Memoirs of the Geological Survey of Pakistan, Volume 7The Survey, 1969 |
From inside the book
Results 1-3 of 4
Page 3
... northern part of the Baluchis- tan geosyncline is of Late Cretaceous - Paleocene age . The instrusions of ultramafic rocks in the Hindubagh region reach considerable dimensions , the largest of them are 40 km long and 20 km wide . In ...
... northern part of the Baluchis- tan geosyncline is of Late Cretaceous - Paleocene age . The instrusions of ultramafic rocks in the Hindubagh region reach considerable dimensions , the largest of them are 40 km long and 20 km wide . In ...
Page 8
... northern part of the belt whereas in the southern part of the Las Bela region barite and barite - galena mineralization is most important . It is quite possible that within this zone skarn iron - ore and copper deposits connected with ...
... northern part of the belt whereas in the southern part of the Las Bela region barite and barite - galena mineralization is most important . It is quite possible that within this zone skarn iron - ore and copper deposits connected with ...
Page 9
... northern marginal part , within the rigid structures of the Chagai median massif that are a consolidated enclosing rock of Alpine geosynclinal troughs located to the south . In the central parts of the Baluchistan geosyncline as well as ...
... northern marginal part , within the rigid structures of the Chagai median massif that are a consolidated enclosing rock of Alpine geosynclinal troughs located to the south . In the central parts of the Baluchistan geosyncline as well as ...
Other editions - View all
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