File:YGS CHR 04 DINA FIG 07.jpg

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Summary[edit]

description
English: Figure 7 An isochore map of the Scremerston Coal Group and its equivalents. Thicknesses are in metres. The increase in thickness to the south may relate to increasing differential subsidence between the Mid North Sea High and the Southern North Sea Basin. Note the continuing strong differential subsidence between the Alston Block and the Stainmore Trough. The contouring ignores the thick Scremerston facies at well 41/10-1, which is regarded as a facies equivalent of thick Fell Sandstone channel sands in other wells.
From: Carboniferous hydrocarbon resources: the southern North Sea and surrounding onshore areas, edited by J. D. Collinson, D. J. Evans, D. W. Holliday, N. S. Jones. Published as volume 7 in the Occasional Publications series of the Yorkshire Geological Society, © Yorkshire Geological Society 2005.
source Yorkshire Geological Society
author John D. Collinson

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Yorkshire rocks and landscape

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Northumbrian rocks and landscape

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Attribution statement: Image from 'Northumbrian rocks and landscape: a field guide.' Yorkshire Geological Society 2004. www.yorksgeolsoc.org.uk

Carboniferous hydrocarbon resources: the southern North Sea and surrounding onshore areas

Images are Copyright Yorkshire Geological Society.

Attribution statement: Image from 'Carboniferous hydrocarbon geology.' Yorkshire Geological Society 2005. www.yorksgeolsoc.org.uk

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