Blar i forfatter Fakultet for naturvitenskap og teknologi "Faber, Carly"
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Anticlockwise metamorphic pressure–temperature paths and nappe stacking in the Reisa Nappe Complex in the Scandinavian Caledonides, northern Norway: evidence for weakening of lower continental crust before and during continental collision
Faber, Carly; Stunitz, Holger; Gasser, Deta; Jeřábek, Petr; Kraus, Katrin; Corfu, Fernando; Ravna, Erling Krogh; Konopásek, Jiří (Journal article; Tidsskriftartikkel; Peer reviewed, 2019)This study investigates the tectonostratigraphy and metamorphic and tectonic evolution of the Caledonian Reisa Nappe Complex (RNC; from bottom to top: Vaddas, Kåfjord, and Nordmannvik nappes) in northern Troms, Norway. Structural data, phase equilibrium modelling, and U-Pb zircon and titanite geochronology are used to constrain the timing and pressure–temperature (<i>P–T</i>) conditions of deformation ... -
Mountain building processes in the northern Norwegian Caledonides - Examining Caledonian continental collision using a combination of structural mapping, phase equilibrium modelling and geochronology
Faber, Carly (Doctoral thesis; Doktorgradsavhandling, 2018-01-17)Studying orogenesis allows us to better understand the construction of continental crust and the lower crustal processes that occur in modern orogenic belts (e.g. the Himalaya). The Scandinavian Caledonides formed when Laurentia and Baltica collided during the Silurian/Devonian, and allow for direct study of mid- to lower crustal metamorphism in a continental collision zone. This work focuses on the ... -
Structural and metamorphic history of the Leech river shear zone, Vancouver Island, British Columbia
Seyler, Caroline E.; Kirkpatrick, James D.; Faber, Carly; Licht, Alexis; Šilerová, Dina; Regalla, Christine (Journal article; Tidsskriftartikkel; Peer reviewed, 2022-10-13)The Leech River Shear Zone (LRSZ) on southern Vancouver Island separates the metasedimentary schists of the Leech River Complex (LRC) from the accreted oceanic plateau of the Siletz-Crescent terrane. The juxtaposition of these rock units suggests a possible origin as a subduction plate boundary but tectonic context of the LRSZ has yet to be fully established. We present field, microstructural, ...