Works matching AU Cambeses, Aitor
Results: 10
Drainage of subduction interface fluids into the forearc mantle evidenced by a pristine jadeitite network (Polar Urals).
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- Journal of Metamorphic Geology, 2021, v. 39, n. 4, p. 473, doi. 10.1111/jmg.12570
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Zircon stability grids in crustal partial melts: implications for zircon inheritance.
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- Contributions to Mineralogy & Petrology, 2021, v. 176, n. 3, p. 1, doi. 10.1007/s00410-021-01772-x
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The Quaternary Kurobegawa Granite: an example of a deeply dissected resurgent pluton.
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- Scientific Reports, 2021, v. 11, n. 1, p. 1, doi. 10.1038/s41598-021-01562-2
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From onset of Cadomian subduction to forearc-arc-continent collision: Insights from the Neoproterozoic Calzadilla Metaophiolite (SW Iberia).
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- International Geology Review, 2025, v. 67, n. 3, p. 257, doi. 10.1080/00206814.2024.2389566
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Accretion and subduction mass transfer processes: Zircon SHRIMP and geochemical insights from the Carboniferous Western Series, Central Chile.
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- International Geology Review, 2024, v. 66, n. 1, p. 54, doi. 10.1080/00206814.2023.2185822
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Relict abyssal mantle in a Caribbean forearc ophiolite (Villa Clara, central Cuba): petrogenetic and geodynamic implications.
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- International Geology Review, 2024, v. 66, n. 1, p. 196, doi. 10.1080/00206814.2023.2179229
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A reassessment of the amphibole-plagioclase NaSi-CaAl exchange thermometer with applications to igneous and high-grade metamorphic rocks.
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- American Mineralogist, 2021, v. 106, n. 5, p. 782, doi. 10.2138/am-2021-7400
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Fluid–Melt–Rock Interaction during the Transition from Magmatism to HT-UHT-Granulite- and Amphibolite-Facies Metamorphism in the Ediacaran Adrar–Suttuf Metamafic Complex, NW Margin of the West African Craton (Southern Morocco).
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- Journal of Petrology, 2024, v. 65, n. 6, p. 1, doi. 10.1093/petrology/egae049
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Precise Measurement of Magnesium Isotopes in Fe‐Mg Minerals Using a Multi‐collector SHRIMP Ion Microprobe.
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- Geostandards & Geoanalytical Research, 2024, v. 48, n. 2, p. 331, doi. 10.1111/ggr.12547
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Compositional Evolution of the Variscan Intra-Orogenic Extensional Magmatism in the Valencia del Ventoso Plutonic Complex, Ossa-Morena Zone (SW Iberia): A View from Amphibole Compositional Relationships.
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- Minerals (2075-163X), 2021, v. 11, n. 4, p. 431, doi. 10.3390/min11040431
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- Article