• Gold Deposits In North Carolina
• Gold Deposits In Georgia

Renforth is offering the update above to shareholders as a result of concerns raised by shareholders regarding trading in shares of Renforth, which seems to contradict our ongoing operations and the current healthy financial and asset state of the Company, which include an open pit constrained gold deposit adjacent to Canadian Malartic and the. Gold may occur as deposits called lodes, or veins, in fractured rock. It may also be dispersed within Earth's crust. Most lode deposits form when heated fluids circulate through gold-bearing rocks, picking up gold and concentrating it in new locations in the crust. The Salaman Gold Deposit in Spain is located on the Leon fault close to small stocks and dykes of intermediate to basic rocks to which the mineralisation is related. Epithermal type mineralisation was developed in two successive stages, the earliest stage being dominant and extensive. The Salaman Gold Deposit in Spain is located on the Leon fault close to small stocks and dykes of intermediate to basic rocks to which the mineralisation is related. Epithermal type mineralisation was developed in two successive stages, the earliest stage being dominant and extensive. This stage comprised very fine crystalline gold-bearing.

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Gold Deposits In North Carolina

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Abstract

First posted November 10, 2020

Director, Geology, Geophysics, and Geochemistry Science Center
U.S. Geological Survey
Box 25046, MS–973
Denver, CO 80225

This report summarizes the primary characteristics of alkalic-type epithermal gold (Au) deposits and provides an updated descriptive model. These deposits, primarily of Mesozoic to Neogene age, are among the largest epithermal gold deposits in the world. Considered a subset of low-sulfidation epithermal deposits, they are spatially and genetically linked to small stocks or clusters of intrusions containing high alkali-element contents. Deposits occur as disseminations, breccia-fillings, and veins and may be spatially and genetically related to skarns and low-grade porphyry copper (Cu) or molybdenum (Mo) systems. Gold commonly occurs as native gold, precious metal tellurides, and as sub-micron gold in arsenian pyrite. Quartz, carbonate, fluorite, adularia, and vanadian muscovite/roscoelite are the most common gangue minerals. Alkalic-type gold deposits form in a variety of geological settings including continent-arc collision zones and back-arc or post-subduction rifts that are invariably characterized by a transition from convergent to extensional or transpressive tectonics.

Gold Deposits In Georgia

The geochemical compositions of alkaline igneous rocks spatially linked with these deposits span the alkaline-subalkaline transition. Their alkali enrichment may be masked by potassic alteration, but the unaltered or least altered rocks (1) have chondrite normalized patterns that are commonly light rare earth element (LREE) enriched, (2) are heavy rare earth element (HREE) depleted, and (3) have high large ion lithophile contents and variable enrichment of high-field strength elements. Radiogenic isotopes suggest a mantle derivation for the alkalic magmas but allow crustal contamination.

Oxygen and hydrogen isotope compositions show that the fluids responsible for deposit formation are dominantly magmatic, although meteoric or other external fluids (seawater, evolved groundwater) also contributed to the ore-forming fluids responsible for these deposits. Carbon and sulfur isotope compositions in vein-hosted carbonates and sulfide gangue minerals, respectively, coincide with magmatic values, although a sedimentary source of carbon and sulfur is evident in several deposits.

Deep-seated structures are critical for the upwelling of hydrous alkalic magmas and for focusing magmatic-hydrothermal fluids to the site of precious metal deposition. The source of gold, silver (Ag), tellurium (Te), vanadium (V), and fluorine (F) was probably the alkalic igneous rocks themselves, and the coexistence of native gold, gold tellurides, and roscoelite in several deposits is primarily a function of similar physicochemical conditions during deposition (for example, overlapping pH and oxygen fugacity (fO2).

Potential environmental impacts related to the mining and processing of alkalic-type epithermal gold deposits include acid mine drainage with high levels of metals, especially zinc (Zn), copper, lead (Pb), and arsenic. However, because alkalic-type gold deposits typically contain carbonates, which contribute calcium and magnesium ions that increase water hardness, aquatic life may be afforded some protection. Impacts vary widely as a function of host rocks, climate, topography, and mining methods.

Geologic mapping to (1) highlight the distribution of potassic alteration; (2) define fault density and orientation of structures; (3) determine the distribution of alkaline rocks and hydrothermal breccias; and (4) identify uniquely colored gangue minerals, such as fluorite and roscoelite, will be critical to exploration and future discoveries. Geophysical techniques that identify potassium (K) anomalies (for example, radiometric and spectroscopic surveys), as well as magnetic, resistivity, aeromagnetic, and gravity surveys, may help locate zones of high-permeability that control advecting hydrothermal fluids. Geochemical surveys that include analyses for Au, Ag, barium, Te, K, F, V, Mo, and mercury, which are key elements in these deposits, should be undertaken along with the measurement of other pathfinder elements such as arsenic, bismuth, Cu, iron, nickel, Pb, antimony, selenium, and Zn.

Suggested Citation

Kelley, K.D., Spry, P.G., McLemore, V.T., Fey, D.L., and Anderson, E.D., 2020, Alkalic-type epithermal gold deposit model: U.S. Geological Survey Scientific Investigations Report 2010–5070–R, 74 p., https://doi.org/ 10.3133/ sir20105070R.

ISSN: 2328-0328 (online)

Table of Contents

• Acknowledgments
• Abstract
• Introduction
• Deposit Type and Associated Commodities
• Regional Environment
• Physical Description of Deposit
• Geophysical Characteristics
• Hypogene and Supergene Ore Characteristics
• Hypogene and Supergene Gangue Characteristics
• Geochemical Characteristics
• Stable Isotope Geochemistry
• Hydrothermal Alteration
• Petrology of Associated Igneous Rocks
• Exploration/Resource Assessment Guides
• Geoenvironmental Features and Anthropogenic Mining Effects
• Metal Mobility from Solid Mine Waste
• Past and Present Mining Methods and Ore Treatment
• Volume and Footprint of Mine Waste and Tailings
• Smelter Signatures
• Climate Effects on Geoenvironmental Signatures
• Potential Ecosystem Impacts
• References Cited

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