Retrogressive hydration of calc-silicate xenoliths in the eastern Bushveld complex: evidence for late magmatic fluid movement

Autor:	C. J. Hatton, R.L. Gibson, T. Wallmach, S. A. de Waal
Rok vydání:	1995
Předmět:	chemistry.chemical_compound Mineral chemistry Metamorphic rock Magma Geochemistry Metamorphism Geology Xenolith Silicate Earth-Surface Processes
Zdroj:	Journal of African Earth Sciences. 21:633-646
ISSN:	1464-343X
DOI:	10.1016/0899-5362(95)00102-6
Popis:	Two calc-silicate xenoliths in the Upper Zone of the Bushveld complex contain mineral assemblages which permit delineation of the metamorphic path followed after incorporation of the xenoliths into the magma. Peak metamorphism in these xenoliths occurred at T =1100–1200°C and P CO 2
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::e59378088cdb9a19d5ea2d68f4834dd4 https://doi.org/10.1016/0899-5362(95)00102-6 Zobrazit plný text záznamu Full Text from ScienceDirect