4 edition of Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada found in the catalog.
Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada
by U.S. Dept. of the Interior, U.S. Geological Survey in Menlo Park, CA
Written in English
|Statement||by Ted G. Theodore ... [et al.].|
|Series||Open file-reports -- 00-402., U.S. Geological Survey open-file report -- 00-402.|
|Contributions||Theodore, Ted G., Geological Survey (U.S.)|
|The Physical Object|
|Pagination||iii, 125 p.|
|Number of Pages||125|
Heitt D G, Dunbar W W, Thompson T B, Jackson R G - Geology and geochemistry of the Deep Star gold deposit, Carlin Trend, Nevada: in Econ. Geol. v98 pp Ressel M W, Noble D C, Henry C D, Trudel W S - Dike-hosted ores of the Beast deposit and the importance of Eocene magmatism in Gold mineralization of the Carlin Trend, Nevada. The Betze/Post orebody of the Goldstrike mine is located on the boundary of Elko and Eureka Counties in north-eastern Nevada, some 40 km to the NNW of the township of Carlin, and 60 km NW of Elko. It is the largest known sediment hosted disseminated gold mine on the Carlin Trend. SUMMARY Pre-mining, the deposit contained around t of gold.
Regional studies in the Beaver Peak (BP) area of the Tuscarora Mountains, Nev., near the northern Carlin trend of Au deposits (fig. 1) have shown that the Upper Pennsylvanian and Lower Permian Strathearn Formation overlap assemblage Author: Vladimir I. Berger, Donald A. Singer, Ted G. Theodore, Anita G. Harris, Calvin H. Stevens. Tuscarora 30xminute Quadrangle Geologic Maps "Title","Year","Author","County","Publisher","Series","Plate","Scale","Remarks","Nlat","Slat","Wlong","Elong","Long_c.
Carlin Trend Map. the carlin trend is a 60 kmlong, northwesttrending linear alignment of approximately 42 disseminated gold deposits located in northeastern nevada figure 1he trend contains 5, mt of gold and contributes 9 of the worlds annual gold production, with annual production of 4 m oz hofstra and cline, The type section of the Upper Pennsylvanian and Lower Permian Strathearn Formation Dott, , Cashman et al., , Cashman et al., is near Carlin Canyon in SW 1/4 Sec. 19, T. 33 N., R. 55 E., approximately 20 km southeast of BP Fig. 1, Fig. formation at the type section is at most m thick. It is composed of mostly quartz-sandy limestone Cited by: 3.
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Publication type: Report: Publication Subtype: USGS Numbered Series: Title: Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada. Buy Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada (SuDoc I ) on FREE SHIPPING on qualified orders.
Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada [microform] / by Ted G. Theodore [et al.] U.S. Dept. of the Interior, U.S. Geological Survey Menlo Park, CA Australian/Harvard Citation.
Get this from a library. Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada. [Ted Nevada book Theodore; Geological Survey (U.S.);]. Buy Rock geochemistry in the Tuscarora Mountains, northern Carlin Trend, Nevada (SuDoc I ) by U.S.
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Geological Survey. commonly are clustered in linear arrays as along the Carlin trend and elsewhere in Nevada. In order to address this question in northern Carlin Trend southern Tuscarora Mountains near the northern terminus of the Carlin trend, systematiccollaborative geologic mapping of the Santa Renia Fields and Beaver Peak quadrangles currently is underway by the Size: 5MB.
THE KM-LONG Carlin trend is the most important of sev-eral major gold-producing areas of north-central Nevada and contains the greatest concentration of Carlin-type gold de-posits in the world. Gold production, reserves, and resources from the sedimentary rock-hosted or Carlin.
The deposit is in secs. 13 T. 35 N., R. 50 E., in the Tuscarora Mountains in northern Eureka County, Nevada. Sincethe Carlin mine has. Cyanide heap leaching- is a technique that was pioneered at the Nevada Carlin trend.
Bymines in the Carlin Trend had produced over 70 million. Ettner, DavidStratigraphy and structure of the Devonian autochthonous rocks, north-central Carlin trend of the southern Tuscarora Mountains, northern Eureka County, Nevada.
