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Zircons from the Granitic Rocks of the Malani Igneous Suite : Morphological and Chemical Studies
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Zircons are hydrothennal or late-magmatic. The high UO2 contents of the Tosham zircons reflect the high UO2 of the host rocks. The Siwana granites, though high in Zr values, have very poor zircon yield. This is probably due to the pcralkalinity of the Si wana magma.
Keywords
Malani Igneous Suite, Zircon, Siwana Granite, Geochemistry, Rajasthan.
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