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Etude structurale du flanc ouest de l anticlinorium de Dalhousie, OEL 20-21. (Structural study of western flank of the anticlinorium of Dalhousie, OEL 20-21).
Initial study of the regional geology concluded that the structural deformation (large anticlinal synclinal) observed at the surface could be associated with the deformation of the Palaeozoic underneath the Mesozoic cover. 1:250000 structure contour...-
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