dolomitization

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dol·o·mite

 (dō′lə-mīt′, dŏl′ə-)
n.
1. A white or light-colored mineral, essentially CaMg(CO3)2, used in fertilizer, as a furnace refractory, and as a construction and ceramic material.
2. A magnesia-rich sedimentary rock resembling limestone.

[French, after Déodat de Dolomieu (1750-1801), French geologist.]

dol′o·mit′ic (-mĭt′ĭk) adj.
dol′o·mit′i·za′tion (-mĭt′ĭ-zā′shən) n.
dol′o·mit·ize′ (-mĭ-tīz′) v.
American Heritage® Dictionary of the English Language, Fifth Edition. Copyright © 2016 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.

dolomitization

(ˈdɒləmɪtaɪˌzeɪʃən) or

dolomitisation

n
the process or act of turning into dolomite
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014
References in periodicals archive ?
Due to their rhomboidal shape, the empty pores are interpreted to result from the local dissolution of metastable dolomite minerals and, as such, the dissolution process appears to be fundamentally unrelated to the dolomitisation process.
Dolomitisation improves reservoir quality in parts but production is controlled by natural fractures.
When dolomitisation is absent, the limestone textures are wackestones and oolitic grainstones; numerous banks show parallel lamination and the karstification is more intense.
Dolomitisation of sedimentary carbonate material is a widely-reported process for many Nigerian carbonates and metacarbonates (e.g.
La cimentation, la dissolution et la dolomitisation suppose la circulation de volumes considerables d'eaux souterraines (peu importe le type et ou la salinite, qu'elles soient douces ou hypersalines), mobilises par les gradients hydrauliques ambiants.