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Epigenetic mineral matter

Epigenetic mineral matter is formed from aqueous solutions that penetrated into cracks of the deposit casting, typically carbonates, quartz, sulfides, or salts washed out from adjacent rocks. Epigenetic mineral matter occurs separated from the organic matrbc. [Pg.69]

See other pages where Epigenetic mineral matter is mentioned: [Pg.195]    [Pg.195]    [Pg.7]    [Pg.92]    [Pg.30]    [Pg.202]    [Pg.72]    [Pg.3673]    [Pg.504]    [Pg.260]    [Pg.125]    [Pg.323]   
See also in sourсe #XX -- [ Pg.92 ]



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