About This Item

Share This Item

The AAPG/Datapages Combined Publications Database

Journal of Sedimentary Research (SEPM)


Journal of Sedimentary Petrology
Vol. 34 (1964)No. 2. (June), Pages 254-269

Petrography and Origin of Some Upper Jurassic Beds from Dorset, England

Philip R. Brown


Petrographic examination of Lower Purbeck sediments indicates that most of them formed in an evaporitic environment. The dominant sediment was a carbonate-mud, now seen either in the form of pellets and lumps in a fine-coarse crystalline calcite cement, or as a homogeneous calcite-mudstone. Contribution by shells to rock formation is important only at certain horizons, but algae appear to have had considerable influence on sedimentation throughout the Lower Purbeck. Brackish or freshwater environments only attained major importance towards the end of Lower Purbeck time.

Pay-Per-View Purchase Options

The article is available through a document delivery service. Explain these Purchase Options.

Protected Document: $10
Internal PDF Document: $14
Open PDF Document: $24