Abstract
Most of the GCR sites documented and discussed in this chapter lie within perhaps 30 km of the original western shoreline of the late Permian Zechstein Sea and north of the Cleveland High (Figure 1.2). There is no evidence of a connection with the Bakevellia Sea at any time during the first two main sedimentary cycles (EZ1 and EZ2) and only limited evidence of a brief connection with the Vale of Eden inland sedimentary basin during Cycle EZ3 (but see Holliday, 1993 and Smith, in press).
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© 1995 Springer Science+Business Media Dordrecht
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Smith, D.B. (1995). North-east England (Durham Province). In: Marine Permian of England. Emotions, Personality, and Psychotherapy. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-1204-8_3
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DOI: https://doi.org/10.1007/978-94-011-1204-8_3
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