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hydrohalite

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Journal Article

Halite and Hydrohalite from Lake Bonney, Taylor Valley, Antarctica

James R. Craig, Richard D. Fortner, Barren L. Weand
Journal: Geology
Published: 01 August 1974
Geology (1974) 2 (8): 389–390.
DOI: https://doi.org/10.1130/0091-7613(1974)2<389:HAHFLB>2.0.CO;2
...James R. Craig; Richard D. Fortner; Barren L. Weand Abstract Halite (NaCl) and hydrohalite (NaCl·2H 2 O) have been found in the bottom sediments of Lake Bonney. These salts are in contact with the hypersaline bottom waters of the lake at depths below 28 m and occur with gypsum and calcite; a porous...
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The ternary system H 2 O–NaCl–CaCl 2 with plotted ice and <span class="search-highlight">hydrohalite</span> melt...

The ternary system H 2 O–NaCl–CaCl 2 with plotted ice and hydrohalite melt...

Published: 01 June 2018
Fig. 11. The ternary system H 2 O–NaCl–CaCl 2 with plotted ice and hydrohalite melting temperatures. Red dots denote ternary fluid compositions for fluid inclusions in Qtz-1; dashed range denotes binary H 2 O–NaCl mixtures in Qtz-1 and Qtz-2.
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Summary of melting temperatures of ice and <span class="search-highlight">hydrohalite</span> in individual type 4...

Summary of melting temperatures of ice and hydrohalite in individual type 4...

Published: 12 December 2014
F ig . 11. Summary of melting temperatures of ice and hydrohalite in individual type 4 L-V aqueous inclusions hosted by quartz from quartz-carbonate veins, plotted in the H 2 O–NaCl–CaCl 2 ternary diagram of Oakes et al. (1990) .
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(a) Raman spectrum of <span class="search-highlight">hydrohalite</span> at −190°C with six Gaussian–Lorentzian co...

(a) Raman spectrum of hydrohalite at −190°C with six Gaussian–Lorentzian co...

Published: 01 October 2004
F ig . 10. (a) Raman spectrum of hydrohalite at −190°C with six Gaussian–Lorentzian contributions, Δν 1   hh , Δν 2   hh and Δν 3   hh , Δν 4   hh , Δν 5   hh and Δν 6   hh . (b) Raman spectra of hydrohalite at −190°, −110° and −30°C, illustrating the shift of Gaussian–Lorentzian contributions
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(a) Raman spectrum of <span class="search-highlight">hydrohalite</span> at −190°C with six Gaussian–Lorentzian co...

(a) Raman spectrum of hydrohalite at −190°C with six Gaussian–Lorentzian co...

Published: 01 October 2004
F ig . 10. (a) Raman spectrum of hydrohalite at −190°C with six Gaussian–Lorentzian contributions, Δν 1   hh , Δν 2   hh and Δν 3   hh , Δν 4   hh , Δν 5   hh and Δν 6   hh . (b) Raman spectra of hydrohalite at −190°, −110° and −30°C, illustrating the shift of Gaussian–Lorentzian contributions
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COMPARISON OF PEAK VALUES AT −170°C FOR ICE, <span class="search-highlight">HYDROHALITE</span> AND MgCl 2 HYDRAT...

COMPARISON OF PEAK VALUES AT −170°C FOR ICE, HYDROHALITE AND MgCl 2 HYDRAT...

Published: 01 October 2004
TABLE 1. COMPARISON OF PEAK VALUES AT −170°C FOR ICE, HYDROHALITE AND MgCl 2 HYDRATE
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Laser induced nucleation of ice and hyrohalite (NaCl·2H 2 O) in a supercool...

Laser induced nucleation of ice and hyrohalite (NaCl·2H 2 O) in a supercool...

Published: 01 October 2007
) show the crystallization of ice whereas in (d)–(f) the crystallization of hydrohalite can be observed as a propagation of the phase boundary due to crystal growth. The vapour bubble is strongly compressed due to volume expansion of the ice and the hydrohalite. On subsequent heating, ice and hydrohalite
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Raman spectrum of a frozen synthetic fluid inclusions at −100°C with a comb...

Raman spectrum of a frozen synthetic fluid inclusions at −100°C with a comb...

Published: 01 October 2004
F ig . 9. Raman spectrum of a frozen synthetic fluid inclusions at −100°C with a combination of ice and hydrohalite peaks. The dashed curve is a Raman spectrum of pure ice, which is subtracted to obtain a signal resulting from hydrohalite only. HH: hydrohalite.
Journal Article

CRYOGENIC RAMAN SPECTROSCOPIC STUDIES IN THE SYSTEM NaCl–CaCl 2 –H 2 O AND IMPLICATIONS FOR LOW TEMPERATURE PHASE BEHAVIOR IN AQUEOUS FLUID INCLUSIONS

Iain M. Samson, Ryan T. Walker
Published: 01 February 2000
The Canadian Mineralogist (2000) 38 (1): 35–43.
DOI: https://doi.org/10.2113/gscanmin.38.1.35
...Iain M. Samson; Ryan T. Walker Abstract The character of Raman spectra in the O–H stretching region collected at low temperatures (~−180°C) from fine-grained aggregates of ice and salt hydrate (hydrohalite or antarcticite or both) in the system H 2 O–NaCl–CaCl 2 reflects the composition...
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Sequence of photographs showing phase changes during a heating-freezing cyc...

Sequence of photographs showing phase changes during a heating-freezing cyc...

