. Bulletin of the British Museum (Natural History), Geology. AND JURASSIC AMMONITES FROM WEST PAKISTAN 327 5- Trans Indus Ranges The bulk of the ammonites described in the paper comes from the Surghar and Maidan Ranges located between Kalabagh (lat. 32°5g '; long. 71 ° 32' 30 ") and Makerwal ('at. 32° 56'30"; long. 7i°9') in Mianwali district (fig. 2; 21-27). The Middle Callovian ammonites occur in the outcrops of Samana Suk Limestone (upper bed) between west of Chichali Pass and Makerwal (Datta, Lunda and Punnu mines sections; Baroch nala section). The Upper Jurassic and Neocomian a
. Bulletin of the British Museum (Natural History), Geology. AND JURASSIC AMMONITES FROM WEST PAKISTAN 327 5- Trans Indus Ranges The bulk of the ammonites described in the paper comes from the Surghar and Maidan Ranges located between Kalabagh (lat. 32°5g '; long. 71 ° 32' 30 ") and Makerwal ('at. 32° 56'30"; long. 7i°9') in Mianwali district (fig. 2; 21-27). The Middle Callovian ammonites occur in the outcrops of Samana Suk Limestone (upper bed) between west of Chichali Pass and Makerwal (Datta, Lunda and Punnu mines sections; Baroch nala section). The Upper Jurassic and Neocomian ammon- ites are distributed in the lower and middle members of Chichali Formation exposed in Maidan and Surghar Ranges and extend eastward in western Salt Range and southward in Shaikh-Budin Hills. 6. Shaikh Bndin Hills The Tithonian ammonites were collected from the lower member of Chichali Formation, 2 miles east and west of Shaikh Budin Village (lat. 32° 18'; long. 70° 49' 45") in Dera Ismail Khan district (fig. 2; 28-30).. 34° Peiuli 2g-A Sh Budin Hills 4516 Fig. 5. Fossil locality map of Hazara, Kala Chitta, Kohat, Trans Indus Ranges including Shaikh Budin Hills, West Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original British Museum (Natural History). London : BM(NH)
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