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Geochemistry of Evaporitic Lacustrine Deposits
Abstract
Carbonatites are igneous rocks formed in the crust by fractional crystallization of carbonate-rich parental melts that are mostly mantle derived. They dominantly consist of carbonate minerals such as calcite, dolomite, and ankerite, as well as minor ...Read More
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“A typical feature of evolved (evaporated) and highly saline waters is a composition marked by the presence of Cl -and SO 4 2-, and a depletion in CO 3 2-/HCO 3 - (Langbein, 1961;Hardie and Eugster, 1970;Eugster, 1980).”
From Brine grades in Andean salars: When basin size matters A review of the Lithium Triangle (2021) · cites this paper as Eugster, 1980
In the citing paper
“Brines concentrate as evaporation (i.e., water loss) induces salt precipitation (Eugster, 1980;Munk et al., 2018).”
From Chemical and isotopic features of Li-rich brines from the Salar de Olaroz, Central Andes of NW Argentina (2020) · cites this paper as Eugster, 1980
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Chemical evolution of shallow groundwater along the northeast shore of Mono Lake, California
Connell, T. L., & Dreiss, S. J. (1995) · Water Resources Research · doi:10.1029/95wr02566 · Cited by 20
Temperature-dependent, VIS-NIR reflectance spectroscopy of sodium sulfates
Angelis, S. D., Tosi, F., Carli, C., Potin, S. M., Beck, P., Brissaud, O., Schmitt, B., Piccioni, G., Sanctis, M. C. D., & Capaccioni, F. (2020) · Icarus · doi:10.1016/j.icarus.2020.114165 · Cited by 20
Ravidà, D. C. G., Caracciolo, L., Henares, S., et al. (2021) · Sedimentology · doi:10.1111/sed.12913 · Cited by 20
“Evidence for gypsum crystals and carbonate cementation support this interpretation (Eugster, 1980).”
BackgroundOrigins of aerosol chlorine during winter over north central Colorado, USA
Jordan, C. E., Pszenny, A. A. P., Keene, W. C., Cooper, O. R., Deegan, B., Maben, J. R., Routhier, M., Sander, R., & Young, A. H. (2015) · Journal of Geophysical Research Atmospheres · doi:10.1002/2014jd022294 · Cited by 20
“In addition to the heterogeneities associated with wind-driven soil deflation described above, the nature of closed playa basins and the minerals and salts within them vary spatially [Eugster, 1980].”
BackgroundKarakaya, M. Ç., Karakaya, N., & Yavuz, F. (2015) · Clays and clay minerals · doi:10.1346/ccmn.2015.0630202 · Cited by 17
Franco, M. G., Peralta Arnold, Y. J., Santamans, C. D., López Steinmetz, R. L., Tassi, F., Venturi, S., Jofré, C. B., Caffe, P. J., & Córdoba, F. E. (2020) · Journal of South American Earth Sciences · doi:10.1016/j.jsames.2020.102742 · Cited by 20
“Brines concentrate as evaporation (i.e., water loss) induces salt precipitation (Eugster, 1980; Munk et al., 2018).”
BackgroundStockstill‐Cahill, K. R., Moersch, J. E., Ruff, S. W., Baldridge, A. M., & Farmer, J. D. (2005) · Journal of Geophysical Research Atmospheres · doi:10.1029/2004je002353 · Cited by 20
“On Earth, playa basin evaporites often display a characteristic spatial pattern resulting from their order of deposition [e.g., Eugster, 1980; Eugster and Hardie, 1978; Jones, 1965].”
