Turbidite-hosted Gold Deposits

Turbidite-hosted Gold Deposits PDF Author: J. Duncan Keppie
Publisher: St. John's, Nfld., Canada : Geological Association of Canada
ISBN:
Category : Science
Languages : en
Pages : 200

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Turbidite-hosted Gold Deposits

Turbidite-hosted Gold Deposits PDF Author: J. Duncan Keppie
Publisher: St. John's, Nfld., Canada : Geological Association of Canada
ISBN:
Category : Science
Languages : en
Pages : 200

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Turbidite-hosted gold deposits

Turbidite-hosted gold deposits PDF Author: Prudence Mary Leeming
Publisher:
ISBN:
Category :
Languages : en
Pages :

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A Comparative Study of the Turbidite-hosted Gold Deposits in the Bendigo-Ballarat and Melbourne Zones, Central Victoria, Australia

A Comparative Study of the Turbidite-hosted Gold Deposits in the Bendigo-Ballarat and Melbourne Zones, Central Victoria, Australia PDF Author: Zhan Lin Gao
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 596

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Turbidite-hosted Micro-disseminated Gold Deposits

Turbidite-hosted Micro-disseminated Gold Deposits PDF Author: Xuexiang Gu
Publisher:
ISBN: 9787561632154
Category :
Languages : en
Pages : 240

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Mineral Resources, Economics and the Environment

Mineral Resources, Economics and the Environment PDF Author: Stephen E. Kesler
Publisher: Cambridge University Press
ISBN: 1316368580
Category : Technology & Engineering
Languages : en
Pages : 447

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Book Description
Written for students and professionals, this revised textbook surveys the mineral industry from geological, environmental and economic perspectives. Thoroughly updated, the text includes a new chapter on technology industry metals as well as separate chapters on mineral economics and environmental geochemistry. Carefully designed figures simplify difficult concepts and show the location of important deposits and trade patterns, emphasising the true global nature of mineral resources. Featuring boxes highlighting special interest topics, the text equips students with the skills they need to contribute to the energy and mineral questions currently facing society, including issues regarding oil pipelines, nuclear power plants, water availability and new mining locations. Technical terms are highlighted when first used, and references are included to allow students to delve more deeply into areas of interest. Multiple choice and short answer questions are provided for instructors online at www.cambridge.org/kesler to complete the teaching package.

Turbidite-hosted Gold Deposits, Meguma Domain, Eastern Nova Scotia

Turbidite-hosted Gold Deposits, Meguma Domain, Eastern Nova Scotia PDF Author: P. K. Smith
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 67

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Controls on Genesis, Distribution, and Nature of the Turbidite-hosted Gold Deposits, Eastbelt, Southwestern Slave Structural Province, Yellowknife, Northwest Territories

Controls on Genesis, Distribution, and Nature of the Turbidite-hosted Gold Deposits, Eastbelt, Southwestern Slave Structural Province, Yellowknife, Northwest Territories PDF Author: Mark Wesley Richardson
Publisher:
ISBN:
Category :
Languages : en
Pages : 0

