Abstract
Given the prolific work on the petrography and mineral chemistry of volcanic rocks to understand magmatic processes for well over a century, it is surprising that there are no quantitatively rigorous size classifications or commonly accepted terminologies regarding the origin of such crystals. This causes some confusion when attempting to make meaningful statements about the origin of crystals in porphyritic volcanic rocks. Here, more rigorous size and genetic terminologies for the crystals in volcanic rocks are proposed (size, cf. Table 1: ultrananolite, nanolite, microlite, microcryst, mesocryst, macrocryst, megacryst; genesis, cf. Table 2: autocryst, antecryst, xenocryst). And some caveats are discussed. The genetic terminology may also be employed when interpreting crystal zoning patterns and can be applied to crystal fragments. Adoption of the proposed size classification scheme is expected to lead to quantitatively more precise descriptions of the dimensions of the crystal cargo in volcanic rocks in the literature. Adoption of the proposed genetic terminology is expected to lead to less ambiguous discussions of the genetic processes that operate in magmatic systems in the lead-up to volcanic eruptions.
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Acknowledgements
GFZ thanks several members of the community for comments, discussions, and feedback during the drafting of this perspective, particularly Don Baker, Scott Bryan, Michele Lustrino, Silvio Mollo, Michihiko Nakamura, and Chiara Petrone. Mayumi Mujin and Charline Lormand kindly provided some images. Constructive reviews by Teresa Ubide and an anonymous reviewer, and the editorial handling and feedback of Jacopo Taddeucci, improved this paper. Support through a Long-term International Research Fellowship of the Japan Society for the Promotion of Science to GFZ is gratefully acknowledged.
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Zellmer, G.F. Gaining acuity on crystal terminology in volcanic rocks. Bull Volcanol 83, 78 (2021). https://doi.org/10.1007/s00445-021-01505-9
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DOI: https://doi.org/10.1007/s00445-021-01505-9