The carbonatite-marble dykes of Abyan Province, Yemen Republic: the mixing of mantle and crustal carbonate materials revealed by isotope and trace element analysis
Dykes of carbonate rocks, that cut gneisses in the Lowder-Mudiah area of southern Yemen, consist of dolomite and/or calcite with or without apatite, barite and monazite. Petrographic observations, mineralogical, XRF and ICP-MS analyses reveal that some of the carbonate rocks are derived from sedimen...
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| Veröffentlicht in: | Mineralogy and petrology 2004-09, Vol.82 (1-2), p.105-135 |
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| creator | Le Bas, M. J. Ba-bttat, M. A. O. Taylor, R. N. Milton, J. A. Windley, B. F. Evins, P. M. |
| description | Dykes of carbonate rocks, that cut gneisses in the Lowder-Mudiah area of southern Yemen, consist of dolomite and/or calcite with or without apatite, barite and monazite. Petrographic observations, mineralogical, XRF and ICP-MS analyses reveal that some of the carbonate rocks are derived from sedimentary protoliths, whereas others are magmatic calcio- and magnesio-carbonatites some of which are mineralized with barite-monazite. The interbanded occurrence and apparent contemporary emplacement of these different rock types within individual dykes, backed by Sr-Nd isotope evidence, are interpreted to show that intrusion of mantle-derived carbonatite magma was accompanied by mobilization of crustal marbles. That took place some 840Ma ago but the REE-mineralization is dated at ca. 400Ma. [PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1007/s00710-004-0056-2 |
| format | Article |
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J. ; Ba-bttat, M. A. O. ; Taylor, R. N. ; Milton, J. A. ; Windley, B. F. ; Evins, P. M.</creator><creatorcontrib>Le Bas, M. J. ; Ba-bttat, M. A. O. ; Taylor, R. N. ; Milton, J. A. ; Windley, B. F. ; Evins, P. M.</creatorcontrib><description>Dykes of carbonate rocks, that cut gneisses in the Lowder-Mudiah area of southern Yemen, consist of dolomite and/or calcite with or without apatite, barite and monazite. Petrographic observations, mineralogical, XRF and ICP-MS analyses reveal that some of the carbonate rocks are derived from sedimentary protoliths, whereas others are magmatic calcio- and magnesio-carbonatites some of which are mineralized with barite-monazite. The interbanded occurrence and apparent contemporary emplacement of these different rock types within individual dykes, backed by Sr-Nd isotope evidence, are interpreted to show that intrusion of mantle-derived carbonatite magma was accompanied by mobilization of crustal marbles. That took place some 840Ma ago but the REE-mineralization is dated at ca. 400Ma. 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| subjects | Calcite Carbonate rocks Dolomite Isotopes Mineralization Mineralogy Minerals Radiometry Rocks Trace elements |
| title | The carbonatite-marble dykes of Abyan Province, Yemen Republic: the mixing of mantle and crustal carbonate materials revealed by isotope and trace element analysis |
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