Relevant bibliographies by topics / Predazzo, Monzoni

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  1. Journal articles
  2. Dissertations / Theses

Academic literature on the topic 'Predazzo, Monzoni'

Author: Grafiati
Published: 9 March 2023
Last updated: 31 July 2025

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Journal articles on the topic "Predazzo, Monzoni"

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Princivalle, F., A. Della Giusta, A. De Min, and E. M. Piccirillo. "Crystal chemistry and significance of cation ordering in Mg-Al rich spinels from high-grade hornfels (Predazzo-Monzoni, NE Italy)." Mineralogical Magazine 63, no. 2 (1999): 257–62. http://dx.doi.org/10.1180/minmag.1999.063.2.11.

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AbstractTwo Mg-Al spinels (FAS1 and FAS2) in high-grade hornfels from the Toal de Mason skarn (Predazzo Monzoni, NE Italy) were investigated by means of single crystal X-ray diffraction and electron microprobe analysis in order to evaluate the last intra-crystalline closure temperature.The evidence provided by crystal chemical data from the investigated spinels, compared with that for two other spinels from a websterite dyke and a chlorite schist (TS2 and SP78a, respectively) with similar chemical characteristics, yielded a new empirical geothermometer. This allowed estimation of intra-crystal
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Alietti, Elisa, Maria Franca Brigatti, and Luciano Poppi. "The crystal structure and chemistry of high-aluminium phlogopite." Mineralogical Magazine 59, no. 394 (1995): 149–57. http://dx.doi.org/10.1180/minmag.1995.59.394.15.

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AbstractCrystal structure refinements were performed on five Al-rich phlogopite-1M crystals (1.50 ⩽ Al3+ ⩽ 1.97 atoms per formula unit) from skarns of the Predazzo and Monzoni Hills petrographic area (north-east Italy) with the aim of characterizing geometrical variation produced by Al3+ increase. The charge imbalance was mostly compensated for by substitutions of highly charged cations in the octahedral sheet (Al3+ and/or Fe3+ for Mg2+). The refinements were carried out in the mean space group C2/m and gave agreement values (R) between 0.025 and 0.030. For some additional crystals, only chemi
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Ferry, John M., Boswell A. Wing, Sarah C. Penniston-Dorland, and Douglas Rumble. "The direction of fluid flow during contact metamorphism of siliceous carbonate rocks: new data for the Monzoni and Predazzo aureoles, northern Italy, and a global review." Contributions to Mineralogy and Petrology 142, no. 6 (2001): 679–99. http://dx.doi.org/10.1007/s00410-001-0316-7.

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4

Lustrino, Michele, Hassan Abbas, Samuele Agostini, Marcello Caggiati, Eugenio Carminati, and Piero Gianolla. "Origin of Triassic magmatism of the Southern Alps (Italy): Constraints from geochemistry and Sr-Nd-Pb isotopic ratios." June 6, 2019. https://doi.org/10.1016/j.gr.2019.04.011.

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During Middle-early Late Triassic (∼243–235?Ma) a diffuse igneous activity developed in the Southern Alps (Italy). Sparse lava flow and pyroclastic succession remnants of such Southern Alps Triassic Igneous Rocks (SATIR) crop out in the Brescian Prealps, the Vicentinian Alps (Recoaro-Schio-Posina), Non Valley, Dolomites and Julian Alps. Plutonic rocks are found in two main plutonic complexes (Monzoni and Predazzo) and a small stock (Cima di Pape). Coeval igneous products can be traced eastward to Austria and Dinarides, for a total length of ∼450?km.
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Nardini, Nicolò, Federico Casetta, Chiara Maria Petrone, Yannick Buret, Theodoros Ntaflos, and Massimo Coltorti. "Modelling ancient magma plumbing systems through clinopyroxene populations: a case study from Middle Triassic volcanics (Dolomites, Italy)." Contributions to Mineralogy and Petrology 179, no. 3 (2024). http://dx.doi.org/10.1007/s00410-024-02102-7.

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AbstractModelling plumbing systems dynamics of active volcanoes through textural and chemical studies of mineral phases is crucial to unravel their eruptive behaviour, but it is rarely applied in ancient volcanic and volcano-plutonic systems. Here, we present an investigation of the architecture, magma dynamics and pre-eruptive timing of Middle Triassic plumbing systems in the Dolomites area (Southern Alps) through a detailed investigation of textures and compositional zoning of clinopyroxenes in lavas and dykes from Predazzo, Mt. Monzoni, Cima Pape and Sciliar volcano-plutonic complexes. The
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Dissertations / Theses on the topic "Predazzo, Monzoni"

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Filipponi, Alessandro. "Modellizzazione petrogenetica dell’origine e dell’evoluzione dei complessi intrusivi di Predazzo e dei Monti Monzoni." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2018. http://amslaurea.unibo.it/15559/.

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I Complessi Intrusivi di Predazzo e dei Monti Monzoni hanno età Ladinica (circa 220-240 Ma) e sono intrusi nelle sequenze carbonatiche del Triassico medio-inferiore delle Dolomiti Occidentali. L’affinità shoshonitica che li caratterizza è in apparente contrasto con il regime geodinamico estensionale esistente. Le teorie evolutive proposte per motivare questa impronta sono molteplici: fusione parziale di un mantello metasomatizzato, subduzione, transpressione, miscelamento tra magmi mantellici e crostali. Tutte le analisi disponibili in letteratura definiscono, su diagrammi di Harker e multiele
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CASETTA, Federico. "Thermobarometry, geochronology and petrological evolution of the Middle-Late Triassic magmatic products in the Dolomitic Area (Southern Alps)." Doctoral thesis, Università degli studi di Ferrara, 2019. http://hdl.handle.net/11392/2487850.

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The Middle Triassic magmatic event in the Dolomitic Area is represented by huge amounts of basaltic/trachybasaltic to trachytic volcanic and volcanoclastic rocks surrounding three main intrusive bodies (Predazzo, Mt. Monzoni and Cima Pape), with pyroxenitic/gabbroic to syenitic and syenogranitic composition. Geochemically, both the volcanic and the plutonic rocks are characterized by orogenic-like (high-K calc-alkaline to shoshonitic) affinity. Lamprophyric dykes with alkaline affinity constitute an additional and volumetrically limited pulse, thought to represent the ultimate stage of the mag
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