CO2 fluid inclusion barometry in mantle xenoliths from central Mexico: A detailed record of magma ascent

Levresse, Gilles; Cruz, K. E. Cervantes‐de la; Aranda-Gómez, José Jorge; Dávalos-Elizondo, María Guadalupe; Jiménez‐Sandoval, S.; Rodriguez-Melgarejo, F.; Alba-Aldave, Leticia A.

doi:10.1016/j.jvolgeores.2015.11.012

Cited by 7 publications

(3 citation statements)

References 70 publications

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“…The spectra shown in absorbance units and wavenumbers (cm , in the mid-IR region. The Raman spectroscopy characterization of liquid and gaseous compounds, solid phases, and solute species in fluid inclusions is supported by studies and catalogs of reference spectra for main phases (Bény et al, 1982;Harvey and Butler, 1986;Dubessy et al, 1989;Rosso and Bodnar, 1995;Burke, 2001;Baumgartner and Bakker, 2009;White, 2009;Frezzotti et al, 2012;Levresse et al, 2016).…”

Section: Analytical Proceduresmentioning

confidence: 99%

Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study

Aguilera

Layana

Rodríguez-Díaz

et al. 2016

andgeo

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ABSTRACT.A multidisciplinary study that includes processing of Landsat ETM+ satellite images, chemistry of gas condensed, mineralogy and chemistry of fumarolic deposits, and fluid inclusion data from native sulphur deposits, has been carried out in the Lastarria Volcanic Complex (LVC) with the objective to determine the distribution and characteristics of hydrothermal alteration zones and to establish the relations between gas chemistry and fumarolic deposits. Satellite image processing shows the presence of four hydrothermal alteration zones, characterized by a mineral assemblage constituted mainly by clay minerals, alunite, iron oxides, and more subordinated ferrous minerals and goethite. Hydrothermal alteration zones present in the Lastarria sensu stricto volcano are directly related to the recent fumarolic activity. Geochemistry of fumarolic gas condensed, obtained from two fumaroles at temperatures between 328 and 320 °C, has allowed detecting 37 diverse elements corresponding to halogens, chalcophiles, siderophiles, alkali metals, alkali earth metals and Rare Earth Elements (REE), with concentrations that vary widely between 5,620 ppm (chlorine) and 0.01 ppm (Mo, Ag, Sn, Pb, Se, Mg and Cr). Logarithm of Enrichment Factor (log EF i ) for each element present values between 6.35 (iodine) and <1 (K, Na, Ca, Fe and Al). Those elements are originated primarily from a magmatic source, whereas at shallow level a hydrothermal source contributes typical rock-related elements, which are leached from the wall rock by a strong interaction with hyperacid fluids. Mostly of elements detected are transported to the surface in the fumarolic emissions as gaseous species, while very few elements (Mg, Ca and Al) are transported in silicate aerosols. A wide spectrum of minerals are present in the fumarolic deposits, which are constituted by sublimates and incrustations, and the main minerals phases are distributed in six mineral families, corresponding to sulphates, hydrated sulphates, sulphides, halides, carbonates, silicates and native element minerals. The sublimate/incrustation minerals are dominated by the presence of sulphate, sulphur, chlorine and diverse rock-related elements, which are formed by processes that include a. oxidation of gaseous phase; b. strong rock-fluid interaction; c. dissolution of silicate minerals and volcanic glass; d. gas-water interaction; e. deposition/precipitation of saline bearing minerals; f. oxidation of sublimates/incrustations to form secondary minerals and g. remobilization of sulphur deposits by meteoric water. Despite that sublimate/ incrustation minerals are dominated by rock-related elements, its chemistry shows high contents of high-volatile elements as As, Sb, Cd, among others. Fluid inclusions studies carried out in thin pseudobanded native sulphur from fumarolic deposits, by use of Raman and infrared spectroscopy combined with microthermometry analyses, provided evidence of H 2 O, CO 2 , H 2 S, SO 4 , COS bearing fluids, homogenization temperatures around 110 °C and salinities v...

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Section: Analytical Proceduresmentioning

confidence: 99%

Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study

Aguilera

Layana

Rodríguez-Díaz

et al. 2016

andgeo

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“…Therefore, the thermoelastic equilibrium might affect the microthermometric data. Recently, the elastic-plastic equilibrium of fluid inclusionhost mineral systems has been studied (e.g., Campione 2018) mainly for tracking volcanic plumbing systems (Levresse et al 2016;Oglialoro et al 2017) and for ascertaining the depth provenance of mantle xenolith (Yamamoto et al 2007(Yamamoto et al , 2012(Yamamoto et al , 2014) using the internal pressure of fluid inclusions. Consequently, it is important to consider the thermoelastic equilibrium in a pure CO 2host mineral system.…”

Section: ð1þmentioning

confidence: 99%

Thermoelastic equilibrium of fluid inclusion–host mineral systems under homogenization measurement

