Geological Bulletin, Volume 6University of Peshawar, 1971 - Geology |
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Page 102
... complexes is thermodynaically the most feasible mechanism . Moreover , the solubility of most metal complexes is well within the geologically feasible limits . However , there is a lot of controversy concerning the relative importance ...
... complexes is thermodynaically the most feasible mechanism . Moreover , the solubility of most metal complexes is well within the geologically feasible limits . However , there is a lot of controversy concerning the relative importance ...
Page 103
... complexes of different orders under various temperatures aud chloride ion concentrations . However , the most important complexes are PbCl * and PbCl.:- . At elevated temperatures above 300 ° C , PbCI + is the most stablo complex in ...
... complexes of different orders under various temperatures aud chloride ion concentrations . However , the most important complexes are PbCl * and PbCl.:- . At elevated temperatures above 300 ° C , PbCI + is the most stablo complex in ...
Page 105
... complexes are most important . In the system ZnS - H_S - NaCl - H20 , Hinners and Holland ( 1963 ) have shown that at 80 ° C and neutral conditions ZnSxhH S complexes usually Predominate . The same conclusion has been drawn by Anderson ...
... complexes are most important . In the system ZnS - H_S - NaCl - H20 , Hinners and Holland ( 1963 ) have shown that at 80 ° C and neutral conditions ZnSxhH S complexes usually Predominate . The same conclusion has been drawn by Anderson ...
Contents
Preliminary geology and petrography of Swat Kohistan | 1 |
The geology of the Gandghar Range Distt Hazara N W F | 33 |
Lithological classification and environment of deposition of | 43 |
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abundant altered amphibolites appears associated bands base beds biotite body brown Bull chlorite colour common complex concentration consist contain correlated cover crystalline crystals dark deposits developed diorites distance dykes east eastern epidote exposed extend feet feldspar folded foliation Formation fractures Gandghar Range garnet Geol geology gneisses grades grains granites green grey Group Hazara hornblende inches Indus intrusions iron Kalam Kohistan latter layers light limestone locally located Lower marble material Member metals Middle miles minerals minor natural norites occur outcrop Pakistan pegmatite Peshawar phyllites places plagioclase present probably quartz quartzites rare region result River road rocks samples schists seen sericite shale shear slates solubility solutions southern stream strike structure suggest sulphide Swat temperature thick thin transport types Univ Upper usually valley varieties various veins village volcanic waters western zone