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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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Reference TypeJournal (article/letter/editorial)
TitleThe composition and origin of the Kef Lakhal amphibolites and associated amphibolite and olivine-rich enclaves, Edough, Annaba, NE Algeria
JournalMineralogical MagazineISSN0026-461X
AuthorsAhmid-Said, Y.Author
Leake, B. E.Author
Year1992 (December)Volume56
Issue385
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-385-459.pdf+
DOIdoi:10.1180/minmag.1992.056.385.02Search in ResearchGate
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Mindat Ref. ID1860Long-form Identifiermindat:1:5:1860:3
GUID0
Full ReferenceAhmid-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
Plain TextAhmid-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
In(1992, December) Mineralogical Magazine Vol. 56 (385) Mineralogical Society
Abstract/NotesAbstractThe 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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Ahmed-Said, Y., Leake, B. E. (1997) The petrogenesis of the Edough amphibolites, Annaba, NE Algeria: two unrelated basic magmas and the lherzolite-harzburgite residue of a possible magma source. Mineralogy and Petrology, 59 (3) 207-237 doi:10.1007/bf01161860
Ahmed-Said, Y., Leake, B.E., Rogers, G. (1993) The petrology, geochemistry and petrogenesis of the Edough igneous rocks, Annaba, NE Algeria. Journal of African Earth Sciences (and the Middle East), 17 (1) 111-123 doi:10.1016/0899-5362(93)90027-n
Ahmed-Said, Y., Leake, B.E. (1995) The petrogenesis of the Edough muscovite orthogneisses, Annaba, northeast Algeria. Journal of African Earth Sciences, 21 (2) 253-269 doi:10.1016/0899-5362(95)00071-z
Khudeir, Ali A., El Haddad, Mervet A., Leake, Bernard E. (1992) Compositional variation in chromite from the Eastern Desert, Egypt. Mineralogical Magazine, 56 (385) 567-574 doi:10.1180/minmag.1992.056.385.12
Leake, Bernard E. (1972) Garnetiferous striped amphibolites from Connemara, Western Ireland. Mineralogical Magazine, 38 (298) 649-665 doi:10.1180/minmag.1972.038.298.01
Ahmed-Said, Y., Leake, B. E. (1990) S-type granite formation in the Dalradian rocks of Connemara, W. Ireland. Mineralogical Magazine, 54 (374) 1-22 doi:10.1180/minmag.1990.054.374.02
Leake, Bernard E. (1968) Optical properties and composition in the orthopyroxene series. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (281) 745-747 doi:10.1180/minmag.1968.036.281.18
Lupini, L., Williams, C. T., Woolley, A. R. (1992) Zr-rich garnet and Zr- and Th-rich perovskite from the Polino carbonatite, Italy. Mineralogical Magazine, 56 (385) 581-586 doi:10.1180/minmag.1992.056.385.14
Kemp, A. J., Leake, B. E. (1975) Two hydrous-rich aluminous hornblendes. Mineralogical Magazine, 40 (311) 308-311 doi:10.1180/minmag.1975.040.311.12
Turner, Simon P., Stüwe, Kurt (1992) Low-pressure corona textures between olivine and plagioclase in unmetamorphosed gabbros from Black Hill, South Australia. Mineralogical Magazine, 56 (385) 503-509 doi:10.1180/minmag.1992.056.385.06
Hall, A. (1992) D. B. Clarke Granitoid rocks. London (Chapman and Hall), 1992. 283 pp. Price £24.95. Mineralogical Magazine, 56 (385) 619 doi:10.1180/minmag.1992.056.385.21
 
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