondary mineral that can be found in sandstone and also in the oxidized zones of vanadium bearing deposits.
48.
Beraunite occurs as a secondary mineral in iron ore deposits, and as an alteration product of primary phosphate minerals in granite pegmatites.
49.
They noticed secondary minerals forming between szaibelyite and ludwigite at the point where they come into contact with each other inside magnetite skarns.
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I was trying to improve a " random " page ( on Wulfenite ) and came across the term " secondary mineral ".
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