Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
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Page 1
... extending in the sub - latitudinal direction from the Straits of Gibralter in the West to Malacca Peninsula in the East . Young , folded structures of the Tethys usually form distinctly lineated folded belts clearly outlining numerous ...
... extending in the sub - latitudinal direction from the Straits of Gibralter in the West to Malacca Peninsula in the East . Young , folded structures of the Tethys usually form distinctly lineated folded belts clearly outlining numerous ...
Page 8
... extends from Karachi in the South to the north Waziristan regions in the North and within its borders coincides with the Central geosynclinal trough , The total extent of the belt is more than 1000 km , the width being 60-80 km ...
... extends from Karachi in the South to the north Waziristan regions in the North and within its borders coincides with the Central geosynclinal trough , The total extent of the belt is more than 1000 km , the width being 60-80 km ...
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Common terms and phrases
Afghanistan Alpine geosynclinal antimony Baluchistan Alpine Baluchistan geosynclinal development barite barite-polymetallic Bela region border central geosynclinal trough central geosynclinal zone Chagai median massif chalcopyrite characteristic characterized chromite deposits chromite ore belt complex confined copper and molybdenum copper-molybdenum Cretaceous Dalbandin distribution of endogenous Early Paleogene endogenous deposits endogenous mineralization Eocene epithermal felsic Fluorite deposits folded structures formation formed fracture zones fractured intrusions gabbro geological development geological structure Geological Survey geosynclinal regime geosynclinal trough zone granodiorite hematite Hindubagh region hydrothermal Indian Platform Khuzdar Las Bela lenses limestones Magmatism magnetite main folding Makran manganese manifestations Mesozoic metallogenic features metallogeny mineral deposits molybdenum Neogene North Waziristan occur Oligocene orebearing structures Paleogene Pishin Pishin-Makran trough Pishin-Makran zone plagiogranites porphyrites Quetta regularities of distribution schists sedimentation skarn southern structural zones submarine effusives Survey of Pakistan terrestrial effusives Tethys thickness took place ultramafic intrusions ultramafic rocks volcanogenous West Pakistan widely developed