Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-223-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-223-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Post-entrapment modification of residual inclusion pressure and its implications for Raman elastic thermobarometry
Xin Zhong
CORRESPONDING AUTHOR
Physics of Geological Processes, The Njord Center, University of Oslo,
Oslo, Norway
Evangelos Moulas
Institute of Geosciences, Johannes Gutenberg University Mainz, Mainz,
Germany
Lucie Tajčmanová
Institute of Earth Sciences, Heidelberg University, Heidelberg, Germany
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Cited
44 citations as recorded by crossref.
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- A brief history of solid inclusion piezobarometry R. Angel et al. 10.5194/ejm-36-411-2024
- Garnet EoS: a critical review and synthesis R. Angel et al. 10.1007/s00410-022-01918-5
- Estimation of P-T entrapment conditions of a subduction fluid using elastic thermobarometry: A case study from Cabo Ortegal Complex, Spain T. Spránitz et al. 10.1016/j.lithos.2023.107171
- A new UHP unit in the Western Alps: First occurrence of coesite from the Monviso Massif (Italy) S. Ghignone et al. 10.2138/am-2022-8621
- Elastic Thermobarometry M. Kohn et al. 10.1146/annurev-earth-031621-112720
- Crystallographic Methods for Non-destructive Characterization of Mineral Inclusions in Diamonds R. Angel et al. 10.2138/rmg.2022.88.05
- Principle and geological applicability of the Raman elastic geothermobarometry for mineral inclusion systems G. XiaoYing et al. 10.18654/1000-0569/2021.04.02
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- Elastic Geobarometry for Anisotropic Inclusions in Anisotropic Host Minerals: Quartz‐in‐Zircon J. Gonzalez et al. 10.1029/2021JB022080
- Assessing P‐T variability in mélange blocks from the Catalina Schist: Is there differential movement at the subduction interface? K. Harvey et al. 10.1111/jmg.12571
- Garnet sand reveals rock recycling processes in the youngest exhumed high- and ultrahigh-pressure terrane on Earth S. Baldwin et al. 10.1073/pnas.2017231118
- Quartz-in-garnet (QuiG) under pressure: insights from in situ Raman spectroscopy N. Campomenosi et al. 10.1007/s00410-023-02026-8
- Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece M. Cisneros et al. 10.5194/se-12-1335-2021
- Elastic thermobarometry on metapelites across the crustal section of the Famatinian Arc, Argentina E. Giovanini et al. 10.1007/s00410-024-02115-2
- The effect of aqueous fluid on viscous relaxation of garnet and modification of inclusion pressures after entrapment X. Zhong et al. 10.1016/j.epsl.2024.118713
- Hidden intact coesite in deeply subducted rocks T. Taguchi et al. 10.1016/j.epsl.2021.116763
- Re-equilibration of quartz inclusions in garnet B. Pummell & J. Thomas 10.5194/ejm-36-581-2024
- Applications and Limitations of Elastic Thermobarometry: Insights From Elastic Modeling of Inclusion‐Host Pairs and Example Case Studies M. Cisneros & K. Befus 10.1029/2020GC009231
- Metamorphic P–T paths of Archean granulite facies metasedimentary lithologies from the eastern Beartooth Mountains of the northern Wyoming Province, Montana, USA: constraints from quartz-in-garnet (QuiG) Raman elastic barometry, geothermobarometry, and thermodynamic modeling L. Tuttle & D. Henry 10.5194/ejm-35-499-2023
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- Combined phase diagram modelling and quartz‐in‐garnet barometry of HP metapelites from the Kamieniec Metamorphic Belt (NE Bohemian Massif) J. Szczepański et al. 10.1111/jmg.12608
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- Measurement of crystallographic orientation of quartz crystal using Raman spectroscopy: application to entrapped inclusions X. Zhong et al. 10.1007/s00410-021-01845-x
- Geologic field evidence for non-lithostatic overpressure recorded in the North American Cordillera hinterland, northeast Nevada A. Zuza et al. 10.1016/j.gsf.2020.10.006
- Effect of Thermoelastic Properties of the Pyrope-Almandine Solid Solutions on the Entrapment Pressure of Garnet-Related Elastic Geobarometer B. Li et al. 10.3389/feart.2021.833405
- Experimental variable effects on laser heating of inclusions during Raman spectroscopic analysis Y. Hagiwara et al. 10.1016/j.chemgeo.2020.119928
- An exact solution to the Lame problem for a hollow sphere for new types of nonlinear elastic materials in the case of large deformations V. Levin et al. 10.1016/j.euromechsol.2021.104345
- Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet X. Chu et al. 10.1111/jmg.12690
- Insight Into the Early Exhumation of the Cycladic Blueschist Unit, Syros, Greece: Combined Application of Zoned Garnet Geochronology, Thermodynamic Modeling, and Quartz Elastic Barometry J. Gorce et al. 10.1029/2021GC009716