BackgroundXia, Z., Lin, Y., Wei, H., Hu, Z., Liu, C., & Li, W. (2021) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2021.110804 · Cited by 18
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Sorokin, D. Y. (2017) · Encyclopedia of Life Sciences · doi:10.1002/9780470015902.a0027654 · Cited by 18
Moral, S. S., Delgado, S. O., Benavente, D., & del Cura, M. Á. G. (2002) · Sedimentary Geology · doi:10.1016/s0037-0738(01)00219-6 · Cited by 17
Richardson, C. D., Hinman, N. W., McHenry, L. J., Kotler, J. M., Knipe, D., & Scott, J. R. (2012) · Planetary and Space Science · doi:10.1016/j.pss.2012.02.002 · Cited by 17
Chidambaram, S., Bhandary, H., & Ali, A. (2021) · Environmental Earth Sciences · doi:10.1007/s12665-021-09924-9 · Cited by 17
“Subsequent to the precipitation of calcite with higher concentration of HCO3, they lead to the formation of Alkali brine (Eugster 1980).”
BackgroundDaswani, M. M., & Kite, E. S. (2017) · Journal of Geophysical Research Planets · doi:10.1002/2017je005319 · Cited by 18
“In contrast, Cl in terrestrial endorheic lakes is largely leached and mobilized from surrounding basin rocks [Eugster and Hardie, 1978; Eugster, 1980].”
BackgroundInfluentialSoltaninejad, A., Ranjbar, H., Honarmand, M., & Dargahi, S. (2017) · Carbonates and Evaporites · doi:10.1007/s13146-017-0339-4 · Cited by 15
“…University of Advanced Technology, Mahan, Iran 4 Department of Geology, Shahid Bahonar University of Kerman, Kerman, Iran largely depends on unstable lithologies that are leached and altered by inflow waters in the drainage basin surrounding a salt lake (Eugster 1980; Hardie and Eugster 1970).”
BackgroundThe trace metal geochemistry of pore water brines from two hypersaline lakes
Lyons, W. B., Spencer, M. J., Hines, M. E., et al. (1988) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(88)90082-8 · Cited by 16
Origin of ore-forming fluids of Mississippi Valley-type (MVT) Pb-Zn deposits in Kangdian area, China
Jiangzhen, W., Li, Z., & Ni, S. (2003) · Acta Geochimica · doi:10.1007/bf02840410 · Cited by 15
“Subaerial evaporative basins are hydrologically closed or restricted ( the rate of evaporation must exceed the rate of inflow), a condition that is met particularly in arid to semi-arid climates ( Eugster, 1980 ).”
BackgroundTorres-Ruíz, J., Pesquera, A., & Sánchez‐Vizcaíno, V. L. (2003) · Mineralogical Magazine · doi:10.1180/0026461036730114 · Cited by 15
“Evaporites typically contain high concentrations of B (Eugster, 1980; Kyle, 1991).”
BackgroundFacies models for Australian precambrian evaporites
Muir, M. D. (2005) · Springer eBooks · doi:10.1007/bfb0010097 · Cited by 14
“Table i. Stratigraphy of the Abu Dhabl sabKha (after Butler, 1969 ), compared wlth that of tlqe Amelia Dolomite and Hallapunyah Formation.”
BackgroundResultYe, C., Mao, J., Ren, Y., et al. (2018) · Aquatic Geochemistry · doi:10.1007/s10498-018-9340-3 · Cited by 13
“The basic idea of the chemical divide rule is that when a binary salt is precipitated, and the initial molar proportion of the two ions forming this salt is not equal in solution, further evaporation will result in an increase in the concentration of the ion present in greater relative concentration in solution and a…”
BackgroundMethodInfluentialTao, K., Cao, J., Wang, Y., et al. (2020) · Energy & Fuels · doi:10.1021/acs.energyfuels.0c01333 · Cited by 13
TES and THEMIS study of proposed paleolake basins within the Aeolis quadrangle of Mars
Stockstill‐Cahill, K. R., Moersch, J. E., McSWEEN, H. Y., Jr., Piatek, J. L., & Christensen, P. R. (2007) · Journal of Geophysical Research Atmospheres · doi:10.1029/2005je002517 · Cited by 14
“evaporites often display a characteristic (bull’s-eye) spatial pattern resulting from their order of deposition [Jones, 1965; Eugster and Hardie, 1978; Eugster, 1980].”
