3 edition of Geologic Controls of Lead and Zinc Deposits in Goodsprings (Yellow Pine) District, Nevada found in the catalog.
Geologic Controls of Lead and Zinc Deposits in Goodsprings (Yellow Pine) District, Nevada
United States Geological Survey
|Series||U.S. Geological Survey bulletin -- 1010|
|Contributions||Albritton, C.C., Richards, A., Brokaw, A.L.|
Geologic setting of the lead and zinc deposits, Drenchwater Creek area, Howard Pass Quadrangle, Western Brooks Range, Alaska Open-File Report C. Following the war, the Bertha Mineral Company owned the mine and began using the mineral deposits to manufacture slab zinc. In , New Jersey Zinc acquired the site and mined both lead and zinc. The invention of the floatation process in resulted in a .
Courtesy Google Books. Yellow Pine and Prairie Flower Mines. by Claude C Albritton Jr. and John A Reinemund. Geologic Controls of Lead and Zinc Deposits in Goodspring (Yellow Pine) District, Nevada. Geologic Survey Bulletin deposit. hewett, d.f., , geology and ore deposits of goodsprings quad: usgs p.p., , p. deposit. longwell, c.r., , , geology and mineral.
PP / Knopf, A. / GEOLOGY AND ORE DEPOSITS OF THE YERINGTON DISTRICT, NEVADA, , afb, 68 pages, 5 plates, 12 figs., $ 50 PP / Hewett, D. F. / GEOLOGY AND ORE DEPOSITS OF THE GOODSPRINGS QUADRANGLE, NEVADA, , afb, pages, 40 plates (6 in pocket on 7 sheets), 55 figs., $ The Potosi Mine is a zinc and lead mine located in Clark county, Nevada at an elevation of 6, feet HEWETT, D.F., , GEOLOGY AND ORE DEPOSITS OF GOODSPRINGS QUAD: USGS P.P., , P. Reference Category: Deposit. GEOLOGIC CONTROLS OF LEAD AND ZINC DEPOSITS IN GOODSPRINGS (YELLOWPINE) DISTRICT, NEVADA: .
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2 GEOLOGIC CONTROLS OF LEAD AND ZINC DEPOSITS and joints of different trends converge and link without offset, or where differ ential movement had created openings along arcuate faults. Locally the breccia along the feeding fissures was mineralized ; more commonly the ore formed in permeable ground that was marginal to the by: 1.
Geological Controls of Lead and Zinc Deposits in Goodsprings (Yellow Pine) District, Nevada Paperback – January 1, by John A. Reinemund Albritton, Claude C., Jr., Arthur Richards, Arnold L.
Brokaw (Author)Author: John A. Reinemund Albritton, Claude C., Jr., Arthur Richards, Arnold L. Brokaw. Geologic controls of lead and zinc deposits in Goodsprings (Yellow Pine) district, Nevada (OCoLC) Material Type: Government publication, National government publication: Document Type: Book: All Authors / Contributors: Claude C Albritton; Arthur Richards; Arnold L Brokaw; John A Reinemund; Geological Survey (U.S.).
Additional Physical Format: Print version: Albritton, Claude C., Geologic controls of lead and zinc deposits in Goodsprings (Yellow Pine) district, Nevada. Structural and paleotopographic controls of lead-zinc mineralization in the Silvermines orebodies, Republic of Ireland Stewart Taylor.
Stewart Taylor genesis lead-zinc deposits metal ores Paleozoic Western Europe Tournaisian Tipperary by: We do not discuss oxide zinc deposits because they have been discussed in a special issue devoted to “Nonsulfide Zinc Deposits: A New Look” (Economic Geology, v.
98, no. 4, ). Objectives The main objectives of this paper are to summarize the salient features of sediment-hosted Pb-Zn deposits and to define the current understanding on. Goodsprings Mining District, Spring Mountains, Clark Co., Nevada, USA: A Cu-Zn-Pb-Ag-Au-V-U mining area located in the Spring Mountains, W of Goodsprings (town).
