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redoxomorphic stage

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redoxomorphic stage [ri¦däk·sə¦mȯr·fik ‚stāj]
(geochemistry)
The earliest geochemical stage of diagenesis characterized by mineral changes primarily due to oxidation and reduction reactions.


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The redoxomorphic stage is mostly responsible for the bulk final colour of the rock, while later changes in rock colour are smaller.
 
 
 
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