Abstract
An overview of the significance and application of most common accessory minerals in igneous systems, mainly in granitic rocks is presented in two parts: (1) General description and definition of the most important accessory phases are given, and (2) a case study from Western Carpathians is dealt which unravels the granite typology. A short account of structure and composition of principal accessory phases is also discussed along with their occurrences, usage of isotopes and thermodynamic constraints which reveal the P-T evolution of parental igneous bodies.
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Acknowledgments
Grant agency Vega (project 2/0060/10 and 2/0159/13) and APVV (project 080-11) are thanked for financial support. Santosh Kumar is thanked for thoughtful review and thorough editorial work. Figures 2, 4, 5, 6, 8 and 11 are published with kind permission of the Veda Publishing House (Broska et al. 2012)
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Broska, I., Petrík, I. (2014). Accessory Phases in the Genesis of Igneous Rocks. In: Kumar, S., Singh, R. (eds) Modelling of Magmatic and Allied Processes. Society of Earth Scientists Series. Springer, Cham. https://doi.org/10.1007/978-3-319-06471-0_6
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