Sediment-hosted stratiform lead-zinc depositsa short course sponsored by the Mineralogical Association of Canada and held immediately prior to the 1983 annual meeting in Victoria, B.C., May 11-13
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Mineralogical Association of Canada , [oronto]
Lead ores -- Congresses, Zinc ores -- Congresses, Petrology -- congr
|Other titles||Short course in sediment-hosted stratiform lead-zinc deposits|
|Statement||[D.F. Sangster, editor], organizing committee: D.F. Sangster, D. MacIntyre.|
|Series||Short course handbook -- v. 8, Short course handbook (Mineralogical Association of Canada) -- v. 8|
|Contributions||Sangster, D. F., Mineralogical Association of Canada.|
|LC Classifications||TN451 S8|
|The Physical Object|
|Pagination||x, 309 p. :|
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Genesis of Stratiform Sediment Hosted Lead and Zinc Deposits: Conference Proceedings (Stanford University Publications.
Geological Sciences, Vol 20) 0th Edition. Short Course in Sediment-Hosted Stratiform Lead-Zinc Deposits [D. Sangster] on *FREE* shipping on qualifying offers.
Most sediment-hosted stratiform lead-zinc deposits contain abundant iron sulfide, in contrast to the copper deposits which are characterized by low sulfide iron contents. Barite is abundant and massive in several of the lead-zinc deposits but is sparse in stratiform copper deposits.
Considering the large task of describing the broad subject matter, we excluded certain types of sediment-hosted Pb-Zn deposits. We will not discuss the fracture-controlled deposits in which fluorite is dominant and barite typically abundant (e.g., Central Kentucky, Hansonburg, New Mexico, or the English Pennines) or the fluorite-rich deposits such as those in southern Illinois, considered a.
Short course in sediment-hosted stratiform lead-zinc deposits. Responsibility: sponsorerd by the Mineralogical Association of Canada and held immediately prior to the annual meeting in Victoria, B.C., May ; edited by D.F.
Sangster. Sediment Hosted Lead-Zinc Sulphide Deposits - M. Deb, Wayne David Goodfellow - Google Books. The Deposit Modeling Program was founded by UNESCO-IUGS with the major aim to disseminate knowledge from scientists in more developed countries to their counterparts from less developed ones.
A fringe benefit of this effort was the compilation Sediment-hosted stratiform lead-zinc deposits book information on existing models and promotion of.
Get this from a library. Sediment-hosted stratiform lead-zinc deposits: a short course sponsored by the Mineralogical Association of Canada and held immediately prior to the annual meeting in Victoria, British Columbia, May [D F Sangster; Mineralogical Association of Canada.;].
By analogy with the volcanic-associated massive sulfide (VMS) deposits discussed earlier (Ch. 10), the descriptive term sediment-hosted massive sulfide (SMS) deposits is preferred, because it emphasizes the lithologic association of the deposits and excludes any genetic by: 2.
Description Sediment-hosted stratiform lead-zinc deposits PDF
Large sediment-hosted lead+zinc deposits like Mount Isa, McArthur River, Navan, Rammelsberg and Sullivan form a distinctive group characterised by stratiform, syngenetic sulphide ores that formed. Large DE () Sediment-hosted massive sulphide lead-zinc deposits: an empiral model.
In: Sangster DF (ed) Sediment-hosted stratiform lead-zinc deposits. Short Course Handbook by: 1. Sediment-hosted Lead-Zinc Sulphide Deposits comprises of thirteen chapters contributed by renowned economic geologists from three continents.
This book highlights the recent advances made in the understanding of the temporal and tectono-stratigraphic distribution of sediment-hosted Pb-Zn sulphide ores and processes governing their genesis. Nine of the 10 largest sediment-hosted Pb-Zn deposits are SEDEX. Of the deposits that contain at least million metric tons (Mt), there are 35 SEDEX (excluding Broken Hill-type) deposits.
Sediment-hosted Pb-Zn deposits contain the world's greatest lead and zinc resources and dominate world production of these metals. They are a chverse group of ore deposits hosted by a wide variety of carbonate and siliciclastic roch that have no obviolls genetic association with igneous activity.
A nmge of ore-fortl1ing processes in a vmiety of geologic and tectonic environments created these Cited by: The publication examines strata-bound tin deposits, geology of the Pine Point lead-zinc district, and genesis of the Rammelsberg ore deposit near Goslar/Upper Harz in the Federal Republic of Germany.
The selection is a valuable reference for researchers wanting to explore ore deposits. Sedimentary-Exhalative (SEDEX) Type Deposits “Syngenetic” stratiform, bedded Zn-Pb deposits hosted by fine-grained clastic sedimentary rocks. These three types may be considered as a spectrum of base-metal ore deposits which form in sedimentary rocks at some time during the evolution of a sedimentary basin.
SEDIMENT-HOSTED DEPOSITS. - Buy Sediment Hosted Stratiform Copper Deposits book online at best prices in India on Read Sediment Hosted Stratiform Copper Deposits book reviews & author details and more at Free delivery on qualified : R.
