91 



iph. This is the 

 iver with parallel 



divided into five 

 these Units, I and 

 Dcene. Biostrati- 

 Zao River section 

 :tions have almost 

 ikhi Nala is also 



n the Rakhi Nala 

 pecies common to 

 tion can easily be 

 vice versa, (see 

 s also been calcu- 

 in the Zao River 

 rrelated with any 



hi Nala and Zinda 

 Hiver and Shpalai 

 es with Alabaster 

 /s (upper Eocene), 

 e Shpalai Khwara 



poorly preserved 

 bly equivalent to 

 ly Limestones and 

 i sediments below 

 and are probably 



in the northern 

 ible for abundant 



tide with Eames' 

 shales, Green and 

 )d fauna and are 

 i is in the Kirthar 

 y. This occurs in 

 n the White Marl 

 i Lower Chocolate 

 White Marl Band 



section has been 

 nes and Nagappa. 



