| Reference Type | Journal (article/letter/editorial) |
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| Title | Origin of appinitic pockets in the diorites of Jersey, Channel Islands |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Key, Colin H. | Author |
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| Year | 1977 (June) | Volume | 41 |
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| Issue | 318 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_41/41-318-183.pdf+ |
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| DOI | doi:10.1180/minmag.1977.041.318.05Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 2758 | Long-form Identifier | mindat:1:5:2758:2 |
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| GUID | 0 |
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| Full Reference | Key, Colin H. (1977) Origin of appinitic pockets in the diorites of Jersey, Channel Islands. Mineralogical Magazine, 41 (318) 183-192 doi:10.1180/minmag.1977.041.318.05 |
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| Plain Text | Key, Colin H. (1977) Origin of appinitic pockets in the diorites of Jersey, Channel Islands. Mineralogical Magazine, 41 (318) 183-192 doi:10.1180/minmag.1977.041.318.05 |
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| In | (1977, June) Mineralogical Magazine Vol. 41 (318) Mineralogical Society |
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| Abstract/Notes | SummaryIsolated pockets of pegmatitic appinite characterized by hollow-shell, prismatic amphiboles are common in the Pre-Cambrian metagabbros and metasomatic diorites of Jersey. Field relationships and petrography indicate a liquid phase in the formation of these appinitic pockets, which are chemically distinct from the associated gabbros and diorites. Close chemical ties between appinites and host rocks, however, prove a replacive, metasomatic, rather than intrusive origin for the pockets. Significant enrichment in SiO2, K2O, and Na2O suggest that surrounding granite provided the metasomatic agents. The localized changes in composition of the basic rocks resulted in the formation of partially molten pockets from which the appinites crystallized. This mechanism probably necessitates a temperature in the region of 900 °C at 2–5 Kb PH2O: Fractured, hollow-shell, prismatic amphiboles of the pockets are consistent with quench crystallization, possibly due to the sudden loss of volatiles. An increase in the oxygen fugacity may have played a major role in inducing the rapid crystallization of kaersutitic amphibole. The envisaged conditions under which these changes took place are those of a high-level, sub-volcanic environment. |
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