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Grant Cawthorn, R. (1994) Formation of chlor- and fluor-apatite in layered intrusions. Mineralogical Magazine, 58 (391) 299-306 doi:10.1180/minmag.1994.058.391.12

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Reference TypeJournal (article/letter/editorial)
TitleFormation of chlor- and fluor-apatite in layered intrusions
JournalMineralogical MagazineISSN0026-461X
AuthorsGrant Cawthorn, R.Author
Year1994 (June)Volume58
Page(s)299-306Issue391
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_58/58-391-299.pdf+
DOIdoi:10.1180/minmag.1994.058.391.12Search in ResearchGate
Mindat Ref. ID2033Long-form Identifiermindat:1:5:2033:0
GUID6eb2fce3-0c79-44fb-89b8-82b792fad05f
Full ReferenceGrant Cawthorn, R. (1994) Formation of chlor- and fluor-apatite in layered intrusions. Mineralogical Magazine, 58 (391) 299-306 doi:10.1180/minmag.1994.058.391.12
Plain TextGrant Cawthorn, R. (1994) Formation of chlor- and fluor-apatite in layered intrusions. Mineralogical Magazine, 58 (391) 299-306 doi:10.1180/minmag.1994.058.391.12
In(1994, June) Mineralogical Magazine Vol. 58 (391) Mineralogical Society
Abstract/NotesAbstractApatite in most igneous intrusions has a high Cl/F ratio. However, chlor-apatite has been reported in the lower portions of the Bushveld and Stillwater Complexes. This has been used as evidence supporting the early separation of a Cl-rich discrete hydrous fluid in these intrusions. Mineralogical evidence is presented here to demonstrate that the Bushveld Complex, at least, formed from a nearly anhydrous magma, and did not release a hydrous fluid before apatite began to crystallize. It is suggested that apatite in the earliest cumulates equilibrated with trapped interstitial liquid, which converted it from the typical F-rich composition of cumulus apatite to a Cl-rich composition. This is an analogous process to that in which cumulus mafic minerals may become more Fe-rich on cooling and reaction with interstitial liquid.


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