Provenance reconstructions. Article 4. Modern methods for investigating detrital minerals (zircon, apatite)
Author:
Affiliation:
1. A.N. Zavaritsky Institute of Geology and Geochemistry, urals Branch of RAS
2. A.N. Zavaritsky Institute of Geology and Geochemistry, urals Branch of RAS, Institute of Geology, ufimian Federal Research Centre of RAS
Publisher
IGG UB RAS
Subject
Stratigraphy,Geochemistry and Petrology,Geology,Geophysics
Reference100 articles.
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2. Ahrens L.H., Cherry R.D., Erlank A.J. (1967) Observation on the Th-U relationship in zircons from granitic rocks and from kimberlites. Geochim. Cosmochim. Acta, 31(12), 2379-2387. DOI: https://doi.org/10.1016/0016-7037(67)90009-9
3. Andersen T. (2005) Detrital zircons as tracers of sedimentary provenance: limiting conditions from statistics and numerical simulation. Chem. Geol., 216(3-4), 249-270. DOI: https://doi.org/10.1016/j.chemgeo.2004.11.013
4. Andersen T., Griffin W.L., Jackson S.E., Knudsen T.-L. (2004) Mid-Proterozoic magmatic arc evolution at the southwest margin of the Baltic Shield. Lithos, 73(3-4), 289-318. DOI: https://doi.org/10.1016/j.lithos.2003.12.011
5. Andersen T., Griffin W.L., Pearson N.J. (2002) Crustal evolution in the SW part of the Baltic Shield: the Hf isotope evidence. J. Petrol., 43, 1725-1747. https://doi.org/10.1093/petrology/43.9.1725
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