Ghosh, S.; Fallick, A. E.; Paul, D. K. and Potts, P.
|DOI (Digital Object Identifier) Link:||http://dx.doi.org/10.1016/S1342-937X(05)71144-8|
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Many granitic bodies intrude the basement gneisses in Meghalaya Plateau, Northeast India. Rb-Sr whole-rock isotopic ages of the granitoids range from 881 to 479 Ma while the ages of the basement orthogneisses vary from 1714 to 1150 Ma. All the plutons are dominantly metaluminous and show geochemical variation. Oxygen isotopic compositions in the granitoids and gneisses are concordant (delta(18)O: + 5.78% to + 8.70%). However, the gneisses from high-grade terrain have low delta(18)O value of +2.52%o to +5.31%o. Initial Sr-87/Sr-86 (I-Sr) ratios of the plutons vary from 0.70459 to 0.71487 and tend to increase with progressive younging in age. The geochemical characters suggest derivation of the granites from lower crustal source. The fractionated rare earth patterns observed in the granitoids can be obtained by partial melting of gneisses or diorites. Some gneiss samples have experienced interaction with hydrothermal fluids resulting in lowering delta(18)O. The isotopic ages of granite plutonism in Meghalaya are similar to the plutonic and tectonothermal events in other parts of India, southwestern Australia and document final amalgamation events of the Gondwana Supercontinent.
|Item Type:||Journal Article|
|Keywords:||Neoproterozoic granite; oxygen isotope; petrogenesis; Meghalaya; Northeast India|
|Academic Unit/Department:||Science > Environment, Earth and Ecosystems
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Astrid Peterkin|
|Date Deposited:||09 Aug 2007|
|Last Modified:||14 Jan 2016 16:41|
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