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Fluid inclusion geothermometry
Geologische Rundschau, 1977Fluid inclusions trapped within crystals either during growth or at a later time provide many clues to the histories of rocks and ores. Estimates of fluid-inclusion homogenization temperature and density can be obtained using a petrographic microscope with thin sections, and they can be refined using heating and freezing stages. Fluid inclusion studies,
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Fluid inclusions in migmatites
1985The fluid inclusions provide petrologists with the only direct method for studying a possible metamorphic fluid from a high P-T environment. Basic principles of a fluid inclusion study are as old as modern petrography (Sorby, 1858), but only in recent years have advances in the technology (heating-freezing stages), and in the understanding of fluid ...
J. Touret, Sakiko N. Olsen
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Journal of the Geological Society, 1988
A thematic session on fluid inclusions was held on 15–16 December 1986, at the University of Southampton as part of the annual meeting of the Mineral Deposits Studies Group and was supported by the Applied Mineralogy Group of the Mineralogical Society. Four of the papers are published in this volume (referees: D. H. M. Alderton, A. V. Bromley, R.
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A thematic session on fluid inclusions was held on 15–16 December 1986, at the University of Southampton as part of the annual meeting of the Mineral Deposits Studies Group and was supported by the Applied Mineralogy Group of the Mineralogical Society. Four of the papers are published in this volume (referees: D. H. M. Alderton, A. V. Bromley, R.
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Validation of LA-ICP-MS fluid inclusion analysis with synthetic fluid inclusions
American Mineralogist, 2005Laser ablation—inductively coupled plasma—mass spectrometry (LA-ICP-MS) has become recognized as a sensitive, efficient, and cost-effective approach to measuring the major-, minor-, and trace-solute compositions of individual fluid inclusions in minerals.
Allan, Murray M. +5 more
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Fluid inclusions: tectonic indicators
Journal of Structural Geology, 1999Abstract During the first half of the 20th century fluid inclusions have been studied in ore geology in order to determine the chemistry and physical parameters (density) of the mineralising fluids. Apart from a few pioneering works in the middle of the century, fluid inclusions were not used as structural markers before the late 1980s.
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Science, 2001
The reconstruction of past conditions on Earth involves a multitude of disciplines and techniques. In his Perspective, Goldstein highlights the potential of fluid inclusions in small halite or calcite crystals, formed, for example, when marine waters evaporate.
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The reconstruction of past conditions on Earth involves a multitude of disciplines and techniques. In his Perspective, Goldstein highlights the potential of fluid inclusions in small halite or calcite crystals, formed, for example, when marine waters evaporate.
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2020
Fluid inclusions are minute samples of fluids trapped in mineral cavities, which are generally smaller than 100 µm in diameter. Fluid inclusions in the mm-range are rather rare. The fluids were trapped during the growth or recrystallisation of the host mineral at a certain event in the geological history of the host rock.
Martin Okrusch, Hartwig E. Frimmel
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Fluid inclusions are minute samples of fluids trapped in mineral cavities, which are generally smaller than 100 µm in diameter. Fluid inclusions in the mm-range are rather rare. The fluids were trapped during the growth or recrystallisation of the host mineral at a certain event in the geological history of the host rock.
Martin Okrusch, Hartwig E. Frimmel
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1992
Proceedings of the 11th European Symposium on Fluid Inclusion Research (ECROFI).Special issue of European Journal of Mineralogy (ISNN 09035-1221)
DE VIVO, BENEDETTO, LATTANZI P, EDS
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Proceedings of the 11th European Symposium on Fluid Inclusion Research (ECROFI).Special issue of European Journal of Mineralogy (ISNN 09035-1221)
DE VIVO, BENEDETTO, LATTANZI P, EDS
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Fluid Inclusions and Isotopic Signatures
2016Low salinity aqueous fluid inclusion and arsenopyrite geothermobarometry support mineralogical estimates of mineralisation P-T conditions between 300° and 400 °C and 10–14 km depth. Isotopic data show that the mineralising fluids had extensive interaction with host rocks and/or were derived from the host rocks. Aditional input of some meteoric water is
Dave Craw, Doug MacKenzie
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Inclusion of Antioxidants in Resuscitation Fluids
1988Hemorrhagic shock is, whenever possible, treated with rapid volume replacement. Such treatment is often initiated by paramedical personnel as soon as possible following blood loss, e.g., at the site of an accident and during transport to an emergency room.
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