Hercynian Fe-Mg Metasomatism in Cornwall

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چکیده

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Fe-Mg order-disorder in orthopyroxenes

Published data on the distribution of Fe and Mg between the two distinct octahedral sites (M1 and M2) in orthopyroxenes show that the equilibrium Fe-Mg distribution coefficient (KD) is roughly constant at intermediate ferrosilite content (XFs of 0.2 to 0.6) but at low XFs ( 0.2) is either anomalously high (Mössbauer data) or low (XRD data) compared to KD at intermediate XFs. We report an experi...

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ژورنال

عنوان ژورنال: Geological Magazine

سال: 1947

ISSN: 0016-7568,1469-5081

DOI: 10.1017/s001675680008242x