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Syn-rift lacustrine carbonates; cycles, microbial mounds, and brackish to hypersaline facies models; Purbeck Group, Wessex Basin, UK. Analogues for south Atlantic pre-salt carbonates?

September 2 — September 4


 

The lacustrine limestones of the Purbeck Group were deposited in a shallow lake on the western margin of the Wessex Basin during its late syn-rift phase of basin evolution. The field trip will demonstrate the palaeoenvironmental setting of these limestones in the latest Jurassic and show how this lake was firstly brackish water and later hypersaline. The lower, brackish phase, of the Purbeck limestones are characterised by in-situ, highly porous, thrombolitic microbial mounds that reveal complex and irregular shapes. These microbial mounds are surrounded by, and interdigitate with, an inter-mound packstone-grainstone facies and together are arranged in high-frequency lacustrine cycles capped by paleosols. This fieldtrip will demonstrate these complex and highly variable carbonate facies and compare them with the pre-salt carbonates of the South Atlantic. This new work on the Dorset Purbecks represents the results of a 4-year industry funded research project at Royal Holloway University of London.

 

Read the reveiw of the 2016 trip here


"On a personal note, as a sedimentologist and geomodeller by background, one thing that always resonates with me after a field trip is the immeasurable value of seeing rocks in the field; being able to visualise the scale and variability of geology in three dimensions. In my opinion, for this reason alone (in addition to fantastic learning, networking and socialising opportunities), it is well worth making the effort to leave the computer screen behind and get out into the field from time to time." Dean Baker, RISC Advisory


 

Registration open now! 

Members: £600 

Registration includes travel to Purbeck from London, travel between locations, 2 nights’ accommodation with breakfast, packed lunches, two full days in the field and a detailed field guide!


By booking a place on these events you agreeing to the event terms and conditions which can be found here. For more information please email bethany@pesgb.org.uk 


The lacustrine limkestones of the Purbeck Group were deposited in a shallow lake on the western margin of the Wessex Basin during its late syn-rift phase of basin evolution. The field trip will demonstrate the palaeoenvironmental setting of these limestones in the latest Jurassic and show how this lake was firstly brackish water and later hypersaline. The lower, brackish phase, of the Purbeck limestones are characterised by in-situ, highly porous, thrombolitic microbial mounds that reveal complex and irregular shapes. These microbial mounds are surrounded by, and interdigitate with, an inter-mound packstone-grainstone facies and together are arranged in high-frequency lacustrine cycles capped by paleosols. This fieldtrip will demonstrate these complex and highly variable carbonate facies and compare them with the pre-salt carbonates of the South Atlantic. This new work on the Dorset Purbecks represents the results of a 4-year industry funded research project at Royal Holloway University of London.

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