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The Stretton Series is a division of Late Precambrian rocks found in Shropshire, England, dating back to a period between 4.6 billion and 542 million years ago. These rocks are primarily composed of grayish and greenish siltstones, sandstones, shales, and volcanic rocks, with thicknesses reaching up to 3,500 meters. The Stretton Series is part of the Eastern Longmyndian subdivision and is separated from the overlying Minton Series by an unconformity, indicating a period of erosion. While unfossiliferous, similar rock sequences in other regions, like the Charnian rocks, contain impressions of Precambrian organisms such as Charnia.1

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2 Britannica Sources
  1. Wenlock Series
  2. Longmyndian

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