- Using the elastic properties of zircon-garnet host-inclusion pairs for thermobarometry of the ultrahigh-pressure Dora-Maira whiteschists: problems and perspectives N. Campomenosi et al. 10.1007/s00410-021-01793-6
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- Extensive fluid–rock interaction and pressure solution in a UHP fluid pathway recorded by garnetite, Lago di Cignana, Western Alps H. van Schrojenstein Lantman et al. 10.1111/jmg.12585
- The choice of a thermodynamic formulation dramatically affects modelled chemical zoning in minerals L. Tajčmanová et al. 10.1038/s41598-021-97568-x
- Resetting of zircon inclusions in garnet: Implications for elastic thermobarometry N. Campomenosi et al. 10.1130/G50431.1
- Modeling diffusion in ionic, crystalline solids with internal stress gradients B. Hess & J. Ague 10.1016/j.gca.2023.06.004
- Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet B. Cesare et al. 10.1016/j.epsl.2020.116708
- First evaluation of stiff-in-soft host–inclusion systems: experimental synthesis of zircon inclusions in quartz crystals J. Gonzalez et al. 10.1007/s00410-023-02081-1
- Quartz-in-garnet barometry constraints on formation pressures of eclogites from the Franciscan Complex, California M. Cisneros et al. 10.1007/s00410-021-01876-4
- Current applications using key mineral phases in igneous and metamorphic geology: perspectives for the future S. Volante et al. 10.1144/SP537-2022-254
- Thermal Structure of the Paleo‐Continental Subduction Zone: Insights From Quantitatively Constrained Prograde P–T Paths of Exhumed LT/UHP Eclogites in the Dabie Orogen M. Xia et al. 10.1029/2022GC010852
- Calculating pressure with elastic geobarometry: A comparison of different elastic solutions with application to a calc-silicate gneiss from the Rhodope Metamorphic Province E. Moulas et al. 10.1016/j.lithos.2020.105803
- Equation of state of spinel (MgAl2O4): constraints on self-consistent thermodynamic parameters and implications for elastic geobarometry of peridotites and chromitites Y. Hagiwara et al. 10.1007/s00410-022-01975-w
44 citations as recorded by crossref.
- On exhumation velocities of high-pressure units based on insights from chemical zoning in garnet (Tianshan, NW China) E. Schwarzenbach et al. 10.1016/j.epsl.2021.117065
- A brief history of solid inclusion piezobarometry R. Angel et al. 10.5194/ejm-36-411-2024
- Garnet EoS: a critical review and synthesis R. Angel et al. 10.1007/s00410-022-01918-5
- Estimation of P-T entrapment conditions of a subduction fluid using elastic thermobarometry: A case study from Cabo Ortegal Complex, Spain T. Spránitz et al. 10.1016/j.lithos.2023.107171
- A new UHP unit in the Western Alps: First occurrence of coesite from the Monviso Massif (Italy) S. Ghignone et al. 10.2138/am-2022-8621
- Elastic Thermobarometry M. Kohn et al. 10.1146/annurev-earth-031621-112720
- Crystallographic Methods for Non-destructive Characterization of Mineral Inclusions in Diamonds R. Angel et al. 10.2138/rmg.2022.88.05
- Principle and geological applicability of the Raman elastic geothermobarometry for mineral inclusion systems G. XiaoYing et al. 10.18654/1000-0569/2021.04.02
- Tectonic discontinuity, partial melting and exhumation in the Garhwal Himalaya (Northwest India): Constrains from spatial and temporal pressure-temperature conditions along the Bhagirathi valley R. Kawabata et al. 10.1016/j.lithos.2021.106488
- Elastic Geobarometry for Anisotropic Inclusions in Anisotropic Host Minerals: Quartz‐in‐Zircon J. Gonzalez et al. 10.1029/2021JB022080
- Assessing P‐T variability in mélange blocks from the Catalina Schist: Is there differential movement at the subduction interface? K. Harvey et al. 10.1111/jmg.12571
- Garnet sand reveals rock recycling processes in the youngest exhumed high- and ultrahigh-pressure terrane on Earth S. Baldwin et al. 10.1073/pnas.2017231118
- Quartz-in-garnet (QuiG) under pressure: insights from in situ Raman spectroscopy N. Campomenosi et al. 10.1007/s00410-023-02026-8
- Insights from elastic thermobarometry into exhumation of high-pressure metamorphic rocks from Syros, Greece M. Cisneros et al. 10.5194/se-12-1335-2021
- Elastic thermobarometry on metapelites across the crustal section of the Famatinian Arc, Argentina E. Giovanini et al. 10.1007/s00410-024-02115-2
- The effect of aqueous fluid on viscous relaxation of garnet and modification of inclusion pressures after entrapment X. Zhong et al. 10.1016/j.epsl.2024.118713
- Hidden intact coesite in deeply subducted rocks T. Taguchi et al. 10.1016/j.epsl.2021.116763
- Re-equilibration of quartz inclusions in garnet B. Pummell & J. Thomas 10.5194/ejm-36-581-2024
- Applications and Limitations of Elastic Thermobarometry: Insights From Elastic Modeling of Inclusion‐Host Pairs and Example Case Studies M. Cisneros & K. Befus 10.1029/2020GC009231
