P. K. Bose and P. P. Chakraborty, “Marine to Fluvial Transition: Proterozoic Upper Rewa Sandstone, Maihar, India,” Sedimentary Geology, Vol. 89, No. 3-4, 1994, pp. 285-302. doi:10.1016/0037-0738(94)90098-1

has been cited by the following article:

• TITLE: Facies Development and Depositional Environment of the Patherwa Formation (Semri Group), Son Valley, India

  AUTHORS: Abul Hasnat Masood Ahmad, Ghulam Mohammad Bhat, Ruchi Agarwal

  KEYWORDS: Vindhyan Basin; Sedimentary Facies; Palaeocurrents; Estuary; Tidal Flats; Upper Flow Regime

  JOURNAL NAME: Open Journal of Geology, Vol.2 No.2, April 25, 2012

  ABSTRACT: The present study documents three facies associations recorded from the Patherwa Formation. These facies are related to tidally influenced fluvial channel (Facies association A), tidal channel (Facies association B) and tidal sand bar/tidal flat sandy facies (Facies association C). The spatio-temporal variation of these facies associations and palaeocurrent trends suggest tide dominated estuarine system. The estuaries were operational along a 60 km long NW-SE trending palaeo-shoreline. The Patherwa Formation grades up-section into facies packages of increasing tidal energy and terminate with the deposition within the upper flow regime estuarine settings.