2026-06-27T23:51:47Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/340862023-08-25T17:24:39Zcom_20.500.14352_14col_20.500.14352_15
Docta Complutense
author
Pina Martínez, Carlos Manuel
2023-06-19T13:35:34Z
2023-06-19T13:35:34Z
2015
ISSN: 0003-004X
10.2138/am-2015-5269
https://hdl.handle.net/20.500.14352/34086
https://pubs.geoscienceworld.org/msa/ammin/article/100/5-6/1017-1018/40446
Little is known about the physico-chemical processes that lead to the formation of dolomite in nature. Issues requiring further investigation include: (1) the role played by amorphous carbonate precursors, (2) the mechanisms of transformation of such precursors into proto-dolomite and dolomite, and (3) the controlling factors of the kinetics of the reactions that eventually result in the crystallization of highly ordered dolomite. In the article by Rodriguez-Blanco et al. in this issue entitled “A route for the direct crystallization of dolomite,” the authors present experimental evidence of a threestage process that, starting from the precipitation of an amorphous magnesium calcium carbonate, produces proto-dolomite via spherulitic growth, and subsequently ordered dolomite. This article provides new insights into reaction pathways toward the formation of dolomite.
eng
Highlights and Breakthroughs. Reaction pathways toward the formation of dolomite
journal article
URL
https://docta.ucm.es/bitstreams/569b85e4-97f8-411d-9822-bde4ad0b597e/download
File
MD5
7fed5b1c667d78685a113baa928633ba
116504
application/pdf
Reaction pathways toward the formation of dolomite Pina 2015-2.pdf
URL
https://docta.ucm.es/bitstreams/0f4b032d-bd3e-4b4c-8c8c-5eb89c693dc3/download
File
MD5
0479f2050b7bde221f6c817813fb2805
8480
text/plain
Reaction pathways toward the formation of dolomite Pina 2015-2.pdf.txt