The ore deposits in the Goodsprings district remained unworked untilalthough. LEAD-ZINC DEPOSITS Quarries Figure 2 shows the positions of the seven quarries withintheIshiagudistrict. QuarryI()occurs km WSW of the Ishiagu railway station on the Enugu to Port Harcourt line.
and are km NE and km W of respectively. Ouarry4 is approximately NW of and at a distance of by: Mackenzie, D. and Davies, R. () Broken Hill lead-silver-zinc deposit at Z. mines, in F. Hughes eds., Geology of the Mineral Deposits of Australia and Papua New Guinea, The Australian Institute of Mining and Metallurgy, Author: 鞠子 正.
Magmatic deposits result when the minerals settle to the bottom of the intrusive body and form thin, high‐grade layers. Hydrothermal deposits rich in copper, lead, zinc, gold, silver, molybdenum, tin, mercury, and cobalt form from hot solutions that circulate through fractured country rock.
The solutions come from nearby intrusions or heated. Part or all of this report is presented in Portable Document Format (PDF). For best results viewing and printing PDF documents, it is recommended that you download the documents to your computer and open them with Adobe Reader.
This book is the result of one such workshop that took place in Delhi and Udaipur, India, in December Sediment-hosted Lead-Zinc Sulphide Deposits compiles the work of renowned economic geologists from three continents. Geology of lead and zinc How lead and zinc deposits are formed: Origin and formation conditions of deposits are now considered more in their classification.
However, several classifications have been proposed that each of them has been accepted by a number of economic geologists. The manuscript takes a look at the McArthur zinc-lead-silver deposits, Appalachian zinc-lead deposits, and tri-state ore deposits. The selection is a dependable source of data for researchers wanting to study Cu, Zn, Pb, and Ag deposits.
GEOLOGICAL SURVEY GEOLOGIC AND GRADE-TONNAGE INFORMATION ON VOLCANIC-HOSTED COPPER-ZINC-LEAD MASSIVE SULFIDE DEPOSITS By D.L.
Mosier, D.A. Singer, and B.B. Salem Open-File Report This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standardsCited by: the Nigerian Mining Corporation has indicated proved reserves of up totonnes .
Nigerian Lead-Zinc Mining Company in gave conservative indicated reserves oftonnes with % lead and % zinc . The Abakaliki field is still Nigeria’s most important lead-zinc deposit.
In Azara area, the Nigerian MiningCited by: 1. Most of the world's Mississippi Valley-type (MVT) zinc–lead deposits occur in orogenic forelands. We examine tectonic aspects of foreland evolution as part of a broader study of why some forelands are rich in MVT deposits, whereas others are barren.
The type of orogenic foreland (collisional versus Andean-type versus inversion-type) is not a first-order control, because each has MVT deposits Cited by: Special Publication No.4, The papers included in this volume were originally presented orally or as posters at the Society of Economic Geologists International Field Conference on Carbonate-Hosted Lead-Zinc Deposits, held in St.
Louis, Missouri, JuneThe concept for this conference was first aired at the conclusion of an SEG. The characteristic features of CD zinc-lead deposits and the problems inherent in classifying them have been discussed by Leach et al. ( Leach et al.
Sediment-Hosted Lead-Zinc Deposits in Earth History Article in Economic Geology (3) June with 4, Reads How we measure 'reads'. B / THE GEOLOGY AND ORE DEPOSITS OF THE REESE RIVER DISTRICT, LANDER COUNTY, NEVADA,pages, 11 plates (in pocket), 33 figs., $ 20 B Series: Zinc and Lead Deposits in Southeast Alaska.Abstract.
Although several deposit types have either been shown or suggested to be associated with paleokarst features in carbonate rocks, lead—zinc sulfide deposits of the “Mississippi Valley-type“ (MVT) have received the most research and by: Argentena Mine, Goodsprings Mining District, Spring Mountains, Clark Co., Nevada, USA: Sec 34 T24S R58E Zn Pb Ag Au Cu V Geology: The ore bodies lie in breccia zones parallel to subparallel to the bedding.
Bedding strikes northward.