Editing A sequence-stratigraphy scheme of the Late Carboniferous, southern North Sea, Anglo-Dutch sector

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Coarse-grained intervals typically are made up of multistorey fluviatile sandstone bodies. Comparison of closely spaced wells indicates that, although individual sandstone bodies are laterally impersistent, they are commonly laterally persistent and of a consistent overall regional thickness. The lower boundaries of some of these sandstones may be sequence boundaries, the onset of major sand deposition within the Coal Measures coastal plain being a response to sea-level fall.
 
Coarse-grained intervals typically are made up of multistorey fluviatile sandstone bodies. Comparison of closely spaced wells indicates that, although individual sandstone bodies are laterally impersistent, they are commonly laterally persistent and of a consistent overall regional thickness. The lower boundaries of some of these sandstones may be sequence boundaries, the onset of major sand deposition within the Coal Measures coastal plain being a response to sea-level fall.
  
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'''[[:File:YGS_CHR_06_ASEQ_TAB_03.jpg|Table 3]] Westphalian systems tracts.'''
  
'''[[:File:YGS_CHR_06_ASEQ_TAB_03.jpg|Table 3]] Westphalian systems tracts.'''
 
  
 
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