5 



I" 



"O o 



-* LU 



O 



o 

 a. 



Correlation between Eames, Bayliss and Latif along the Rakhi Nala 



Eames ( 1952, p.162-163 ) 



& 



Succession 



Pellatispira Beds 



Upper Chocolate Clays (Upper part) 



c 



._ 



w 





u 



o 



a 





n 





CI 







w 





S 



" 



o 



J£ 



CARDIU 



beaumomi 



BEDSt 



Upper Chocolate Clays ( Lower part) 



White Marl Band 



Lower Chocolate Clays 



Platy Limestone 



Shales with Alabaster 



Rubbly Limestones 



Green and Nodular Shales 



Upper Rakhi Gaj Shales 



Lower Rakhi Gaj Shales. (Topmost 



portion onlyS Irregularis Limestone, 



Lower Rakhi Gaj Shales (Max pars) 



Gorge Beds 



Venericardia Shales 



Thickness 

 in feet 



Sample no. 



as used in 



present 



paper 



60 



425-495 



420-490 



40 



930 



70 



750 



410 



850 



1620 



60 



775 



470 



95 



3666 

 3657 



K38 

 3413 



36.67 

 3668 



3667.367! 

 3139 



3,t 



3115 

 3110 



Bayliss & SamantaOn press) 



Succession 



Kirthar 



Ghazij 



Dunghan 



Ranikot 



6> 



D.C 

 i <■> 



slS 



o 



LU 



O 



a. 



Thickness 



in feet & 



sample nos. 



2212 



3607 



759 



3,15 



553 3no 



Latif (1961, p. 33-36,1964, p. 31) 



Thickness 



in feet & 



sample nos 



110 



2m 



3664 

 3651 



A25 



K0 

 170 



160 



360G 

 3498 



900 



100 



1160 



670 



30 



100 



ur 



240 



850 



1840 



Zones 



Globigerina cf. trilocula 



Chiloouembelina victoriana 



Hastiqerina micro 



Chiloquembelina att martini 



Catapsvdrax unicavus 



Globigerina yequaensis 



No Pelagic foraminifera 



Globorotalia sp. 3 



Globorotalia sp. 4 



Globigerina esnaensis 



Hastigerina pseudoiota 



Globigerina sp. 5 



Globorotalia rex 



Globorotalia (T ) crater 



Globorotalia angulata 



No Pelagic foraminifera 



Succession 



Tapti 



Kirthar 



Ghazij 



Ranikot 



Pab Sandstones 



Pab 



Pab 



* Probable equivalents of Eames, 1952. 



**Eames, personal communication. 



+ Danian according to Nagappa, 1959, which he regards as basal Paleocene. 

 *■ ? Paleocene. 



FIG. 2 



