Upper Cretaceous to Lower Tertiary sedimentary environments and clay mineral associations in the Kharga Oasis area (Egypt)

1985 ◽  
Vol 1985 (10) ◽  
pp. 579-591
Author(s):  
Frits Hendriks
1986 ◽  
Vol 46 (1-2) ◽  
pp. 111-133 ◽  
Author(s):  
Mohamed A. Soliman ◽  
Mohamed E. Habib ◽  
Ezzat A. Ahmed

1911 ◽  
Vol 8 (12) ◽  
pp. 539-549 ◽  
Author(s):  
James Park

With the question of conformity or unconformity between the Lower Tertiary and Upper Cretaceous, there is associated a problem of great economic importance to New Zealand. The subject involves something more than a mere academic discussion. If conformity exists, then we have only one coal-bearing formation; but if unconformity, then we have two. I believe that both the stratigraphical and palæontological evidence is overwhelmingly in favour of the latter.


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