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Thickness change involved in the peat-to- coal transformation for a bituminous coal of Cretaceous age in central Utah

Thomas A. Ryer·A.W. Langer
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Abstract

The ratio of the thicknesses of a layer of peat and the coal bed formed from that peat has been calculated for a bituminous coal bed in central Utah. The method used involves comparison of the thickness of peat eroded by a laterally migrating channel system with the thickness of coal now absent from the outcrop. The peat:coal thickness ratio calculated by this method is approximately 11:1.

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Thomas A. Ryer, A.W. Langer. 1980. Thickness change involved in the peat-to- coal transformation for a bituminous coal of Cretaceous age in central Utah. https://doi.org/10.1306/212f7b44-2b24-11d7-8648000102c1865d

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