Memoirs of the Geological Survey of Pakistan, Volumes 7-8The Survey, 1969 |
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Page 3
... Hindubagh region is of the Eocene age . This conclusion is due to the fact that limestones containing fauna of this age obviously super- impose the weathered surface of the ultramafic rocks . According to these data the time of ...
... Hindubagh region is of the Eocene age . This conclusion is due to the fact that limestones containing fauna of this age obviously super- impose the weathered surface of the ultramafic rocks . According to these data the time of ...
Page 8
... Hindubagh and Las Bela zone . For the Hindubagh zone which has a sub - latitudinal trend , a pronounced confinement of ultramafic intrusions to the old zones of fractures is very characteristic . Beyond the chro- mite belt a zone of ...
... Hindubagh and Las Bela zone . For the Hindubagh zone which has a sub - latitudinal trend , a pronounced confinement of ultramafic intrusions to the old zones of fractures is very characteristic . Beyond the chro- mite belt a zone of ...
Page 12
... Hindubagh ; III - Fort Sandeman ( southern fra ment of Waziristan zone ) ; IV — Ras Koh zone . The scheme is compiled on the data of the Geological Survey of Pakistan ( GSP ) and the geotectonic bas worked out by K. N. Kravchenko , B.A. ...
... Hindubagh ; III - Fort Sandeman ( southern fra ment of Waziristan zone ) ; IV — Ras Koh zone . The scheme is compiled on the data of the Geological Survey of Pakistan ( GSP ) and the geotectonic bas worked out by K. N. Kravchenko , B.A. ...
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Common terms and phrases
ammonite ammonite bed antimony argillaceous limestone bed Bajocian Baluchistan Baluchistan geosynclinal development barite Bathonian Belemnite bifurcating body chamber central geosynclinal trough Chagai median massif Chiltan limestone Choffatia chromite chromite deposits Cutch described specimen diadematus Waagen disconformably Dolikephalites endogenous deposits endogenous mineralization Fatmi felsic fluorite fluorite deposits fractured genus geosynclinal holotype Homoeoplanulites indet Indian Platform Indocephalites Locality.-Wam Tangi Lower Callovian Lower Callovian ammonite Macrocephalites magmatism magnetite Massive limestone Mazar Drik formation Mazar Drik limestone metallogeny microconch molybdenum Noetling Oligocene Paleogene Paralcidia Pishin Pleurocephalites polyphemus primary ribs pyritic pyritic argillaceous limestone regularities of distribution ribbing style rocks Sembar formation sequence shale shell side view skarn southern Spath specimens internal mould Stratigraphic Range.-Lower Callovian subgenus Survey of Pakistan Takatu limestone thin bedded limestone Tithonian trifurcate ultramafic intrusions Umbilical diameter umbilical wall umbilicus Upper venter volcanogenous Vredenburg 1909 Wam Tangi West Pakistan Whorl height whorl section whorl side Whorl thickness