Lambert, J.L.M.  <br/><br/>
Cross - Folding in the Gramscatho beds at Helford river, Cornwall 

 - 489-496pp.  Illustration 
<br/><br/> Abstract<br/>Minor folds in the Gramscatho Beds at the mouth of the Helford River have two predominant trends: W.S.W.-E.N.E., and N.W.-S.E. Main folds on W.S.W.-E.N.E. axes and cross folds on N.W.-S.E. axes have sub-parallel apical planes and occur in alternate zones which trend N.E.-S.W., parallel to the strike of the cleavage. The relations between the two systems of folding suggest that they are virtually synchronous.<br/><br/>It is concluded that the style of folding can be explained by a unidirectional regional stress acting normal to the apical planes of the folds. 
<br/><br/><label>Subjects--Topical Terms: </label><br/>Folds - Gramscatho beds - Helford river - Cornwall - England<br/>Folds - Cornwall - England<br/>Tectonics - Cornwall - England