Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

K. K. Sinha ¹, Pradeep Pandey ¹, C. L. Bhairam ¹, P. S. Parihar ²

Affiliations
1 Atomic Minerals Directorate for Exploration and Research, West Block VII, R.K. Puram, New Delhi - 110 067, IN
2 Atomic Minerals Directorate for Exploration and Research, AMD Complex, 1-10-153/156, Begumpet, Hyderabad - 500 016, IN

Abstract

In the western part of Bundelkhand massif, a caldera with intra-caldera sediments, known as Dhala Formation, occurs as an outlier in and around Mohar village of Shivpuri district, Madhya Pradesh. For the first time, occurrence of peperite is being reported from the basal part of the Dhala sediment. Two types of peperites have been recognized: blocky and fluidal or globular with variable morphology. In peperitic zones, features like soft sediment deformations, presence of sediment into the rhyolite along cracks, vesiculation of the sediments and other evidences suggestive of sediment fluidization are some definite characteristics of interaction of hot magma with wet sediments forming peperite. The occurrence of peperites reflects the contemporaniety of deposition of the Dhala sediments and volcanism, which is well in accordance to the volcanic origin of Dhala structure. Further, the nature of unconformity between the Dhala and overlying Kaimur which is characterized by merely a few centimeter thick pebbly/conglomeratic bed does not appear to represent a large hiatus as expected between the Semri and Kaimur of Vindhyan Supergroup. So, the contemporaniety of the Dhala Formation (at least the lower part) as reflected by occurrence of peperites, coupled with the available age of the rhyolite and the nature of the unconformity between the Dhala and overlying Kaimur provide convincing evidence to correlate the Dhala Formation with the Lower part of the Kaimur and unlikely with the Semri Group or Bijawar as proposed earlier.

Keywords

Caldera, Peperites, Dhala Sediment, Bundelkhand, Vindhyans, Madhya Pradesh.

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