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    U-Pb dating of metamorphic monazite establishes a Pan-African age for tectonism in the Nallamalai Fold Belt, India

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    Authors
    Sheppard, S.
    Rasmussen, B.
    Zi, J.
    Soma Sekhar, V.
    Srinivasa Sarma, D.
    Ram Mohan, M.
    Krapež, B.
    Wilde, S.
    McNaughton, Neal
    Date
    2017
    Type
    Journal Article
    
    Metadata
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    Citation
    Sheppard, S. and Rasmussen, B. and Zi, J. and Soma Sekhar, V. and Srinivasa Sarma, D. and Ram Mohan, M. and Krapež, B. et al. 2017. U-Pb dating of metamorphic monazite establishes a Pan-African age for tectonism in the Nallamalai Fold Belt, India. Journal of the Geological Society. 174 (6): pp. 1062-1069.
    Source Title
    Journal of the Geological Society
    DOI
    10.1144/jgs2017-051
    ISSN
    0016-7649
    School
    John de Laeter Centre
    URI
    http://hdl.handle.net/20.500.11937/58974
    Collection
    • Curtin Research Publications
    Abstract

    © 2017 The Author(s). The Nallamalai Fold Belt comprises late Palaeoproterozoic to Mesoproterozoic sedimentary rocks deformed into a fold-and-thrust belt along the eastern side of Peninsular India. The age of thin-skinned thrusting, folding and low- to mediumgrade metamorphism in the belt is unclear, with estimates ranging from Palaeoproterozoic to early Palaeozoic. A possible Pan- African age for thrusting has previously been inferred from Rb-Sr dating of muscovite in shear zones from the adjacent Krishna Province (501 - 474 Ma) but these structures are separated from the Nallamalai Fold Belt by a major thrust. Here, we present in situ U-Pb dating of metamorphic monazite within a low-grade metasedimentary rock in the Nallamalai Fold Belt at the Mangampeta barite mine. Our date of 531 ± 7 Ma for the monazite is the first direct evidence that west- to NW-directed nappe stacking, folding and low-grade metamorphism in the fold belt are related to Pan-African incorporation of India into the Gondwana supercontinent.

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