Eclogitic metagabbro from the Lanzada Window, eastern Central Alps: confirmation of subduction beneath the Malenco Unit
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geology
Link
http://link.springer.com/content/pdf/10.1007/s00015-014-0162-z.pdf
Reference114 articles.
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3. Austrheim, H., & Prestvik, T. (2008). Rodingitization and hydration of the oceanic lithosphere as developed in the Leka ophiolite, north-central Norway. Lithos, 104, 177–198.
4. Bachmann, R., Glodny, J., Oncken, O., & Seifert, W. (2009). Abandonment of the South Penninic—Austroalpine palaeosubduction zone, Central Alps, and shift from subduction erosion to accretion: constraints from Rb/Sr geochronology. Journal of the Geological Society, 166, 217–231.
5. Banerjee, N. R., Gillis, K. M., & Muehlenbachs, K. (2000). Discovery of epidosites in a modern oceanic setting, the Tonga forearc. Geology, 28, 151–154.
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1. Subduction of oceanic lithosphere in the Alps: Selective and archetypal from (slow-spreading) oceans;Earth-Science Reviews;2021-03
2. Deformation along the roof of a fossil subduction interface in the transition zone below seismogenic coupling: The Austroalpine case and new insights from the Malenco Massif (Central Alps);Geosphere;2020-02-13
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