The auriferous gravel deposit of Gold Bluffs [Klamath County, California]
نویسندگان
چکیده
منابع مشابه
Geochemistry of pyrite and whole rock samples from the Getchell Carlinâ•fitype gold deposit, Humboldt County, Nevada
متن کامل
Postglacial vegetation and fire history, eastern Klamath Mountains, California, USA
Pollen and high-resolution charcoal data from Bluff Lake and Crater Lake, California, indicate similar changes in climate, vegetation and fire history during the last 15 500 years. Pollen data at Bluff Lake suggest that the vegetation between c. 15 500 and 13 100 cal. BP consisted of subalpine parkland with scattered Pinus and Abies. After 13 100 cal. BP a relatively closed forest of P. montico...
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The Chah-Bagh gold occurrence is located in Muteh mining district, in the central part of the Sanandaj-Sirjan zone. Gold mineralization occurs in ductile to ductile-brittle shear zones and is comparable with orogenic gold deposits. Silicification and sulfidization are the most important hydrothermal alteration features in the inner parts of altered shear zones and coincide most closely with the...
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The term "Carlin-type" deposit has been applied to a number of low-grade, sedimentary rock-hosted gold deposits that have been discovered and brought into production in the western United States since the 1960s. Carlin-type deposits are characterized by replacement of carbonate and silty carbonate rocks by silica, pyrite, barite, various arsenic, mercury, antimony, and thallium minerals and by ...
متن کاملGeochemical Exploration of the Tareek Darreh Gold Deposit, North of Torbat-e Jaam, East Iran
The Tareek Darreh gold deposit is located 40km north of Torbat-e Jaam in the Khorassan-Razavi province, NE-Iran. The study area mainly comprises slightly metamorphosed, sedimentary rocks of Jurassic age including alternation of shale, siltstone, and sandstone. These rocks have been intruded by plutonic rocks such as gabbro-norite, diorite, quartz-diorite, and rhyodacite. The ore bodes are expos...
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ژورنال
عنوان ژورنال: American Journal of Science
سال: 1874
ISSN: 0002-9599
DOI: 10.2475/ajs.s3-7.40.379