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bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall

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Page 1: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 2: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 3: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 4: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 5: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 6: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 7: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 8: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 9: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 10: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 11: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 12: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 13: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 14: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall
Page 15: bdigital.ufp.pt · The Cenozoic sediments are almost entirely terrigenous clastics, which prograded beyond the Early Cretaceous shelf margin to the present continental slope. Overall

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