BackgroundFreshwater inflows to closed basins of the Andean plateau in Chile, Argentina, and Bolivia
Kirshen, A., Moran, B., Munk, L., Russo, A. A., McKnight, S., Jenckes, J., Corkran, D., Bresee, M., & Boutt, D. F. (2025) · Communications Earth & Environment · doi:10.1038/s43247-025-02130-6 · Cited by 18
Önalgıl, N., Kadır, S., Külah, T., et al. (2014) · Journal of African Earth Sciences · doi:10.1016/j.jafrearsci.2014.10.020 · Cited by 12
Depositional Chemistry and Hydrology
Warren, J. K. (2016) · Springer eBooks · doi:10.1007/978-3-319-13512-0_2 · Cited by 12
Oehlert, A. M., Suosaari, E. P., Kong, T., Piggot, A. M., Maizel, D., Lascu, I., Demergasso, C. S., Chong, G., & Reid, R. P. (2022) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2022.155378 · Cited by 12
Geochemistry of Evaporites in Lacustrine Basin, Dongying Depression, Bohai Bay Basin, China
Zhonghong, C., Jiqing, Z., Li, W., et al. (2013) · Journal of Petroleum & Environmental Biotechnology · doi:10.4172/2157-7463.1000156 · Cited by 12
“In a closed hydrological system the composition of concentrated lake brines largely depends on labile lithologies that are leached and altered by inflow waters in the drainage basin surrounding a salt lake [17,18].”
BackgroundNjamnsi, N. Y., Njoh, O. A., Ngiamte, G. L., et al. (2022) · Journal of African Earth Sciences · doi:10.1016/j.jafrearsci.2022.104674 · Cited by 11
Nasri, N., Bouhlila, R., Saaltink, M. W., & Gamazo, P. (2014) · Applied Geochemistry · doi:10.1016/j.apgeochem.2014.11.003 · Cited by 11
“The genesis of these deposits is controlled by hydrology, sedimentology, chemistry and brine mineralogy (Eugster, 1980).”
BackgroundCheng, H., Hai, Q., Li, J., Song, J., & Ma, X. (2019) · Geofluids · doi:10.1155/2019/7808036 · Cited by 12
Vignoni, P., Jurikova, H., Schröder, B., Tjallingii, R., Córdoba, F., Lecomte, K., Pinkerneil, S., Grudzinska, I., Schleicher, A. M., Viotto, S. A., et al. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.11.032 · Cited by 10
Mayo, A. L., & Tingey, D. G. (2021) · Hydrogeology Journal · doi:10.1007/s10040-021-02371-7 · Cited by 10
“…great economic significance as sources of boron, iodine, lithium, magnesium, potassium, sodium sulfate, sodium carbonate, and tungsten (Hardie 1991; Eugster 1980; Riascher and Fritz 2009; Rosen 1994)—for example, one-third of the world’s lithium is from a single source, the Salar de Atacama in…”
BackgroundNeumann, K., Lyons, W. B., & Marais, D. J. D. (1998) · Annals of Glaciology · doi:10.3189/1998aog27-1-685-689 · Cited by 10
“Evidence of these changes can be fo und in the form of perched or fl ooded shorelines (G ilbert, 1890; J ones and others, 1971; Cutfi eld, 1974), and salt deposits in lake sed iments (H ard ie and others, 1978; Eugster, 1980).”
Steinmetz, R. L. L., Ávila, P., & Dávila, F. M. (2020) · Geomorphology · doi:10.1016/j.geomorph.2020.107032 · Cited by 11
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“The continuous increase in water salinity eventually led to a shift in the mineral precipitation from carbonate to evaporative salts, which cemented the nodules (Eugster, 1980).”
BackgroundTorfstein, A., & Turchyn, A. V. (2017) · Frontiers in Earth Science · doi:10.3389/feart.2017.00062 · Cited by 9
“…by low precipitation-to-evaporation ratios which result in the development of hypersaline water bodies and high deposition rates of evaporate minerals such as carbonate and gypsum (e.g., Great Salt Lake of Utah, Lake Chad of Central Africa, the Caspian Sea, and the Dead Sea; Eugster, 1980).”
