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In ore deposit geology , hypogene processes occur deep below the earth's surface, and tend to form deposits of primary minerals, as opposed
Kaynak: Hypogene (geology)

Metals that have been leached from the oxidized ore are carried downward by percolating groundwater, and react with hypogene sulfides at
Kaynak: Supergene (geology)

This hypogene process is applicable to the original copper sulfide deposition; however, it is difficult to account for the many features
Kaynak: Turquoise

Sarabauite's formation makes it the only hypogene antimony mineral whose fluid inclusions can be studied in thin section under normal light
Kaynak: Sarabauite

they were of hypogene origin Other precious metals such as platinum form nuggets in the same way. Composition: Nuggets are usually 20K to 22
Kaynak: Gold nugget

The operation of mining was divided into mining the hypogene sulfide mineralization (chalcopyrite ) at depth and the shallow supergene
Kaynak: San Manuel Copper Mine

descending surface water in the supergene enrichment zone oxidizes and redeposits covellite on hypogene sulfides (pyrite and chalcopyrite).
Kaynak: Covellite

The main sulfides are pyrite and chalcopyrite and all mineralization came from processes occurring deep below the surface (hypogene).
Kaynak: Kerr Sulphurets Mitchell

The deeper sulfide (hypogene ) ore was much more difficult to work and had to be roasted prior to amalgamation. Milling and concentration
Kaynak: Austin, Nevada

secondary sulfides arise from the leaching of the overlying ore and its re-deposition on and replacement of the deeper primary (hypogene) sulfides.
Kaynak: Chuquicamata

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