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Chapter 10 Palaeo-Mesoproterozoic sedimentation and tectonics of the Singhbhum Craton, eastern India, and implications for global and craton-specific geological events

Rajat Mazumder, Shuvabrata De, Tohru Ohta, David Flannery, Leena Mallik, Trisrota Chaudhury, Priyanka Chatterjee, Marinah A. Ranaivoson and Makoto Arima
Geological Society, London, Memoirs, 43, 139-149, 2015, https://doi.org/10.1144/M43.10
Rajat Mazumder
School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Sydney, NSW 2052, Australia
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Shuvabrata De
Department of Geology, University of Calcutta, Kolkata, 700035, India
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Tohru Ohta
Faculty of Education and Integrated Arts and Sciences, Waseda University, 1-6-1, Nishiwaseda, Shinjuku-ku, Tokyo, 169-8050, Japan
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David Flannery
Australian Centre for Astrobiology, School of Biotechnology and Biomolecular Sciences, University of New South Wales, Sydney, NSW 2052, Australia
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Leena Mallik
Department of Geological Sciences, Jadavpur University, Kolkata, 700032, India
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Trisrota Chaudhury
Department of Geological Sciences, Jadavpur University, Kolkata, 700032, India
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Priyanka Chatterjee
Department of Geology, University of Calcutta, Kolkata, 700035, India
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Marinah A. Ranaivoson
Graduate School of Environment and Information Sciences, Yokohama National University, 79-7 Tokiwadai Hodogaya, Yokohama, 240-8501, Japan
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Makoto Arima
Graduate School of Environment and Information Sciences, Yokohama National University, 79-7 Tokiwadai Hodogaya, Yokohama, 240-8501, Japan
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Abstract

The Singhbhum Craton in eastern India preserves a depositional record from the Palaeo-Mesoarchaean to the Mesoproterozoic. Herein, we have summarized the Palaeo-Mesoproterozoic supracrustal record of the Singhbhum Craton, discussed tectonosedimentary processes and discriminated Palaeo-Mesoproterozoic global and craton-specific events. The late Palaeo-Mesoproterozoic supracrustal record of the Singhbhum Craton is limited. It includes evidence for high continental freeboard conditions during 2.6–2.1 Ga in the form of terrestrial deposits (alluvial fan–fluvial) of the Dhanjori Formation. This was followed by a major transgression and a transition to the relatively deeper-water shelf to shallow intertidal environments recorded by the Chaibasa Formation. A long hiatus ensued before deposition of the Dhalbhum Formation and conformably overlying Dalma and Chandil formations, suggesting continued high continental freeboard during 2.2–1.6 Ga. In significant contrast to the craton-specific Dhanjori Formation volcanism, the 1.7–1.6 Ga plume-related Dalma volcanism was probably part of a global tectonothermal event.

  • © 2015 The Geological Society of London

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Geological Society, London, Memoirs: 43 (1)
Geological Society, London, Memoirs
Volume 43
2015
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Chapter 10 Palaeo-Mesoproterozoic sedimentation and tectonics of the Singhbhum Craton, eastern India, and implications for global and craton-specific geological events

Rajat Mazumder, Shuvabrata De, Tohru Ohta, David Flannery, Leena Mallik, Trisrota Chaudhury, Priyanka Chatterjee, Marinah A. Ranaivoson and Makoto Arima
Geological Society, London, Memoirs, 43, 139-149, 2015, https://doi.org/10.1144/M43.10
Rajat Mazumder
School of Biological, Earth and Environmental Sciences, and Australian Centre for Astrobiology, University of New South Wales, Sydney, NSW 2052, Australia
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • For correspondence: rajatunsw@gmail.com
Shuvabrata De
Department of Geology, University of Calcutta, Kolkata, 700035, India
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
Tohru Ohta
Faculty of Education and Integrated Arts and Sciences, Waseda University, 1-6-1, Nishiwaseda, Shinjuku-ku, Tokyo, 169-8050, Japan
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
David Flannery
Australian Centre for Astrobiology, School of Biotechnology and Biomolecular Sciences, University of New South Wales, Sydney, NSW 2052, Australia
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Leena Mallik
Department of Geological Sciences, Jadavpur University, Kolkata, 700032, India
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Trisrota Chaudhury
Department of Geological Sciences, Jadavpur University, Kolkata, 700032, India
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Priyanka Chatterjee
Department of Geology, University of Calcutta, Kolkata, 700035, India
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Marinah A. Ranaivoson
Graduate School of Environment and Information Sciences, Yokohama National University, 79-7 Tokiwadai Hodogaya, Yokohama, 240-8501, Japan
  • Find this author on Google Scholar
  • Find this author on PubMed
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Makoto Arima
Graduate School of Environment and Information Sciences, Yokohama National University, 79-7 Tokiwadai Hodogaya, Yokohama, 240-8501, Japan
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Chapter 10 Palaeo-Mesoproterozoic sedimentation and tectonics of the Singhbhum Craton, eastern India, and implications for global and craton-specific geological events

Rajat Mazumder, Shuvabrata De, Tohru Ohta, David Flannery, Leena Mallik, Trisrota Chaudhury, Priyanka Chatterjee, Marinah A. Ranaivoson and Makoto Arima
Geological Society, London, Memoirs, 43, 139-149, 3 March 2015, https://doi.org/10.1144/M43.10
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    • Abstract
    • Palaeo-Mesoproterozoic Singhbhum supracrustals
    • Tectonosedimentary processes
    • Global and craton-specific Palaeo-Mesoproterozoic events
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