Boyle. Sediment-Hosted Zinc-Lead Deposits of the World— Database and Grade and Tonnage Models. By Donald A. Singer1, Vladimir I. Berger1, and Barry C.
Moring1. Open-File Report 1U.S. Geological Survey, Menlo Park, Calif. U.S. Department of the InteriorFile Size: KB. Detailed studies of the host lithologies, mineral textures, metal zoning and configurations of numerous sediment‐hosted stratiform copper deposits have established a post‐sedimentary (diagenetic) timing and overprint concept for the genesis of this important mineral deposit type.
Metals were probably deposited from low‐temperature oxidised saline brines which circulated across the Cited by: THE SEDIMENT-HOSTED STRATIFORM COPPER DEPOSIT MODEL.
Description: Sediment-hosted Lead-Zinc Sulphide Deposits comprises thirteen chapters contributed by renowned economic geologists from three continents.
This book highlights the recent advances made in the understanding of the temporal and tectono-stratigraphic distribution of sediment-hosted Pb-Zn sulphide ores and processes governing their genesis.
The Cannington deposit, situated at the southern end of the Mt. Isa basin, is a strata-bound, rather than stratiform, sedimentary rock-hosted Ag-Pb-Zn deposit, which shows sig- nificant differences from the other five deposits, and has been termed a Broken Hill-type deposit (Bodon, ; Walters and Bailey, ; Walters et al., ).
Carbonate-hosted lead-zinc ore deposits are important and highly valuable concentrations of lead and zinc sulfide ores hosted within carbonate (limestone, marl, dolomite) formations and which share a common genetic origin. These ore bodies range from million tonnes of contained ore, to 20 million tonnes or more, and have a grade of between 4% combined lead and zinc to over 14% combined.
typically fine-grained and stratiform down to the hand-specimen scale. They are also commonly referred to as "sediment-hosted stratiform deposits" or "sedimentary-exhalative lead-zinc", or "sedex" deposits because they are considered to mainly have formed through exhalation of basinal brines atCited by: 6.
Pb-Zn-Ag stratiform deposits occur in ancient continental rift sediments (Sawkins, ). These deposits, which are not associated with igneous rocks, occur in marine carbonates and are probably deposited from brines, which migrate to the edge of rift basins.
Particular attention has been paid to the sediment-hosted, stratiform lead-zinc and volcanic-hosted massive sulphide deposits, but the review also includes discussions of Archaean ocean composition, orogenic lode gold deposits, Proterozoic Broken Hill-type and Cu and Au ores, and banded iron formations and their related iron ores.
Details Sediment-hosted stratiform lead-zinc deposits PDF
Stratiform ore deposits associated with calc-alkaline and tholeiitic volcanism form as chemically precipitated sediments and, like other sediments, display facies variations. An attempt to characterise these vertical and lateral facies variations and to relate them to distance in time and space from the volcanic centre is presented here.
Table of Contents. Preface / Section I: Australian and Canadian Deposits: Proterozoic Stratiform Sediment-Hosted Zn-Pb-Ag Deposits of Northern Australia-Ross Large et.
/ Geology, Genesis and Exploration of SEDEX Deposits, with Emphasis on the Selwyn Basin, Canada-Wayne D. Goodfellow / Geology of the Belt-Purcell Basin and the Sullivan deposit-John W.
Lydon / Genetic models for. Sedimentary exhalative deposits (SedEx deposits) are ore deposits which are interpreted to have been formed by release of ore-bearing hydrothermal fluids into a water reservoir (usually the ocean), resulting in the precipitation of stratiform ore.
SedEx deposits are the most important source of lead, zinc and barite, a major contributor of silver, copper, gold, bismuth and tungsten. Purchase Regional and Specific Deposits, Volume 9 - 1st Edition.
Download Sediment-hosted stratiform lead-zinc deposits PDF
Print Book & E-Book. ISBNBook Edition: 1. Sediment-Hosted Lead-Zinc Deposits in Earth History scale) laminated and stratiform ores that formed by highly se-lective carbonate replacement millions of years after deposition of the host rocks. Other deposits containing strati-form and laminated sulfides in a variety of rocks, particularly.
Porphyry–Copper Deposits Sediment-Hosted Stratiform Copper Deposits 3. Major Sources of Base Metals Historical Immediate Past and Present Near Future Glossary Bibliography Biographical Sketch Summary In the geological and mining File Size: KB.Large sediment-hosted lead+zinc deposits like Mount Isa, McArthur River, Navan, Rammelsberg and Sullivan form a distinctive group characterised by stratiform, syngenetic sulphide ores that formed in local basins on the sea floor as a result of protracted hydrothermal activity accompanying continental rifting.
Generally there is a development of a sedimentary pre-ore phase mineralization often.A List to some Major Types of Ore Deposits and a link Book Download. Komatiite-associated nickel deposits Layered mafic-ultramafic intrusion deposits Skarn deposits Fractionated granitoid-associated deposits Porphyry-associated deposits Iron oxide copper gold deposits Syn-deformational hydrothermal and replacement deposits Orogenic gold deposits Carbonate-hosted stratabound lead-zinc deposits.
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