Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Stratigraphy of the Purana Supergroup Around Ramgundam, Andhra Pradesh


Affiliations
1 Geological Studies Unit, Indian Statistical Institute, 203, Barrackpore Trunk Road, Calcutta 700 035, India
     

   Subscribe/Renew Journal


Middle and Late Proterozoic Purana Supergroup at Ramgundam in the Pranhita Godavari valley is separated from the underlying granites and gneisses of the Basement Complex and the overlying Gondwana Supergroup by two major unconformities. Evidence is adduced to show that two other major unconformities divide the Purana sequence into three chronologically independent units correlatable with the Mallampalli Subgroup and the Mulug Subgroup, two major divisions of the Pakhal Group, and the Sullavai Group in adjacent areas, viz., Mancherial and Mulug.

Both the Subgroups of the Pakhal Group comprise of silici-clastics at the base and are followed by carbonates while the Sullavai Group is constituted entirely of siliciclastics. Detailed section measurements show rapid facies variation, both lateral and vertical, to be a characteristic feature of the Pakhal formations. Formations in the Sullavai Group are regionally more uniform in character.


Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 211

PDF Views: 4




  • Stratigraphy of the Purana Supergroup Around Ramgundam, Andhra Pradesh

Abstract Views: 211  |  PDF Views: 4

Authors

A. Chaudhuri
Geological Studies Unit, Indian Statistical Institute, 203, Barrackpore Trunk Road, Calcutta 700 035, India

Abstract


Middle and Late Proterozoic Purana Supergroup at Ramgundam in the Pranhita Godavari valley is separated from the underlying granites and gneisses of the Basement Complex and the overlying Gondwana Supergroup by two major unconformities. Evidence is adduced to show that two other major unconformities divide the Purana sequence into three chronologically independent units correlatable with the Mallampalli Subgroup and the Mulug Subgroup, two major divisions of the Pakhal Group, and the Sullavai Group in adjacent areas, viz., Mancherial and Mulug.

Both the Subgroups of the Pakhal Group comprise of silici-clastics at the base and are followed by carbonates while the Sullavai Group is constituted entirely of siliciclastics. Detailed section measurements show rapid facies variation, both lateral and vertical, to be a characteristic feature of the Pakhal formations. Formations in the Sullavai Group are regionally more uniform in character.