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Geology of lead-zinc vein deposits in formations of the geosynclinal stage
International Geology Review, 1969exaly +2 more sources
On Some Problems oi the Lead Isotope Method and Its Application in Geology
1985exaly +2 more sources
The geology of the Zawar lead-zinc mine; a reply
Economic Geology, 1968Reply is made to several critical discussions published since the publication of the original paper in 1964 (for reference, see this Bibliography Vol. 29, Mookherjee 1; see also Vol. 29, Mookherjee 2; Vol. 30, Poddar 2; Vol. 31, No. 4, 02 E67-02447; Vol. 32, No. 1, 02 E68-00608). The deposit is regarded as a product of ascending hydrothermal solutions.
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The data of lead isotope geology related to problems of ore genesis
Economic Geology, 1961Searching questions about the origins of ore deposits have been asked for many years. Where do ore fluids originate - within the crust, or deeper? Can specific sources of ore metals be identified? When were ores deposited? How long did mineralization continue? What was the rate and paragenesis of deposition?
R. S. Cannon +3 more
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The geology of the Aguilar lead-zinc mine, Argentina
Economic Geology, 1950"The Aguilar deposit, in northern Argentina, is a hypothermal lead, zinc, silver replacement in Cambrian calcareous quartzite. The rocks had previously been altered to tactite by a granite stock whose contact is from 150 to 250 m. from the ore bodies.
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Geology of the zinc-lead deposit on Calumet Island, Quebec
Geological Society of America Bulletin, 1941The zinc-lead deposit described is located on Calumet Island, Quebec, 53 miles northwest of Ottawa. The complex ores resemble those of Edwards, New York, and Montauban, Quebec, and other Grenville deposits. They occur in moderately inclined Grenville metamorphic rocks, including crystalline limestone, amphibolite, amphibolite-gneisses, quartzitic ...
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Geology and structural features of vein-type lead and zinc deposits
Geology of Ore Deposits, 2007The geological and structural position and localization conditions of the vein-type Pb-Zn deposits of the Sadon (North Ossetia) and East Karamazar (North Tajikistan) ore districts are considered. The leading role of long-lived deep faults in the control of large deposits is emphasized. Examples of such deposits in different provinces are given.
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Geology of the Ozark Lead Company Mine, Viburnum Trend, Southeast Missouri
Economic Geology, 1977In contrast to most of the other mines in the Viburnum Trend, much of the Ozark Lead Company orebody lies at right angles to the depositional strike of the sediments. This divergence is due to localization of much of the ore along the flank of a northwest-trending Precambrian high situated on the upthrown side of a high-angle reverse fault.A second ...
M. M. Mouat, C. W. Clendenin
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