Proterozoic intracontinental basin: The Vindhyan example |
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Authors: | Chandan Chakraborty |
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Institution: | (1) Geological Studies Unit, Indian Statistical Institute, 203 B.T. Road, 700 108 Kolkata, India |
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Abstract: | Summary The features of the Vindhyan succession clearly indicate a vast intracratonic basin that remained within tens of meters of
sea level throughout its lifetime. Apparently, shallow water condition was maintained over a large area for a long period
of time suggesting that the sub-Vindhyan lithosphere suffered subsidence over a larger area producing a wide shallow ramp
type basin. Hundreds of meters thick accumulation of peritidal strata in sequence 5 of the Vindhyan succession indicates that
the subsidence rate was in perfect concert with the rate of sediment supply for a considerably long period of time during
the end phase of Vindhyan basin evolution — the hallmark of cratonic basins Sloss (1988a, b). It is inferred that during the
terminal period of the Vindhyan sedimentation a self-regulating system of uplift, erosion, sedimentation and subsidence controlled
the accumulation of strata. |
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Keywords: | Intracratonic basin Proterozoic depositional environments sedimentation sequence stratigraphy |
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