Publication Name: PESA (QLD) Petroleum Symposium 1997
Authors: P.V. Grech
Date Published: December 1997
Number of Pages: 14
Reference Type: Magazine Article
Abstract:The Rewan Group consists of two depositional sequences. The first depositional sequence is composed of the Sagittarius Sandstone which is marked at its base by a third-order sequence boundary. The Brumby Sandstone Member (Arcadia Formation) lies at the base of the second depositional sequence and was also deposited over a third-order sequence boundary. The Arcadia Formation is in turn erosively overlain by the pebbly sandstone Clematis Group. Each sequence boundary represents regional tectonic and climatic changes that affected subsequent depositional systems.