Hagiwara

Torimoto

Yamamoto

2019

Journal of Mineralogical and Petrological Sciences

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Microthermometric data of fluid inclusions can elucidate the physicochemical properties of lithospheric fluids, but the inclusions must satisfy several criteria to yield proper fluid information. One is the 'constant volume criterion': the inclusion volume must remain constant after being trapped. However, volume changes of fluid inclusions occur in nature during emplacement underground or uplifting to the surface. They can also occur during sample preparation or data collection in the laboratory. Therefore, thermoelastic deformation of the crystal lattice surrounding fluid inclusions during experiments might increase uncertainty about microthermometric data. Herein, we introduce and assess a method using the equation of state of pure CO 2 and thermoelastic equilibrium between a fluid inclusion and a host mineral to estimate fluid inclusion volume changes accurately during measurements of homogenization temperature. The estimation is valid if the inclusion and host are isotropically elastic, concentric spheres. Subsequently, we extended the equation of state to a more comprehensive Redlich and Kwong equation of state, which is applicable to more complicated fluid systems. Furthermore, for accurate treatment of the elastic effects involving an elastically anisotropic host mineral, we propose the method's application to an anisotropic host mineral. If physical properties of the host mineral and the molar volume of the fluid inclusion at an arbitrary temperature are known, then one can use this method for accurate estimation of the molar volume at a given temperature. This microthermometric data based method can accurately elucidate characteristics of the crust and mantle-fluid activity.

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“…Fluid inclusions with compositions approximated as CO 2 ‐rich systems are common in many geologic environments, including hydrothermal ore deposits, [ 1–3 ] medium‐grade to high‐grade metamorphic rocks, [ 1,4–7 ] and mantle xenoliths. [ 1,8,9 ] In many geological settings, the density of those fluid inclusions has been studied to track volcanic plumbing systems, [ 10–13 ] to ascertain the depth provenance of mantle xenoliths, [ 14–18 ] and to identify the pre‐eruptive volatile contents of magmas. [ 19–24 ] Although microthermometry is the principal method for estimating the density of CO 2 ‐rich inclusions, this method is effective only when inclusion is sufficiently large to measure the CO 2 homogenization temperature accurately because change in the fluid phase is determined using an optical microscope.…”

Section: Introductionmentioning

confidence: 99%

Temperature dependence of a Raman CO₂ densimeter from 23°C to 200°C and 7.2 to 248.7 MPa: Evaluation of density underestimation by laser heating

Hagiwara

Kawano

Takahata

et al. 2021

J Raman Spectroscopy

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Unintended local temperature enhancement by excitation laser might change Raman spectral features and potentially lead to misinterpretation of the data. To evaluate robustness of Raman CO2 densimeters in the presence of laser heating, we investigate the relation between temperature (T, °C), density (ρ, g/cm3), and Fermi diad split (Δ, cm−1) using a high‐pressure optical cell at 23°C to 200°C and 7.2–248.7 MPa. Results indicate that Δ decreases concomitantly with increasing temperature for a constant density in all density regions investigated. This result suggests that the density estimated based on Δ might be underestimated if the fluid is heated locally by the laser. Combining results of earlier studies with those of the present study indicates that the temperature dependence of Δ (|(∂Δ/∂T)ρ|) has a maximum value around 0.6–0.7 g/cm3. Consequently, at very high densities such as 1.1–1.2 g/cm3, |(∂Δ/∂T)ρ| is small. Thus, Δ at such densities is less affected by laser heating. However, at densities below approximately 0.7 g/cm3, although |(∂Δ/∂T)ρ| becomes smaller at lower densities, the relative density decrease becomes larger even for a small density decrease because the density itself becomes smaller. Therefore, at such densities, a density decrease of more than 10% was observed for some fluid inclusions, even at typical laser powers for inclusion analysis. Finally, to accurately estimate the density even in the presence of laser heating, we show that it is effective to estimate the intercept Δ from the correlation between Δ and laser power and substitute it into Δ–ρ relations.

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CO2 fluid inclusion barometry in mantle xenoliths from central Mexico: A detailed record of magma ascent

Cited by 7 publications

References 70 publications

Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study

Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study

Thermoelastic equilibrium of fluid inclusion–host mineral systems under homogenization measurement

Temperature dependence of a Raman CO₂ densimeter from 23°C to 200°C and 7.2 to 248.7 MPa: Evaluation of density underestimation by laser heating

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CO2 fluid inclusion barometry in mantle xenoliths from central Mexico: A detailed record of magma ascent

Cited by 7 publications

References 70 publications

Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study

Hydrothermal alteration, fumarolic deposits and fluids from Lastarria Volcanic Complex: A multidisciplinary study

Thermoelastic equilibrium of fluid inclusion–host mineral systems under homogenization measurement

Temperature dependence of a Raman CO2 densimeter from 23°C to 200°C and 7.2 to 248.7 MPa: Evaluation of density underestimation by laser heating

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Temperature dependence of a Raman CO₂ densimeter from 23°C to 200°C and 7.2 to 248.7 MPa: Evaluation of density underestimation by laser heating