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The Ptarmigan and Tom mesothermal gold deposits are located 10 km to the northeast of the city of Yellowknife, Northwest Territories. Both gold deposits comprise a series of en echelon veins. These veins are hosted within upper greenschist to lower amphibolite facies ~2630 Ma rocks. A low-temperature reduced hydrothermal environment during ore deposition formed as either a part of the main arsenopyrite-dominated mineralization or a distinct late-stage ore-formation event. At the deposit scale, the high-grade gold ores are preferentially developed with three contextual scenarios: (1) along contacts, especially the contact between black siltstone host rock and major barren, cleavage-parallel veins; (2) the contact between quartz laminae and carbonaceous host rock slivers; (3) proximity to bismuth telluride mineralization. Thus, competent, barren quartz veins along the axial plane of fold/thrust belts locally host superimposed gold mineralization and provide favourable targets for gold exploration. Hydrothermal apatite is a common accessory mineral in both mineralized and non-mineralized quartz veins in the metasedimentary host rocks that constitute the Ptarmigan and Tom deposits. The apatite in this study likely formed coeval with early stages of sulphide precipitation. The apatite age of 2585 ± 15 Ma is consistent with the intrusions of the 2605 and 2590 Ma two-mica granites of the Prosperous Suite. The near-concordant [superscript 204]Pb-corrected data of the LCT pegmatite hosted apatite reveals two clusters of ages. An older population with an intercept age (N = 4) of 2581 ± 15 Ma, and a younger population with an intercept age (N = 3) of 2519 ± 12 Ma . Furthermore, plotting a regression through all near – concordant data for the pegmatite hosted apatite hints that metamorpic resetting occured around ~2200 Ma. The distribution and abundance of major, minor, and trace elements from in-situ recovered apatite were studied to characterize the nature of mineralizing fluids. Most apatite from mineralized and non-mineralized veins show different Mn, Sr, and Pb contents, as well as chondrite-normalized rare-earth element (REE) and Y abundance patterns. REEs display five unique chondrite-normalized patterns: (1) negative sloped pattern with slight negative Eu anomaly, (2) a flat pattern with a positive Eu anomaly, (3) a positive slope with a negative Eu anomaly, (iv) light rare earth element (LREE) depleted pattern with positive Eu anomaly, and (v) bell-shaped pattern with a negative Eu anomaly. The REE patterns likely reflect both the source of the auriferous hydrothermal fluids and, perhaps, co-precipitating mineral phases. Apatite from the Ptarmigan vein occurs with both: (1) a flat pattern with a positive Eu anomaly and (2) bell-shaped pattern with a negative Eu anomaly. The bell-shaped and flat patterns typify orogenic gold deposits. Vein-hosted apatite commonly displays compositional zoning with a characteristic yellow cathodoluminescence (CL) emission spectra with darker cores and brighter rims. The cores have lower REE, whereas the rims are notably REE higher. It is thought that the darker cores in CL images reflect a transition from an early low REE hydrothermal fluid to one enriched in REE. Lastly, this study breaks ground for conducting a more robust study to classify the trace-element composition of apatite in gold deposits worldwide.

The Lithogeochemical and Mineralogical Setting of Turbidite Hosted Arsenic-gold Deposits in the Lower Palaeozoic of Scotland

The Lithogeochemical and Mineralogical Setting of Turbidite Hosted Arsenic-gold Deposits in the Lower Palaeozoic of Scotland PDF Author: Paul R. Duller
Publisher:
ISBN:
Category :
Languages : en
Pages :

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Turbidite-hosted gold deposits, Meguma domain, eastern Nova Scotia

Turbidite-hosted gold deposits, Meguma domain, eastern Nova Scotia PDF Author: P. K. Smith
Publisher:
ISBN:
Category :
Languages : en
Pages : 67

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The Metallogeny of Lode Gold Deposits

The Metallogeny of Lode Gold Deposits PDF Author: Ulrich Kretschmar
Publisher: Elsevier
ISBN: 0128032235
Category : Science
Languages : en
Pages : 356

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Book Description
The Metallogeny of Lode Gold Deposits: A Syngenetic Perspective is a synthesis of lode gold vein forming processes, addressing the commonality in similar worldwide deposits. The book's empirical model incorporates widely known and accepted principles of ore deposition and shows how it applies in the volcanic-sedimentary greenstone belt environment. Several chapters detail outcrop maps and photos of field occurrences and textures. The interpretations flow directly from the authors' field work, and are coupled with analyses of underlying physical processes. Utilizing detailed geological mapping, field work, and chemical analyses as the basis of a syngenetic formation mode, the text arms readers with the tools necessary to accurately analyze and interpret new data on the subject. This includes information on decoding the significance of asymmetry in vein formation, as well as the role of lamprophyres in gold camps, how Archean geology requires integration into a lode vein formation model, and how to develop an understanding of the worldwide applicability of gold cycles to lode vein formation and exploration and how it can be applied to deposits of all ages. - Presents the first book to galvanize lode gold research into a single authoritative reference - Simplifies the complexity of lode gold's underlying processes and presents valid concepts surrounding the lode gold forming environment - Features color figures, illustrations, and photos that enrich the content's focus and aid in the retention of key concepts