Polyphase development of slaty cleavage and the confrontation of facing directions in the Devonian rocks of north Cornwall
Polyphase development of slaty cleavage and the confrontation of facing directions in the Devonian rocks of north Cornwall
 
  UPPER Devonian rocks in north Cornwall are flanked to the north and south by Middle Devonian rocks1. For many kilometres to the south, recumbent folds with a well developed slaty cleavage parallel to their axial planes face northwards whereas, for many kilometres to the north, recumbent folds with an equally well developed axial planar slaty cleavage face southwards2. Structural and stratigraphie relationships on a regional scale preclude an interpretation of this change in facing direction in terms of orthodox refolding. There is, moreover, no local evidence to support such an interpretation. 
  
  
  87-89
  
    
      Roberts, John L.
      
        f1f9800c-50a1-4497-981d-1f5f5beb79ff
      
     
  
    
      Sanderson, David J.
      
        5653bc11-b905-4985-8c16-c655b2170ba9
      
     
  
  
   
  
  
    
      22 March 1971
    
    
  
  
    
      Roberts, John L.
      
        f1f9800c-50a1-4497-981d-1f5f5beb79ff
      
     
  
    
      Sanderson, David J.
      
        5653bc11-b905-4985-8c16-c655b2170ba9
      
     
  
       
    
 
  
    
      
  
  
  
  
  
  
    Roberts, John L. and Sanderson, David J.
  
  
  
  
   
    (1971)
  
  
    
    Polyphase development of slaty cleavage and the confrontation of facing directions in the Devonian rocks of north Cornwall.
  
  
  
  
    Nature, 230, .
  
   (doi:10.1038/physci230087a0). 
  
  
   
  
  
  
  
  
   
  
    
      
        
          Abstract
          UPPER Devonian rocks in north Cornwall are flanked to the north and south by Middle Devonian rocks1. For many kilometres to the south, recumbent folds with a well developed slaty cleavage parallel to their axial planes face northwards whereas, for many kilometres to the north, recumbent folds with an equally well developed axial planar slaty cleavage face southwards2. Structural and stratigraphie relationships on a regional scale preclude an interpretation of this change in facing direction in terms of orthodox refolding. There is, moreover, no local evidence to support such an interpretation. 
        
        This record has no associated files available for download.
       
    
    
   
  
  
  More information
  
    
      Published date: 22 March 1971
 
    
  
  
    
  
    
  
    
  
    
  
    
  
    
  
    
  
    
  
  
  
    
  
  
        Identifiers
        Local EPrints ID: 76168
        URI: http://eprints.soton.ac.uk/id/eprint/76168
        
          
        
        
        
          ISSN: 0028-0836
        
        
          PURE UUID: 788c8a84-19b0-471a-bbef-8c10c7fe2410
        
  
    
        
          
        
    
        
          
            
              
            
          
        
    
  
  Catalogue record
  Date deposited: 11 Mar 2010
  Last modified: 14 Mar 2024 02:53
  Export record
  
  
   Altmetrics
   
   
  
 
 
  
    
    
      Contributors
      
          
          Author:
          
            
            
              John L. Roberts
            
          
        
      
        
      
      
      
    
  
   
  
    Download statistics
    
      Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.
      
      View more statistics