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Zinc isotopes reveal disparate enriched sources of contemporary lamprophyres in Eastern Dharwar Craton

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Abstract

Lamprophyres are mantle-derived rocks characterized by enrichment of incompatible elements and volatiles; however, the origin of their enriched sources remains enigmatic. Here we present zinc isotopic data for contemporary Mesoproterozoic (~ 1.1 Ga) lamprophyres from three localities of the Eastern Dharwar Craton. The Mudigubba and Kadiri lamprophyres with island-arc basalt (IAB)-like trace element features, such as positive Pb and negative Nb–Ta, Zr–Hf and Ti anomalies, have mid-ocean ridge basalt (MORB)-like δ66Zn values ranging from + 0.22‰ to + 0.29‰. In contrast, the Udiripikonda lamprophyre shows higher-than-MORB δ66Zn values of + 0.39‰ to + 0.48‰ and elemental features of intra-plate magmas with a lack of pronounced Nb–Ta-negative anomalies. Based on the covariations between Zn isotopes and trace element ratios, we infer that the Mudigubba and Kadiri lamprophyres with MORB-like Zn isotopes and high Ba/La, K/Nb and low Nb/La, Ce/Pb ratios are inherited from sub-continental lithospheric mantle metasomatized by fluids derived from a subducted slab. On the contrary, the higher-than-MORB Zn isotopic compositions, with low Ba/La, K/Nb and high Nb/La, Ce/Pb, K/U and Ba/Th ratios for the Udiripikonda lamprophyre are inferred to derive from lithospheric mantle enriched by carbonatitic melts or subducted carbonate-bearing sediments within the mantle transition zone. Hence, our study suggests that contemporary lamprophyres can be derived from disparate enriched mantle sources.

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Acknowledgements

We are grateful to Dan-Dan Li for assistance with the Zn isotopic analyses. Rong Xu and an anonymous reviewer are warmly thanked for their detailed and instructive reviews, and the editorial support of Hans Keppler is also greatly appreciated. This work was supported by the National Natural Science Foundation of China (42130310 and 41802045). LK was supported by the EXPRO 2019 project (No. 19-29124X) of the Czech Science Foundation and the RVO 67985831 project of the Institute of Geology of the Czech Academy of Sciences. NVCR thanks BHU for awarding him a faculty incentive grant (IOE). We are indebted to Daniel Müller for his comments on an earlier draft of this manuscript.

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Authors and Affiliations

  1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an, 710069, China

    Jian-Qiang Liu, Li-Hui Chen & Xiao-Jun Wang

  2. Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, 165 02, Prague 6, Czech Republic

    Lukáš Krmíček

  3. Faculty of Civil Engineering, Institute of Geotechnics, Brno University of Technology, Veveří 95, 602 00, Brno, Czech Republic

    Lukáš Krmíček

  4. BIC Brno, Technology Innovation Transfer Chamber, Purkyňova 648/125, 612 00, Brno, Czech Republic

    Lukáš Krmíček

  5. State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing, 210023, China

    Gang Zeng & Xiao-Yu Zhang

  6. School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, QLD, 4000, Australia

    David T. Murphy

  7. School of Geography, Earth and Atmospheric Sciences, The University of Melbourne, Parkville, VIC, Australia

    Hayden Dalton

  8. Department of Earth Sciences, School of Physical, Chemical, and Applied Sciences, Pondicherry University, Puducherry, 605014, India

    Ashutosh Pandey

  9. Department of Geology, Institute of Science, Banaras Hindu University, Varanasi, 221005, India

    N. V. Chalapathi Rao

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  1. Jian-Qiang Liu
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Liu, JQ., Chen, LH., Wang, XJ. et al. Zinc isotopes reveal disparate enriched sources of contemporary lamprophyres in Eastern Dharwar Craton. Contrib Mineral Petrol 178, 89 (2023). https://doi.org/10.1007/s00410-023-02073-1

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