oa Granophyric Texture as a Possible Indicator of Magma Water Saturation and the Depth of Didkovychi-Type Granites Formation (Korosten Pluton, Ukrainian Shield)

References

1. Bezborodko, M.I. (1934). Monzonites of Ukraine.Ukraine geol. Institute of the Academy of Sciences of the Ukrainian SSR, 5, issue 2. Petrography. [in Ukrainian]
   [Google Scholar]
2. EklundO., ShebanovA. D. (1999). The origin of the rapakivi textures by sub-isothermal decompression.Precambrian Research., 95, 129–146.
   [Google Scholar]
3. HoltzF., JohannesW., TamicN., BehrensH. (2001). Maximum and minimum water contents of granitic melts generated in the crust: a reevaluation and implications.Lithos56, 1, 1–14.
   [Google Scholar]
4. LevkovskyyR.Z. (1975). Rapakivi. Nedra Publ., 223 p. [in Russian]
   [Google Scholar]
5. MytrokhynO.V. (2011). Anorthosite-rapakivigranite formation of the Ukrainian shield (geology, composition and conditions).Extended Abstract of Dr. Geol. Sci.: 04.00.01 – general and regional geology, 346 p. [in Ukrainian].
   [Google Scholar]
6. ShnyukovS. E. et al. (2018). Geochemical model of Precambrian granitoid magmatic evolution in the Korosten pluton (Ukrainian Shield): petrogenetic aspects and genesis of complex ore mineralization in metasomatic zones.Visnyk of Taras Shevchenko National University of Kyiv. Geology, 81, 12–22.
   [Google Scholar]
7. ShnyukovS.E. (2001). Widespread accessory minerals in geochemical modeling of magmatic processes.Zbirnik naukovih prats UkrDGRI0, 1–2, 41–53. [in Ukrainian].
   [Google Scholar]
8. ShnyukovS. E. (2002). Geochemical models of the magmatic systems and Earth’s continental crust evolution: potential source of petrophysical and ore genetic information.Geophysical Journal, 6, 201–219. [in Russian].
   [Google Scholar]
9. SukhorukovY. T. (1996). Petrological and geochemical aspects of the rapakivi ovoid origin. In: HaapalaI., RämöO. T., KosunenP. (eds.) Symposium on Rapakivi Granites and Related Rocks, Abstract Volume. University Press, p. 71.
   [Google Scholar]