Ανορθίτης (Greek Wikipedia)

Analysis of information sources in references of the Wikipedia article "Ανορθίτης" in Greek language version.

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Warr, L.N. (2021). «IMA–CNMNC approved mineral symbols». Mineralogical Magazine 85 (3): 291-320. doi:10.1180/mgm.2021.43. Bibcode: 2021MinM...85..291W.
Bennett, Emma N.; Lissenberg, C. Johan; Cashman, Katharine V. (21 May 2019). «The significance of plagioclase textures in mid-ocean ridge basalt (Gakkel Ridge, Arctic Ocean)». Contributions to Mineralogy and Petrology 174 (6). doi:10.1007/s00410-019-1587-1.
Wenk, H.-R.; Wilde, W.R. (1 August 1973). «Chemical anomalies of Lunar plagioclase, described by substitution vectors and their relation to optical and structural properties». Contributions to Mineralogy and Petrology 41 (2): 89-104. doi:10.1007/BF00375035.

Warr, L.N. (2021). «IMA–CNMNC approved mineral symbols». Mineralogical Magazine 85 (3): 291-320. doi:10.1180/mgm.2021.43. Bibcode: 2021MinM...85..291W.

J.R. Goldsmith (1980): «The melting and breakdown reactions of anorthite at high pressures and temperatures», Am. Mineralogist, τόμ. 65, σσ. 272-284

«Significant Lunar Minerals» (PDF). In Situ Resource Utilization (ISRU). NASA. Αρχειοθετήθηκε από το πρωτότυπο (PDF) στις 27 Μαΐου 2010. Ανακτήθηκε στις 23 Αυγούστου 2018.

Bennett, Emma N.; Lissenberg, C. Johan; Cashman, Katharine V. (21 May 2019). «The significance of plagioclase textures in mid-ocean ridge basalt (Gakkel Ridge, Arctic Ocean)». Contributions to Mineralogy and Petrology 174 (6). doi:10.1007/s00410-019-1587-1.

«Significant Lunar Minerals» (PDF). In Situ Resource Utilization (ISRU). NASA. Αρχειοθετήθηκε από το πρωτότυπο (PDF) στις 27 Μαΐου 2010. Ανακτήθηκε στις 23 Αυγούστου 2018.