BackgroundSchröder, T., Hoff, J. V. '., Ortíz, J. E., Torres, T., Sáez, J. A. L., Melles, M., Holzhausen, A., Wennrich, V., Viehberg, F., & Reicherter, K. R. (2017) · Quaternary International · doi:10.1016/j.quaint.2017.08.006 · Cited by 11
Soda lakes and origin of their trona deposits on the Nei Mongol Plateau of China
Dapeng, S. (1987) · Chinese Journal of Oceanology and Limnology · doi:10.1007/bf02843817 · Cited by 9
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“The combination of Na, K, Al, and Si observed in Figure 4d indicates the presence of sodic and potassium feldspars, characterized by igneous continental materials, modified through marine processes such as saline incrustations [72,73].”
Lameck, A. S., Saeed, O., & Boros, E. (2024) · Journal of Hydrology Regional Studies · doi:10.1016/j.ejrh.2024.101668 · Cited by 8
The engineering geology of playas, salt playas and salinas
Fookes, P. G., & Lee, E. M. (2018) · Quarterly Journal of Engineering Geology and Hydrogeology · doi:10.1144/qjegh2017-084 · Cited by 8
“The nature of the end product is defined by the input water chemistry (Eugster 1980).”
BackgroundMoran, B., Boutt, D. F., & Munk, L. (2019) · doi:10.31223/osf.io/katyv · Cited by 8
Fan, X., Wang, C., Teng, X., Kemp, D. B., Lu, Y., Yan, K., Wei, W., & Zhang, J. (2024) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2024.112283 · Cited by 7
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“Althoughmeteoric water contains small amounts of most of the main solutes, these are negligible compared with other sources such as rock weathering, and leaching and dissolution of pre-existing salts in sedimentary deposits (Eugster 1980; Nganje et al. 2015; Moayedi et al. 2019).”
BackgroundThe Precambrian continental record: A window into early Earth environments
Cosgrove, G. I. E., Colombera, L., & Mountney, N. P. (2024) · Precambrian Research · doi:10.1016/j.precamres.2023.107286 · Cited by 7
Hydrothermal Alteration of Etna Ash and Implications for Mars
Bloise, A., Cannata, C. B., & Rosa, R. D. (2020) · Minerals · doi:10.3390/min10050450 · Cited by 8
“Analcime formations also occur in highly alkaline lake waters [40], as a result of weathering of tephra [41], and, infrequently, as a primary magmatic product [39,42,43].”
BackgroundWarren, J. K. (2016) · Encyclopedia of earth sciences series/Encyclopedia of earth sciences · doi:10.1007/978-3-319-39193-9_100-1 · Cited by 7
Gu, A., & Eastoe, C. J. (2021) · Geosciences · doi:10.3390/geosciences11110455 · Cited by 6
“These seemingly conflicting requirements are reconciled in orographic deserts, where high mountains catch precipitation and generate rain shadows on neighboring basin floors [12].”
BackgroundLake Urmia Brine Evolution from 2007 to 2019
Lak, R., Mohammadi, A., & Khatooni, J. D. (2021) · The handbook of environmental chemistry · doi:10.1007/698_2021_807 · Cited by 6
Contemporary and relic waters strongly decoupled in arid alpine environments
Moran, B., Boutt, D. F., Munk, L., & Fisher, J. (2024) · PLOS Water · doi:10.1371/journal.pwat.0000191 · Cited by 9
The Mojave Vadose Zone: A Subsurface Biosphere Analogue for Mars
Abbey, W. J., Salas, E. C., Bhartia, R., & Beegle, L. W. (2013) · Astrobiology · doi:10.1089/ast.2012.0948 · Cited by 6
“Minerals that form in a closed-basin evaporitic environment typically precipitate in a specific sequence depending upon their solubilities; in order from least to most soluble ( i.e., first to last), this order is carbonates, sulfates, borates, halides, and nitrates (Eugster, 1980; Kendall, 1992).”
