Geochemical constraints of bulk rocks and in-situ zircon from the granitoids of the Hungund Schist Belt: An insight for hydrothermal activity
Author:
Funder
Department of Science and Technology, India
Ministry of Mines, India
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12040-022-01930-0.pdf
Reference101 articles.
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2. Alderton D H, Pearce J A and Potts P J 1980 Rare earth element mobility during granite alteration: Evidence from southwest England; Earth Planet Sci. Lett. 49 149–165.
3. Allen D E and Seyfried Jr W E 2005 REE controls in ultramafic hosted MOR hydrothermal systems: An experimental study at elevated temperature and pressure; Geochim. Cosmochim. Acta 69 675–683, https://doi.org/10.1016/j.gca.2004.07.016.
4. Badhe K V and Pandalai H S 2018 Evolution of Hutti–Maski greenstone belt of the Eastern Dharwar Craton: Evidence for metamorphic and hydrothermal phases from the Hira-Buddini deposit, Raichur district, Karnataka, India; J. Earth Syst. Sci. 127 1–15, https://doi.org/10.1007/s12040-018-0995-3.
5. Ballouard C P, Poujol M, Boulvais P, Branquet Y, Tartèse R and Vigneresse J L 2016 Nb–Ta fractionation in peraluminous granites: A marker of the magmatic–hydrothermal transition; Geology 44(3) 231–234, https://doi.org/10.1130/G37475.1.
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