Reply to Thomas and Davidson on “A petrologic assessment of internal zonation in granitic pegmatites” (London, 2014a)
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference113 articles.
1. Dissolution of corundum and andalusite in H2O-saturated haplogranitic melts at 800°C and 200MPa: constraints on diffusivities and the generation of peraluminous melts;Acosta-Vigil;Journal of Petrology,2002
2. Dissolution of quartz, albite, and orthoclase in H2O-saturated haplogranitic melt at 800°C and 200MPa: diffusive transport properties of granitic melts at crustal anatectic conditions;Acosta-Vigil;Journal of Petrology,2006
3. Mechanisms of crustal anatexis: a geochemical study of partially melted metapelitic enclaves and host dacite, SE Spain;Acosta-Vigil;Journal of Petrology,2010
4. Are silicate-rich inclusions in spodumene crystallized aliquots of boundary layer melt?;Anderson;Geofluids,2013
5. The occurrence and origin of zabuyelite (Li2CO3) in spodumene-hosted fluid inclusions; implications for the internal evolution of rare-element granite pegmatites;Anderson;Canadian Mineralogist,2001
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3. Mapping Lithium-Bearing Pegmatite With Short-Wave Infrared (SWIR) Hyperspectral Imaging of Jingerquan Li–Be–Nb–Ta Pegmatite Deposit, Eastern Tianshan, NW China;IEEE Transactions on Geoscience and Remote Sensing;2024
4. Trace element partitioning in strongly peraluminous rare-metal silicic magmas – Implications for fractionation processes and for the origin of the Macusani Volcanics (SE Peru);Geochimica et Cosmochimica Acta;2024-01
5. The petrogenesis of highly fractionated gem-bearing pegmatites of Malawi: evidence from mica and tourmaline chemistry and finite step trace element modelling;Mineralium Deposita;2023-12-06
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