The early part of the Cenozoic succession of Kutch is still debated for the age of the formations overlying the Deccan basalt. Authors have differed on the question of the presence of marine Palaeocene, Lutetian and Priabonian sediments in Kutch. This paper integrates the larger foraminifer based shallow benthic zones (Serra Kiel et al., 1998) and the planktic foraminiferal zones (Berggren and Pearson, 2005) of the Eocene succession to present a revised chronostratigraphy. It is concluded that there is no evidence of Palaeocene marine sediments in on-land Kutch. The Eocene successions are referred to Ypressian and Bartonian stages. A small thickness of sediments below the Bartonian lacks age-diagnostic taxa and could questionably be of late Lutetian age. There is no evidence of Priabonian sediments in the area. Based on the present biostratigraphic study and the latest Geologic Time Scale (Gradestein et al., 2012), hiatuses of ~7 Myr between the Deccan Trap and Naredi Formation, ~7 Myr between Naredi Formation and Harudi Formation and ~4 Myr between Fulra Limestone and Maniyara Fort Formation are estimated.
An Updated Eocene Stratigraphy of Kutch
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The early part of the Cenozoic succession of Kutch is still debated for the age of the formations overlying the Deccan basalt. Authors have differed on the question of the presence of marine Palaeocene, Lutetian and Priabonian sediments in Kutch. This paper integrates the larger foraminifer based shallow benthic zones (Serra Kiel et al., 1998) and the planktic foraminiferal zones (Berggren and Pearson, 2005) of the Eocene succession to present a revised chronostratigraphy. It is concluded that there is no evidence of Palaeocene marine sediments in on-land Kutch. The Eocene successions are referred to Ypressian and Bartonian stages. A small thickness of sediments below the Bartonian lacks age-diagnostic taxa and could questionably be of late Lutetian age. There is no evidence of Priabonian sediments in the area. Based on the present biostratigraphic study and the latest Geologic Time Scale (Gradestein et al., 2012), hiatuses of ~7 Myr between the Deccan Trap and Naredi Formation, ~7 Myr between Naredi Formation and Harudi Formation and ~4 Myr between Fulra Limestone and Maniyara Fort Formation are estimated.
Publication Mode |
Online |
---|---|
Publication Author |
Pratul Kumar Saraswati, Sonal Khanolkar, D. S. N. Raju, Santanu Banerjee |
Publication Language |
English |
Publication Type |
Conference Paper |
Publication Year |
2016 |
DOI |
10.17491/cgsi/2016/105406 |
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