Trace element geochemistry of zircons from the Kahnouj ophiolite complex: implications for petrogenesis and geodynamic setting
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://link.springer.com/content/pdf/10.1007/s12517-021-07575-5.pdf
Reference81 articles.
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2. Belousova EA, Walters S, Griffin WL, O’Reilly SY, Fisher NI (2002) Zircon trace-element compositions as indicators of source rock type. Contrib Mineral Petrol 143:602–622
3. Boudier F, Ceulenaar G, Nicolas A (1988) Shear zones, thrusts and related magmatism in the Oman ophiolite: initiation of thrusting on an ocean ridge. Tectonophysics 151:275–296
4. Brophy JG (2009) La–SiO2 and Yb–SiO2 systematics in mid-ocean ridge magmas: implications for the origin of oceanic plagiogranite. Contrib Mineral Petrol 158:99–111
5. Campbell LS, Compston W, Sircombe KN, Wilkinson CC (2014) Zircon from the East Orebody of the Bayan Obo Fe–Nb–REE deposit, China, and SHRIMP ages for carbonatite-related magmatism and REE mineralization events. Contrib Mineral Petrol 168:1041. https://doi.org/10.1007/s00410-014-1041-3
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1. The journey of the Band-e-Zeyarat ophiolite (Makran Accretionary Wedge, SE Iran) from the mid-ocean ridge to the accretionary complex: new insights from its sedimentary cover and associated basaltic dykes and sills;Journal of the Geological Society;2023-11-03
2. Petrogenesis and Tectonic Evolution of the Kahnouj Ophiolitic Complex (SE Iran): Constraints from geochemistry and Sr-Nd-Pb isotope composition;2023-07-18
3. Precise U–Pb zircon dates from silicic super-eruptions during late Ediacaran extension in the Avalonian Caledonia terrane of southern New Brunswick, Canada;Canadian Journal of Earth Sciences;2023-04-01
4. Origin of Fe Ti mineralization in the Late Jurassic to Early Cretaceous Kahnouj ophiolitic complex, Makran accretionary prism, SE Iran;Lithos;2022-10
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