Published: 01 December 2006
in the liquid phase. C) At −36.0°C, after occurrence of the first melting, a mixture of ice, hydrohalite, and aqueous liquid coexisted with a distorted vapor bubble. D) At −30.0°C ice, hydrohalite, and aqueous liquid are optically distinguishable. The vapor bubble expanded. E) At −25.5°C coarse crystals
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Ternary H 2 O-NaCl-CaCl 2 phase diagrams showing the major element composi...

Ternary H 2 O-NaCl-CaCl 2 phase diagrams showing the major element composi...

Published: 01 June 2021
Fig. 7. Ternary H 2 O-NaCl-CaCl 2 phase diagrams showing the major element composition of fluids in the Jinding deposit. Solid circles represent fluid inclusions with hydrohalite as the last melting phase, and their salinities were calculated from the ice- and hydrohalite-melting temperatures
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A) Comparison of the identified Raman spectra of a complex hydrate in the ...

A) Comparison of the identified Raman spectra of a complex hydrate in the ...

Published: 01 April 2008
Figure 11 A) Comparison of the identified Raman spectra of a complex hydrate in the high-salinity inclusions of cS-Dol with the standard spectra for magnesium-chloride hydrate (Ice + MH) and hydrohalite (Ice + HH) from Bakker (2004) . B) Raman spectrum of the metastable mixture
Journal Article

Petrography and Microthermometry of Fluid Inclusions in Apatite in the Turamdih Uranium Deposit, Singhbhum Shear Zone, Eastern India - An Insight into Ore Forming Fluid

Dipak C Pal, Trisrota Bhowmick
Published: 01 September 2015
Jour. Geol. Soc. India (2015) 86 (3): 253–262.
DOI: https://doi.org/10.1007/s12594-015-0310-8
... varies between ~ 22 to 43 wt % NaCl equivalents. Although, the final melting temperature of hydrohalite could not be determined due to very small size of the inclusions, the minimum concentrations of CaCl 2 was calculated considering the final ice melting temperature to be the hydrohalite melting...
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Journal Article

Characterization of Dolomitizing Fluids in the Carboniferous of the Cantabrian Zone (NW Spain): A Fluid-Inclusion Study with Cryo-Raman Spectroscopy

Marta Gasparrini, Ronald J. Bakker, Thilo Bechstädt
Published: 01 December 2006
Journal of Sedimentary Research (2006) 76 (12): 1304–1322.
DOI: https://doi.org/10.2110/jsr.2006.106
... in the liquid phase. C) At −36.0°C, after occurrence of the first melting, a mixture of ice, hydrohalite, and aqueous liquid coexisted with a distorted vapor bubble. D) At −30.0°C ice, hydrohalite, and aqueous liquid are optically distinguishable. The vapor bubble expanded. E) At −25.5°C coarse crystals...
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H 2 O-NaCl-CaCl 2 phase diagram showing the composition of the fluid inclu...

H 2 O-NaCl-CaCl 2 phase diagram showing the composition of the fluid inclu...

Published: 01 September 2017
Fig. 13. H 2 O-NaCl-CaCl 2 phase diagram showing the composition of the fluid inclusions from the Maw zone REE deposit. Circles with light blue color represent the inclusions with ice as the last melting phase, and circles with pink color represent inclusions with hydrohalite as the last melting
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Partial phase diagram for the ternary system H 2 O–NaCl–CaCl 2 (after Van...

Partial phase diagram for the ternary system H 2 O–NaCl–CaCl 2 (after Van...

Published: 01 October 2002
F ig . 17. Partial phase diagram for the ternary system H 2 O–NaCl–CaCl 2 (after Vanko et al. 1988 ) showing the bulk compositions for L H2O –V aqueous fluid inclusions hosted by quartz in pegmatite. The data plotted are for aqueous L–V inclusions in which both hydrohalite (HH) and ice
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F ig . 8. Microthermometric results of the fluid inclusions in ore-bearing ...

F ig . 8. Microthermometric results of the fluid inclusions in ore-bearing ...

Published: 01 August 2003
and II. C. Variation in T m (ice) of secondary fluid inclusions in a single secondary trail in late-stage calcite. D. Ternary H 2 O-NaCl-CaCl 2 diagram showing the modeled compositions of fluid inclusions in which hydrohalite melting could be measured. Gray area denotes the range in NaCl/CaCl 2 ratio
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Comparison of Raman spectra of a NaCl-rich glass (a) and a microcrystalline...

Comparison of Raman spectra of a NaCl-rich glass (a) and a microcrystalline...

Published: 01 October 2004
F ig . 12. Comparison of Raman spectra of a NaCl-rich glass (a) and a microcrystalline mixture of ice and hydrohalite (b) at −190°C.
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Raman spectra of frozen, natural fluid inclusions from the Oregon 3 graniti...

Raman spectra of frozen, natural fluid inclusions from the Oregon 3 graniti...

Published: 01 February 2000
contain peaks that can be assigned to ice and hydrohalite, at 3092 and 3536 cm −1 , respectively, and a series of composite peaks between 3350 and 3460 cm −1 that correspond to a mixture of hydrohalite and antarcticite ( cf . Fig. 1 ).
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The H 2 O-NaCl-CaCl 2 ratios of fluid inclusions in fracture-filling miner...

The H 2 O-NaCl-CaCl 2 ratios of fluid inclusions in fracture-filling miner...

Published: 01 October 2021
Figure 9. The H 2 O-NaCl-CaCl 2 ratios of fluid inclusions in fracture-filling minerals hosted by upper Carboniferous rocks (green) and Zechstein-2-Carbonate (red). equiv. = equivalent; HH = hydrohalite.