- Metamorphic P–T paths of Archean granulite facies metasedimentary lithologies from the eastern Beartooth Mountains of the northern Wyoming Province, Montana, USA: constraints from quartz-in-garnet (QuiG) Raman elastic barometry, geothermobarometry, and thermodynamic modeling L. Tuttle & D. Henry 10.5194/ejm-35-499-2023
- Life-cycle analysis of coesite-bearing garnet J. Schönig et al. 10.1017/S0016756821000017
- Large-strain Elastic and Elasto-Plastic Formulations for Host-Inclusion Systems and Their Applications in Thermobarometry and Geodynamics E. Moulas et al. 10.2475/001c.68195
- Combined phase diagram modelling and quartz‐in‐garnet barometry of HP metapelites from the Kamieniec Metamorphic Belt (NE Bohemian Massif) J. Szczepański et al. 10.1111/jmg.12608
- Approaches to the Solution of the Lamé–Gadolin Problem for a Composite Hollow Ball Made of Nonlinear Elastic and Elasto-Plastic Materials Under Superimposed Finite Deformations V. Levin et al. 10.1007/s11182-023-03044-6
- Measurement of crystallographic orientation of quartz crystal using Raman spectroscopy: application to entrapped inclusions X. Zhong et al. 10.1007/s00410-021-01845-x
- Geologic field evidence for non-lithostatic overpressure recorded in the North American Cordillera hinterland, northeast Nevada A. Zuza et al. 10.1016/j.gsf.2020.10.006
- Effect of Thermoelastic Properties of the Pyrope-Almandine Solid Solutions on the Entrapment Pressure of Garnet-Related Elastic Geobarometer B. Li et al. 10.3389/feart.2021.833405
- Experimental variable effects on laser heating of inclusions during Raman spectroscopic analysis Y. Hagiwara et al. 10.1016/j.chemgeo.2020.119928
- An exact solution to the Lame problem for a hollow sphere for new types of nonlinear elastic materials in the case of large deformations V. Levin et al. 10.1016/j.euromechsol.2021.104345
- Thermal pulse induced by emplacement of Ramba leucogranites in southern Tibet X. Chu et al. 10.1111/jmg.12690
- Insight Into the Early Exhumation of the Cycladic Blueschist Unit, Syros, Greece: Combined Application of Zoned Garnet Geochronology, Thermodynamic Modeling, and Quartz Elastic Barometry J. Gorce et al. 10.1029/2021GC009716
- Using the elastic properties of zircon-garnet host-inclusion pairs for thermobarometry of the ultrahigh-pressure Dora-Maira whiteschists: problems and perspectives N. Campomenosi et al. 10.1007/s00410-021-01793-6
- EntraPT: An online platform for elastic geothermobarometry M. Mazzucchelli et al. 10.2138/am-2021-7693CCBYNCND
- Extensive fluid–rock interaction and pressure solution in a UHP fluid pathway recorded by garnetite, Lago di Cignana, Western Alps H. van Schrojenstein Lantman et al. 10.1111/jmg.12585
- The choice of a thermodynamic formulation dramatically affects modelled chemical zoning in minerals L. Tajčmanová et al. 10.1038/s41598-021-97568-x
- Resetting of zircon inclusions in garnet: Implications for elastic thermobarometry N. Campomenosi et al. 10.1130/G50431.1
- Modeling diffusion in ionic, crystalline solids with internal stress gradients B. Hess & J. Ague 10.1016/j.gca.2023.06.004
- Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet B. Cesare et al. 10.1016/j.epsl.2020.116708
- First evaluation of stiff-in-soft host–inclusion systems: experimental synthesis of zircon inclusions in quartz crystals J. Gonzalez et al. 10.1007/s00410-023-02081-1
- Quartz-in-garnet barometry constraints on formation pressures of eclogites from the Franciscan Complex, California M. Cisneros et al. 10.1007/s00410-021-01876-4
- Current applications using key mineral phases in igneous and metamorphic geology: perspectives for the future S. Volante et al. 10.1144/SP537-2022-254
- Thermal Structure of the Paleo‐Continental Subduction Zone: Insights From Quantitatively Constrained Prograde P–T Paths of Exhumed LT/UHP Eclogites in the Dabie Orogen M. Xia et al. 10.1029/2022GC010852
- Calculating pressure with elastic geobarometry: A comparison of different elastic solutions with application to a calc-silicate gneiss from the Rhodope Metamorphic Province E. Moulas et al. 10.1016/j.lithos.2020.105803
- Equation of state of spinel (MgAl2O4): constraints on self-consistent thermodynamic parameters and implications for elastic geobarometry of peridotites and chromitites Y. Hagiwara et al. 10.1007/s00410-022-01975-w
Latest update: 04 Oct 2024
Short summary
In this study, we present a 1-D visco-elasto-plastic model in a spherical coordinate system to study the residual pressure preserved in mineral inclusions. This allows one to study how much residual pressure can be preserved after viscous relaxation. An example of quartz inclusion in garnet host is studied and it is found that above 600–700 °C, substantial viscous relaxation will occur. If one uses the relaxed residual quartz pressure for barometry, erroneous results will be obtained.
In this study, we present a 1-D visco-elasto-plastic model in a spherical coordinate system to...