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• W2016036327 abstract "Abstract Several small bodies of massive to banded amphibolite occur within plagioclase-quartz-biotite hornblende gneiss at or close to its boundary with a quartz diorite pluton in the Neoproterozoic terrain of southern Israel. Entrapped within the amphibolite are nodules consisting mainly of calcite+talc, and rare banded marble. Remnant laminae and certain geochemical features such as the negative Ce anomaly and depleted δ 13 C of the nodules sugggest that they initially formed as stromatolites. The local geological setting of the amphibolites together with the presence of the enclosed meta-carbonates favoured an origin as sediments, although some of the geochemical data point to a basaltic precursor and some of the carbonates have a puzzlingly high (>1000 ppm) Ni content. The origin of the amphibolites is thus enigmatic." @default.
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• W2016036327 date "2004-08-01" @default.
• W2016036327 modified "2023-10-18" @default.
• W2016036327 title "Carbonate nodules of probable stromatolitic origin in amphibolite from the Neoproterozoic terrain of southern Israel" @default.
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• W2016036327 doi "https://doi.org/10.1180/0026461046840213" @default.
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