| Reference Type | Journal (article/letter/editorial) |
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| Title | The composition and origin of the Kef Lakhal amphibolites and associated amphibolite and olivine-rich enclaves, Edough, Annaba, NE Algeria |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Ahmid-Said, Y. | Author |
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| Leake, B. E. | Author |
| Year | 1992 (December) | Volume | 56 |
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| Issue | 385 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_56/56-385-459.pdf+ |
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| DOI | doi:10.1180/minmag.1992.056.385.02Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 1860 | Long-form Identifier | mindat:1:5:1860:3 |
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| GUID | 0 |
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| Full Reference | Ahmid-Said, Y., Leake, B. E. (1992) The composition and origin of the Kef Lakhal amphibolites and associated amphibolite and olivine-rich enclaves, Edough, Annaba, NE Algeria. Mineralogical Magazine, 56 (385) 459-468 doi:10.1180/minmag.1992.056.385.02 |
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| Plain Text | Ahmid-Said, Y., Leake, B. E. (1992) The composition and origin of the Kef Lakhal amphibolites and associated amphibolite and olivine-rich enclaves, Edough, Annaba, NE Algeria. Mineralogical Magazine, 56 (385) 459-468 doi:10.1180/minmag.1992.056.385.02 |
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| In | (1992, December) Mineralogical Magazine Vol. 56 (385) Mineralogical Society |
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| Abstract/Notes | AbstractThe Kef Lakhal amphibolitcs and associated amphibolitc and olivine-rich enclaves are dcscribcd and their major and trace element chemistry indicates that both amphibolites were evolved medium to high alumina tholeiitic basalts with talc-alkaline affinities probably formed within plate settings. The olivine-rich enclaves are disrupted periodotites of the type lherzolite-harzburgite and probably represent mantle residua after melting. |
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