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  • 1
    Keywords: Igneous rocks Congresses Inclusions ; Magmas Congresses ; Volcanism Congresses ; Konferenzschrift ; Aufsatzsammlung ; Vulkanismus ; Mineralbildung ; Kristallisation ; Magma ; Schmelze ; Einschluss ; Fluideinschluss ; Geothermobarometrie ; Gesteinskunde ; Eruption ; Isotopengeochemie
    Type of Medium: Book
    Pages: XIV, 674 S , Ill., graph. Darst
    ISBN: 9780939950836
    Series Statement: Reviews in mineralogy and geochemistry 69
    DDC: 552/.1
    RVK:
    Language: English
    Note: The chapters in this volume represent an extensive review of the material presented by the invited speakers at a two-day short course on 'Minerals, Inclusions and Volcanic Processes' held prior to the annual fall American Geophysical Union meeting in San Francisco, California (December 13 - 14, 2008) , Introduction to minerals, inclusions and volcanic processes , Experimental studies of the kinetics and energetics of magma crystallization , Thermometers and barometers for volcanic systems , Thermometers and thermobarometers in granitic systems , Fluid inclusion thermobarometry as a tracer for magmatic processes , Petrologic reconstruction of magmatic system variables and processes , Magma ascent rates , Melt inclusions in basaltic and related volcanic rocks , Interpreting H₂O and CO₂ contents in melt inclusions : constraints from solubility experiments and modeling , Volatile abundances in basaltic magmas and their degassing paths tracked by melt inclusions , Inter- and intracrystalline isotopic disequilibria : techniques and applications , Oxygen Isotopes in mantle and crustal magmas as revealed by single crystal analysis , Uranium-series crystal ages , Time scales of magmatic processes from modeling the zoning patterns of crystals , Mineral textures and zoning as evidence for open system process , Decryption of igneous rock textures : crystal size distribution tools , Deciphering magma chamber dynamics from styles of compositional zoning in large silicic ash flow sheets
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  • 2
    Publication Date: 2011-12-01
    Description: This Geosphere themed issue is an outgrowth of our Penrose Conference: Origin and Uplift of the Sierra Nevada, California, which was held in Bridgeport, California, August 16–20, 2010. The theme is here expanded to include the Walker Lane (Fig. 1), since a large number of our Penrose abstracts were oriented to that topic, and because that region is no less a part of the Sierran story than the high peaks themselves. A fundamental question for the conference and themed issue is “How did the Sierra Nevada form?” The question can mean many things to disparate disciplines. One might refer to the age and origin of the rocks that form the Sierra Nevada batholith, or instead to the time at which such rocks were uplifted to form the topographic crest of the eastern Sierra. One might also speak to the origin of canyons and peaks formed by erosion as much as uplift, or to the time at which the Sierra's varied present-day ecological zones were established. The answers to these questions can be quite different, but are not necessarily independent, as insights from one may lend insight to another. Finally, the complete story of the Sierra also cannot be told without the tectonic forces that act on the Sierran crust, which involves the evolution of the San Andreas Fault system and the opening of the Gulf of California.
    Electronic ISSN: 1553-040X
    Topics: Geosciences
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  • 3
    Publication Date: 2020-02-07
    Description: We have refined the clinopyroxene-based hygrometer published by Armienti et al. (2013) for a better quantitative understanding of the role of H2O in the differentiation of Etnean magmas. The original calibration data set has been significantly improved by including several experimental clinopyroxene compositions that closely reproduce those found in natural Etnean products. To verify the accuracy of the model, some randomly selected experimental clinopyroxene compositions external to the calibration data set have been used as test data. Through a statistic algorithm based on the Mallows' C-P criterion, we also check that all model parameters do not cause data overfitting, or systematic error. The application of the refined hygrometer to the Mt. Etna 2011-2013 lava fountains indicates that most of the decreases in H2O content occur at P 〈 100 MPa, in agreement with melt inclusion data suggesting abundant H2O degassing at shallow crustal levels during magma ascent in the conduit and eruption to the surface.
    Description: Published
    Description: 2774–2777
    Description: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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