Abstract
The Round Top hypabyssal rhyolite laccolith is a highly evolved magmatic system, enriched in incompatible elements including REE [Rare Earth Element(s)], U, Be, and F. The Round Top intrusion is part of a series of Paleogene intrusions emplaced as the Sierra Blanca Complex. These intrusions are situated within long-lived, complex tectonic regimes that have been subjected to regional compression and subduction, punctuated by extensional bimodal volcanism. The enrichment in the rhyolite that comprises Round Top is the result of the prolonged removal of compatible elements from the source magma chamber through the emplacement of earlier magmatic events. With the emplacement of each sequential laccolith, the F-rich source magma became more enriched in incompatible elements, with increasing HREE [Heavy Rare Earth Elements(s)] concentrations. The emplacement of Round Top as a laccolith (versus that of an extrusive rhyolitic flow) facilitated the retention of the volatile-rich vapor phase within the magma, forming ubiquitous REE-bearing minerals, mainly yttrofluorite and yttrocerite. The high temperature mineral-vapor phase alteration of the feldspar groundmass was essential to the formation of REE minerals, where the pervasive open pore space was occupied by the late-crystallizing minerals. These late-forming REE-bearing minerals also occur as crystals associated with other accessory and trace phases, as inclusions within other phases, along grain boundaries, and along fractures and within voids. The rhyolite at Round Top and other laccolith intrusions in the Sierra Blanca Complex represent a new sub-type of magmatic rare earth element hosting system.
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Acknowledgements
We thank the Texas Rare Earth Resources Corporation for permission to conduct research on their property, assistance in conducting fieldwork, and providing access to existing maps, drill-hole data and samples, and previous studies. We are indebted to two anonymous experts as well as editor Daniel Harlov whose critical and constructive reviews helped to greatly improve the manuscript’s overall content and quality. The funding for this study was provided by the Jackson School of Geosciences and the State of Texas Advanced Resource Recovery (STARR) program through the University of Texas at Austin, Bureau of Economic Geology, Mineral Resource Program. This study was greatly enhanced by regional mapping products, produced by the University of Texas at Austin Bureau of Economic Geology, and funded through the United States Geological Survey Mapping Cooperative Program, STATEMAP Award No. G13AC00178. Additional support for O’Neill (2014) thesis research was provided by the III Yager Professorship of the Jackson School of Geosciences, the West Texas Geological Society, the Society of Economic Geologists, and the Association of Environmental and Engineering Geologists.
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O’Neill, L.C., Elliott, B.A. & Kyle, J.R. Mineralogy and crystallization history of a highly differentiated REE-enriched hypabyssal rhyolite: Round Top laccolith, Trans-Pecos, Texas. Miner Petrol 111, 569–592 (2017). https://doi.org/10.1007/s00710-017-0511-5
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DOI: https://doi.org/10.1007/s00710-017-0511-5