Late-magmatic immiscibility during batholith formation: assessment of B isotopes and trace elements in tourmaline from the Land’s End granite, SW England-Reference-Cited by-同舟云学术

Late-magmatic immiscibility during batholith formation: assessment of B isotopes and trace elements in tourmaline from the Land’s End granite, SW England

Published:2015-06 Issue:6 Volume:169 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Drivenes Kristian,Larsen Rune B.,Müller Axel,Sørensen Bjørn E.,Wiedenbeck Michael,Raanes Morten P.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-015-1151-6.pdf

Reference105 articles.

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2. Bai TB, Koster van Groos AF (1999) The distribution of Na, K, Rb, Sr, Al, Ge, Cu, W, Mo, La, and Ce between granitic melts and coexisting aqueous fluids. Geochim Cosmochim Acta 63:1117–1131. doi: 10.1016/S0016-7037(98)00284-1

3. Balen D, Broska I (2011) Tourmaline nodules: products of devolatilization within the final evolutionary stage of granitic melt? Geol Soc Lond Spec Publ 350:53–68. doi: 10.1144/sp350.4

4. Brammal A, Harwood HF (1925) Tourmalinization in the Dartmoor granite. Mineral Mag 20:319–330

5. Breiter K, Ackerman L, Svojtka M, Müller A (2013) Behavior of trace elements in quartz from plutons of different geochemical signature: a case study from the Bohemian Massif, Czech Republic. Lithos 175–176:54–67. doi: 10.1016/j.lithos.2013.04.023

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