Memoirs of the Geological Survey of Pakistan, Volume 12The Survey, 1977 |
From inside the book
Results 1-3 of 49
Page 39
... stone is accepted here to represent similar thick bedded limestone referred to by Vredenburg ( 1909 ) as " massive limestone " , by Williams ( 1959 ) and Woodward ( 1959 ) as " Takatu lime- stone " and upper part of " Sulaiman limestone ...
... stone is accepted here to represent similar thick bedded limestone referred to by Vredenburg ( 1909 ) as " massive limestone " , by Williams ( 1959 ) and Woodward ( 1959 ) as " Takatu lime- stone " and upper part of " Sulaiman limestone ...
Page 68
... stone " , " Wakabi limestone " , Wakai lime- stone " , " Khude limestone " , " Kasria group ' and upper parts of the " Jakker " and " Jam- buro groups " of Hunting Survey Corporation ( 1961 ) of similar lithology . Parts of the strata ...
... stone " , " Wakabi limestone " , Wakai lime- stone " , " Khude limestone " , " Kasria group ' and upper parts of the " Jakker " and " Jam- buro groups " of Hunting Survey Corporation ( 1961 ) of similar lithology . Parts of the strata ...
Page 79
... stone . The limestone interbeds become dominant in other parts of the Kohat area , where they are characterized by an abundance of Nummulites . The formation is confined to the Kohat , northern Potwar , and Kala Chitta areas . It is 130 ...
... stone . The limestone interbeds become dominant in other parts of the Kohat area , where they are characterized by an abundance of Nummulites . The formation is confined to the Kohat , northern Potwar , and Kala Chitta areas . It is 130 ...
Contents
FOREWORD | 1 |
Tanawal formation | 8 |
Khyber undifferentiated carbonate complex | 15 |
2 other sections not shown
Other editions - View all
Common terms and phrases
Ahmad ammonoids arenaceous argillaceous Axial Belt Baluchistan Baluchistan Basin basal brachiopods brown calcareous Cambrian Chagai Chichali clay colour conformably conglomerate Cretaceous dark grey deposits disconformable dolomite Early eastern Salt Range Eocene Eruptive Zone exposed fauna foraminifers formation consists Fort Munro fossiliferous fossils Geological Ghazij greenish grey gypsum Hinglaj Hunting Survey Corporation Jurassic Kala Chitta Kala Chitta Range Khan Khisor Range Khyber Kirthar Province Kohat Kohat area Kohat-Potwar Province Late light grey limestone lithology Lower Indus Basin marl mation metres thick million tonnes mineral Nala Northern Montane Area overlain overlies Paleocene Permian Potwar quartzite Quetta Quetta region Ranikot reported Saindak Salt Range Samana Samana Range sandstone sediments sequence Shah shale Shirinab formation Siwalik slate Stauffer Sulaiman Province Surghar Range Surv Survey Corporation 1961 Teichert thick bedded thin tion Trans-Indus ranges Triassic type locality type section unconformably upper contact Upper Indus Basin volcanic Vredenburg West Pakistan western