Agrotermos

Preferred term

Dolomitización

Dolomitization is one of the most significant diagenetic reactions in carbonate systems, occurring where limestone (CaCO3) is replaced by dolomite (CaMg (CO3)2) under a wide range of crystallization temperatures and fluids.

Diagénesis

English

Created

2019-09-04T12:02:37

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

881a9371

dolomitization

French

Created

2022-03-18T16:52:06

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

881a9371

dolomitisation

URI

http://aims.fao.org/aos/agrovoc/c_881a9371

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Created 9/4/19, 12:02 PM, last modified 10/10/24, 2:04 PM