Suosaari, E. P., Oehlert, A. M., Lascu, I., et al. (2022) · Geosciences · doi:10.3390/geosciences12060247 · Cited by 6
“Evaporation and subsurface water–rock interactions significantly influence brine composition across this gradien [4–7].”
BackgroundWagner, B., Ortlepp, S., Kenig, F., et al. (2010) · Antarctic Science · doi:10.1017/s0954102010000556 · Cited by 6
“…sessionid5&docid5knb-lter-mcm.88, accessed 8 July 2010; Lyons & Welch, http://metacat.lternet.edu:8080/ knb/metacat?action5read&qformat5 mcm&sessionid5&docid5knb-ltermcm.62, accessed 12 December 2009). brine at the lake bottom overlain by fresher surface water (Eugster 1980).”
BackgroundFactors leading to sub-surface pan silcrete formation in north-central Botswana
Ringrose, S., Cassidy, L., Diskin, S., et al. (2023) · South African Journal of Geology · doi:10.25131/sajg.126.0003 · Cited by 5
Isotopes Applications in Earth Sciences
Rahman, R. O. A. (2019) · IntechOpen eBooks · doi:10.5772/intechopen.77560 · Cited by 5
Mayo, A. L., Tingey, D. G., Rey, K. A., et al. (2020) · Hydrogeology Journal · doi:10.1007/s10040-020-02209-8 · Cited by 5
“…studies have been conducted on groundwater flow in large and small groundwater systems in endorheic basins (Chen et al. 2014; Corenthal et al. 2014; Eugster 1980; Fisher and Kreitler 1987; Johnson et al. 2010; Mayo et al. 2007; Mayo et al. 2010; Miguel et al. 2005; Ortega-Guerrero 2003; Tejeda et…”
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Warren, J. K. (2018) · Encyclopedia of earth sciences series/Encyclopedia of earth sciences · doi:10.1007/978-3-319-39312-4_100 · Cited by 5
Deciphering the origin of dubiofossils from the Pennsylvanian of the Paraná Basin, Brazil
Saldanha, J. P., Cagliari, J., Horodyski, R. S., Mouro, L. D., & Pacheco, M. L. A. F. (2023) · Biogeosciences · doi:10.5194/bg-20-3943-2023 · Cited by 7
“Dawsonite is a common authigenic mineral that can have an acicular shape, more elongated than classes A and B; usually it forms in the eodiagenesis of continental alkaline saline environments, when pore water is concentrated in Al, or in mesodiagenetic CO2 storage environments (Eugster, 1980; Hellevang et al., 2013; X…”
BackgroundTemporal dynamics of inundation area, hydrochemistry and brine in Bakhtegan Lake, South-Central Iran
Vahidipour, M., Raeisi, E., & van der Zee, S. E. A. T. M. (2024) · Journal of Hydrology Regional Studies · doi:10.1016/j.ejrh.2024.101714 · Cited by 4
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“Salinity has a great influence on the type and distribution of minerals in the lacustrine basin, since different mineral types are formed at different stages of salinization in the lacustrine basin (Eugster 1980).”
Background杨, 江., 颜, 佳., 杜, 远., et al. (2014) · SCIENTIA SINICA Terrae · doi:10.1360/zd-2014-44-10-2172 · Cited by 3
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de Castro, A. P., Oste, J. T. F., Silva, W. D., & Borghi, L. (2026) · Journal of South American Earth Sciences · doi:10.1016/j.jsames.2026.106208 · Cited by 2
Kenny, R. (2017) · Acta Geochimica · doi:10.1007/s11631-016-0138-y · Cited by 2
“…requires either: (1) elevated pH values likely due to the polymerization of H4SiO4 which generally occurs under warm and/or arid climate conditions (Eugster 1980); and/or, (2) solute concentration fluctuations (Hesse 1989) usually occurring as a result of an influx of waters interacting with a…”
BackgroundDas, D., Turner, S. M. R., Schwenzer, S. P., Gasda, P. J., Palandri, J. L., Berlo, K., Léveillé, R., Crossey, L. J., Tutolo, B. M., Clegg, S. M., et al. (2025) · Meteoritics and Planetary Science · doi:10.1111/maps.14375 · Cited by 2
“These form as a result of fluid evaporation or freezing, and their chemical and physical characteristics are representative of their parent fluid compositions and surrounding environment (Ba z bel & Schreiber, 2014; Eugster, 1980; Smykatz-Kloss & Roy, 2010).”
