Abstract
The mineral pumpellyite, W4X2Y4Z6O(20+t) (OH)(8−t) where W = Ca, Mn; X = (Mg, Fe2+, Mn)2−t (Fe3+, Al)t; Y = Fe3+, Al; Z = Si (ref. 1) is a well-known constituent of very low-grade metamorphic rocks, especially of metabasic compositions. Schiffmann and Liou2 have synthesized the ideal Fe-free endmember ‘Mg–-Al’ pumpellyite', Ca4MgAl5Si6O21(OH)7, and found its upper thermal stability to lie near 375–400 °C in the range of 5–8 kbar water pressure. Here we report the high-pressure synthesis of a pumpellyite-type phase in which the position W of the above formula is solely occupied by magnesium. This ‘Mg–Mg–Al pumpellyite’, which is chemically nearly equivalent to pyrope+H2O, crystallizes at 40–55 kbar, 700–850 °C. Therefore, it qualifies as a potential hydrous mantle phase in a subduction zone regime.
Similar content being viewed by others
References
Coombs, D. S., Nakamura, Y. & Vuagnat, M. J. Petrol. 17, 440–471 (1976).
Schiffman, P. & Liou, J. G. J. Petrol. 21, 441–474 (1980).
Schreyer, W., Baller, T. & Chopin, C. Terra cognita 5, 327 (1985).
Galli, E. & Alberti, A. Acta crystallogr. B25, 2276–2281 (1969).
Yoshiasa, A. & Matsumoto, T. Am. Miner. 70, 1011–1019 (1985).
Hölscher, A., Schreyer, W. & Lattard, D. Contr. Miner. Petrol. 92, 113–127 (1986).
Chopin, C. Contr. Miner. Petrol. 86, 107–118 (1984).
Ringwood, A. & Major, A. Earth planet. Sci. Lett. 2, 130–133 (1967).
Yamamoto, K. & Akimoto, S. Am. J. Sci. 277, 288–312 (1977).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Schreyer, W., Maresch, W., Medenbach, O. et al. Calcium-free pumpellyite, a new synthetic hydrous Mg–Al-silicate formed at high pressures. Nature 321, 510–511 (1986). https://doi.org/10.1038/321510a0
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1038/321510a0
- Springer Nature Limited
This article is cited by
-
The high-pressure stability of chlorite and other hydrates in subduction mélanges: experiments in the system Cr2O3–MgO–Al2O3–SiO2–H2O
Contributions to Mineralogy and Petrology (2014)
-
Retrograde evolution of eclogites: evidences from microstructures and 40Ar/39Ar white mica dates, M�nchberg Massif, northern Bavaria
Contributions to Mineralogy and Petrology (1992)