The Pleistocene Knocknasilloge Member, an upward coarsening sequence of massive and laminated muds to cross-laminated fine sands and silts, was deposited in a series of shallow lacustrine basins formed at the retreating margin of the Late Devensian Irish Sea ice-sheet. Sedimentary successions mark i
β¦ LIBER β¦
The Palaeontology and Stratigraphy of the Marine Pliocene and Pleistocene of San Pedro, California
β Scribed by W., B. B.
- Book ID
- 109440402
- Publisher
- Nature Publishing Group
- Year
- 1904
- Tongue
- English
- Weight
- 102 KB
- Volume
- 69
- Category
- Article
- ISSN
- 0028-0836
- DOI
- 10.1038/069266a0
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