Les tourmalinites stratiformesàdravite d'origine colloïdale du Paléoprotérozoïque sénégalo-malien
Ndiaye, P. M., & Guillou, J.-J. (1997) · Journal of African Earth Sciences · doi:10.1016/s0899-5362(97)00039-0 · Cited by 2
Isotopic Application in High Saline Conditions
Li, M., Fang, X., Li, J., et al. (2019) · IntechOpen eBooks · doi:10.5772/intechopen.88532 · Cited by 2
“However, no two drainage basins have identical climatic and hydrologic conditions, and even adjacent basins can show striking variations in evaporite mineralogy [8].”
BackgroundShchipalkina, N. V., Koshlyakova, N. N., Pekov, I. V., et al. (2023) · The Canadian Journal of Mineralogy and Petrology · doi:10.3749/2200062 · Cited by 2
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McKnight, S. (2021) · Scholarworks (University of Massachusetts Amherst) · doi:10.7275/14209209 · Cited by 1
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“…weathering of surrounding rocks, dissolving and redeposition of previous chloride deposits, volcanic outgassing, and extraterrestrial delivery (Eugster, 1980; Haskin et al., 2005; E. K. Leask & Ehlmann, 2022; Rubin et al., 2002; Thomas et al., 2019; Warren, 2010) have been suggested on Mars,…”
Dendritic crystal pattern from a drying droplet: A distinctive feature of feng-flavor Baijiu
Fu, H., Zhong, Y., Cai, L., Cheng, T., Xia, Y., Jian, X., Liu, J., Li, Z., Luo, H., Wu, Z., et al. (2026) · Current Research in Food Science · doi:10.1016/j.crfs.2026.101324 · Cited by 1
“In multicomponent solutions, the phase that first reaches a sufficient supersaturation to overcome the nucleation barrier typically precipitates first, followed by other phases as their respective supersaturation thresholds are exceeded (De Yoreo and Vekilov, 2003; Eugster, 1980).”
Cheng, H.-D., Chen, Y., & Zhang, S. (2026) · Molecules · doi:10.3390/molecules31081269
“It typically forms thin and multiple layers of lacustrine–lagoonal salt in the basin, resulting in a large cumulative thickness [1,2].”
Ye, C., Zheng, M., Nie, Z., Lv, Y., & Wu, Q. (2016) · GEOCHEMICAL JOURNAL · doi:10.2343/geochemj.2.0421 · Cited by 1
“7), with the alkalinity usually expressed as HCO3 – (Eugster, 1980; Hardie and Eugster, 1970).”
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“Colluvium deposits were created when materials enter a stream channeled in quaternary strata as a result of regional erosion on topographic slopes [47].”
Diversity of inland playas and aspects of marginal calcium carbonate landform formation
Ringrose, S., & Cassidy, L. (2024) · Scottish Geographical Journal · doi:10.1080/14702541.2024.2400649 · Cited by 2
“This includes work by Neal (1969), Glennie (1970), Mabbutt (1977), Eugster and Hardie (1978), Hardie et al. (1978), Eugster (1980a), Eugster and Kelts (1983), Goudie and Pye (1983), Street-Perrott and Roberts (1983), Rosen (1994a, 1994b), Lowenstein and Hardie (1985), Bowler (1986), Torgersen et…”
Towards the Improvement of Salt Extraction from Lake Katwe Raw Materials in Uganda
Kasedde, H. (2015) · KTH Publication Database DiVA (KTH Royal Institute of Technology) · Cited by 1
A Characterization of Lake Abert Tufa Mounds Lake Abert, Oregon
Bartruff, A. (2000) · doi:10.15760/etd.1061 · Cited by 1
“7 A Lake Brine Evolution flow chart originally produced by Eugster and Hardie (1978) and modified by Warren (2010).”
