Possible roles of clay minerals in the formation of dolomite
Abstract
The possibility is considered that clay minerals can influence the formation of some kinds of dolomite, either by supplying magnesium ions or serving as membranes that control ionic migration.
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Interpretations of studies concerning the effect of clay minerals on abiotic dolomite formation are largely contradictory.
“Although there are a few studies concerning the effect of clay minerals on abiotic dolomite formation, the interpretations are largely contradictory.”
From Experimental evidence for abiotic formation of low-temperature proto-dolomite facilitated by clay minerals (2019) · cites this paper as Kahle, 1965
Dolomite authigenesis in many sedimentary settings indicates the growth of dolomite crystals in pore spaces around detrital clay particles.
“As a matter of fact, it has been observed that the dolomite authigenesis in many sedimentary settings indicates 8 the growth of dolomite crystals in pore spaces around detrital clay particles.10,44”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [44]
The smaller growth rate of dolomite and magnesite compared to calcite is often related to the slower water exchange rate and higher dehydration enthalpies for Mg cations compared with Ca cations.
“The smaller growth rate of dolomite and magnesite when compared to calcite is often related to the slower water exchange rate and higher dehydration enthalpies for Mg cations compared with Ca cations”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [45]
The kinetic model of magnesite precipitation is still a matter of debate, with other studies suggesting that magnesite grows via a kink site nucleation and propagation model.
“However, the kinetic model of magnesite precipitation is still a matter of debate, other studies suggesting that magnesite grows via a kink site nucleation and propagation model.45”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [45]
MgCl2 and artificial brine have been investigated as precursors for mineral carbonation due to their high availability in seawater and brine lakes and their high likelihood of being the Mg precursors in natural reservoirs of dolomite and/or magnesite.
“MgCl 2 and artificial brine have been investigated as precursors for routes of mineral carbonation, not only due to their high availability in seawater and brine lakes, but also due to their high likelihood of being the Mg precursors in natural reservoirs of dolomite and/or magnesite.”
From Mechanisms of Mg carbonates precipitation and implications for CO <sub>2</sub> capture and utilization/storage (2023) · cites this paper as [45]
Cited by
Sorted by citations
Dolomite: occurrence, evolution and economically important associations
Warren, J. (2000) · Earth-Science Reviews · doi:10.1016/s0012-8252(00)00022-2 · Cited by 1,435 · see citing works
Liu, D., Xu, Y., Papineau, D., Yu, N., Fan, Q., Qiu, X., & Wang, H. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2018.12.036 · Cited by 141 · see citing works
Santos, H. S., Nguyen, H., Venâncio, F., Ramteke, D., Zevenhoven, R., & Kinnunen, P. (2023) · Inorganic Chemistry Frontiers · doi:10.1039/d2qi02482a · Cited by 108 · see citing works
LINDTKE, J., ZIEGENBALG, S. B., BRUNNER, B., ROUCHY, J. M., PIERRE, C., & PECKMANN, J. (2011) · Geological Magazine · doi:10.1017/s0016756811000124 · Cited by 50 · see citing works
An Early Holocene Primary Dolomite Layer of Abiotic Origin in Lake Sayram, Central Asia
Cheng, J., Meng, X., Zhang, E., Jiang, Q., Ni, Z., & Ji, J. (2021) · Geophysical Research Letters · doi:10.1029/2021gl096309 · Cited by 20 · see citing works
- Authors
- Kahle, C. F.
- Corresponding author
- Kahle, Charles F.
- Venue
- Journal of Sedimentary Research
- Publisher
- Society for Sedimentary Geology
- Published
- 1965-06-01
- Volume
- 35
- Issue
- 2
- Pages
- 448-453
- ISSN
- 0022-4472 (ISSN-L)
- 1938-3681
- 1527-1404
- OpenAlex
- W1974146357
- Cited by
- 56
- References
- 0
- Citations by year
- 2026: 1 · 2025: 1 · 2024: 2 · 2023: 3 · 2022: 2 · 2021: 4 · 2020: 1 · 2019: 4 · 2018: 1 · 2017: 1 · 2016: 3 · 2014: 1
- FWCI
- 4.12
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Sedimentary Research (publishedVersion)
- Funders
- Oklahoma State University
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
- Physical Sciences › Engineering › Mechanics of Materials › Hydrocarbon exploration and reservoir analysis
- Keywords
- clay minerals, dolomite formation, magnesium ions, ion exchange, ion migration, diagenesis
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