[M.S. Thesis] Pocatello/Boise, Idaho State University/Boise State University, p. 3 plates. Applied Geochemistry, Geology, and Mineralogy of the Northernmost Carlin Trend, Nevada Ted G. Theodore U.S. Geological Survey, Middlefield Road, Menlo Park, California Cited by: Controls of Fault and Fold Geometry on the Distribution of Gold Mineralization on the Carlin T rend Figure 5B.
Geology of the southern Lynn W indow, Leeville-Carlin and Genesis Bluestar districts. Buy Re-Examination of Rock Geochemistry in the Copper Canyon Area, Lander County, Nevada: Usgs Open-File Report on FREE SHIPPING on qualified orders Re-Examination of Rock Geochemistry in the Copper Canyon Area, Lander County, Nevada: Usgs Open-File Report Kotlyar, B.
B., Theodore, T. G., Jachens, R. C.: Author: R. Jachens. All of these rock types are present along the northern and southern Carlin trend (Tuscarora Mountains) as a complexly intercalated, folded, and imbricated mass. The Vinini Formation contains an estimated cumulative thickness in excess of 5, feet (1, m).
On the Carlin trend, this sequence is host to smaller high-angle. chemistry of the Carlin deposit, the largest dissemi- nated replacement gold deposit in carbonate rocks discovered to date in the western United States. The deposit is in secs. 13 T. 35 N., R. 50 E., in the Tuscarora Mountains in northern Eureka County, Nevada (Fig.
Sincethe Carlin. Following concepts proposed on the relationship of gold and silver mineralization to windows through the Palaeozoic Roberts Mountains thrust fault in north-central Nevada (Roberts, ), Newmont conducted an exploration programme in the Tuscarora Mountains north of Carlin, Nevada, that resulted in the discovery of the Carlin gold deposit in Cited by: Interstate 80 between Elko and Carlin, Nevada, follows the valley of the Humboldt River.
The Humboldt drains a 17, square mile basin along its mile course, located entirely within the State of Nevada. While barely a trickle of water in late summer, spring floods may swell the river well over its banks. JOURNAL OF GEOCHEMICAL EXPLORATION ELS EV I ER Journal of Geoche~cal Exploration 51 () Geology and lithogeochemistry of the Ren gold prospect, Elko County, Nevada the role of rock sampling in exploration for deep Carlin-type deposits George V.
Albinot U.S. Geological Survey, Reno Field Office, c/o Mackay School of Mines, University of Nevada, Cited by: 6. Implications of Regional Geology and Geochemistry in the Northern Carlin Trend, Southern Tuscarora Mountains, Nevada.
Lewis Teal | Regional Geologist, Newmont Mining. Geologic Overview of the Carlin-Trend Gold Deposits and Carlin-Type Deposits in Southern China. Andy Wallace | Exploration Manager, Cordex Exploration. Folowing concepts proposed on the relationship of gold and silver mineralization to windows through the Palacozoic Roberts Mountains thrust fault in north-central Nevada (Reboerts, ), Newmont conducted an exploration proramme in the Tuscarora Mountains north of Carlin, Nevada, that resulted in the discovery of the Carlin gold deposit in Cited by:.
the west side of the North Tuscarora Range and the south end of the Owyhee Desert around the Burner Hills. In recent years very few elk have been observed wintering in unit along the west side of the South Tuscarora Range (north of the Carlin Trend mining area) and Richmond Mountain south to Marys Size: 77KB.Author of Geochemistry and geology of deep drill holes at Iron Canyon, Lander County, Nevada, Geochemistry and potassium-argon ages of plutonic rocks in the Battle Mountain mining district, Lander County, Nevada, Geology and geochemistry of the west ore body and associated skarns, Copper Canyon porphyry copper deposits, Lander County, Nevada, Geology and geochemistry .The geology of Nevada began to form in the Proterozoic at the western margin of North America.
The Carlin trend extends from the Pinon Range to the Tuscarora Mountains, an area 70 miles long and 10 miles wide. Epithermal, skarn, vein and Carlin-type deposits are also found in the neighboring Battle Mountain-Eureka trend to the southwest.