BackgroundInfluentialMcKnight, S., Boutt, D. F., & Munk, L. (2020) · doi:10.31223/osf.io/ea783 · Cited by 1
Phase developments during natural evaporation simulation of Lake Katwe brine based on Pitzer's model
Kasedde, H., Kirabira, J. B., Bäbler, M. U., et al. (2014) · KTH Publication Database DiVA (KTH Royal Institute of Technology)
MODIFY OF EUGSTER & HARDIE BRINE EVOLUTION FLOW DIAGRAM IN THE BASE OF BRINE OF MAHARLOU LAKE
Fayazi, F., Mohammad, N., & Lak, R. (2007)
DESERTIFICATION AND PLAYA EXPANSIONS IN EVERGLADES OF IRAN (CASE STUDY: MEGHAN LAKE)
Manije, G. T., Mirzakhani, B., & Askari, A. (2013)
Oveisi, K. (2021) · DOAJ (DOAJ: Directory of Open Access Journals) · doi:10.22108/coth.2020.117934.1307
Toala, F. J. M. (2018) · UPM Digital Archive (Technical University of Madrid) · doi:10.20868/upm.thesis.52306 · Cited by 1
Greensmith, J. T. (1989) · Springer eBooks · doi:10.1007/978-94-011-9640-6_13
Parthasarathy, K., Shailaja, R., Tamilarasan, G., et al. (2022) · Journal of the Geological Society of India · doi:10.1007/s12594-022-2105-z
“…(Jones, 1966, p.181) Hardie-Eugster model of evaporite formation, classified five major water types in continental evaporite basins (Hardie,1970; Eugster, 1980), in which dilute meteoric water with equivalents Ca < [HCO3 – + CO3 2–], precipitates alkaline earth carbonates and evolves into…”
BackgroundSaldanha, J. P., Cagliari, J., Horodyski, R. S., et al. (2023) · Biogeosciences · doi:10.5194/bg-2023-56-rc1
Saldanha, J. P. (2023) · Biogeosciences · doi:10.5194/bg-2023-56-ac1
Saldanha, J. P., Cagliari, J., Horodyski, R. S., et al. (2023) · Biogeosciences · doi:10.5194/bg-2023-56-rc2
Saldanha, J. P. (2023) · Biogeosciences · doi:10.5194/bg-2023-56-ac2
Saldanha, J. P., Cagliari, J., Horodyski, R. S., et al. (2023) · Biogeosciences · doi:10.5194/bg-2023-56-rc4
Microplastic pollution in marine sea salts
Charles, P. E., Rajaram, R., Selvam, S., & Paramasivam, S. (2024) · Elsevier eBooks · doi:10.1016/b978-0-323-90980-8.00013-3
Metadata
- Authors
- Eugster, H. P.
- Corresponding author
- Eugster, H P
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 1980-05
- Volume
- 8
- Issue
- 1
- Pages
- 35-63
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2175368274
- Cited by
- 211
- References
- 0
- Citations by year
- 2026: 7 · 2025: 11 · 2024: 10 · 2023: 12 · 2022: 7 · 2021: 17 · 2020: 11 · 2019: 12 · 2018: 8 · 2017: 9 · 2016: 6 · 2015: 10 · 2014: 8 · 2013: 6 · 2012: 4
- FWCI
- 2.71
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Annual Review of Earth and Planetary Sciences (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- evaporite geochemistry, carbonatites, carbonate minerals, calcite, dolomite, ankerite, fractional crystallization, mantle-derived magma
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