Page 3 - An Atlas of Carboniferous Basin Evolution in Northern England
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Geological  Society  Special Publications
                                Society  Book  Editors
                             A.  J.  FLEET (CHIEF  EDITOR)
                                     P.  DOYLE
                                   F.  J.  GREGORY
                                   J.  S.  GRIFFITHS
                                   A.  J.  HARTLEY
                                 R.  E.  HOLDSWORTH
                                   A.  C.  MORTON
                                    N.  S.  ROBINS
                                   M.  S.  STOKER
                                   J.  P.  TURNER



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       It  is recommended  that  reference to  this book  should  be made  in the following
       way:

       FRASER,  A.  J.  &  GAWTHORPE,  R.  L.  2003.  An  Atlas  of  Carboniferous  Basin
       Evolution  in Northern  Englalnd.  Geological  Society,  London,  Memoir  28.
                                                                                                      View looking east along Hope Valley from  Mam  Tor, Derbyshire. Early Namurian  Edale shales (sequence LC la) in the valley onlap
                                                                                                      the now exhumed  late Dinantian carbonate platform  margin (sequence EC4) forming  the righthand  valley side. The  left-hand  valley
                                                                                                      side is composed of pro-delta Kinderscoutian turbidites and  the snow capped hills  in the distance late Namurian mouthbar and delta
                                                                                                      top  fluvial  sandstones.  Below  the  composite  seismic  line  from  the  Edale  Gulf  illustrates  the  subsurface  geology to  the  east of  the
                                                                                                      outcrop  location  and  highlights  the  half graben  and  fault-controlled  geometry  of  the  Dinantian  basins (also see Fig.  17, p. 21).
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