Fluorite Veins Near Meyers Cove, Lemhi County, Idaho PDF Download
Are you looking for read ebook online? Search for your book and save it on your Kindle device, PC, phones or tablets. Download Fluorite Veins Near Meyers Cove, Lemhi County, Idaho PDF full book. Access full book title Fluorite Veins Near Meyers Cove, Lemhi County, Idaho by United States. Bureau of Mines. Download full books in PDF and EPUB format.
Author: United States. Bureau of Mines
Publisher:
ISBN:
Category : Fluorspar
Languages : en
Pages : 7
Get Book Here
Book Description
Author: United States. Bureau of Mines
Publisher:
ISBN:
Category : Fluorspar
Languages : en
Pages : 7
Get Book Here
Book Description
Author: D. C. Cox
Publisher:
ISBN:
Category : Fluorspar
Languages : en
Pages : 384
Get Book Here
Book Description
The fluorspar deposits near Meyers Cove, Lemhi County, Idaho, are localized along three groups of shear zones: one group strikes northeast and dips steeply northwestward, another strikes northeast and dips gently northwestward, and the third strikes northwest and dips gently southwestward. The country rocks are tuffs and flows of the Casto volcanics of Permian (?) age and the Challis volcanics of late Oligocene or early Miocene age. The known deposits are in a belt about 3 miles long and 2 miles wide and crop out at altitudes between 5,100 feet and 7,200 feet above sea level. The principal vein minerals are fluorite, chalcedony, and barite. The fluorite occurs as lodes, crusts around fragments of rock, and replacements of fine breccia. The lodes range in size from veinlets to vein zones several hundred feet long and as much as 20 feet wide and contain ore that ranges in grade from 40 percent to 85 percent CaF2 ; the average grade is about 50 percent CaF2.
Author: D.C. Cox
Publisher: BiblioGov
ISBN: 9781289007232
Category :
Languages : en
Pages : 34
Get Book Here
Book Description
The fluorspar deposits near Meyers Cove, Lemhi County, Idaho, are localized along three groups of shear zones: one group strikes northeast and dips steeply northwestward, another strikes northeast and dips gently northwestward, and the third strikes northwest and dips gently southwestward. The country rocks are tuffs and flows of the Casto volcanics of Permian (?) age and the Challis volcanics of late Oligocene or early Miocene age. The known deposits are in a belt about 3 miles long and 2 miles wide and crop out at altitudes between 5,100 feet and 7,200 feet above sea level. The principal vein minerals are fluorite, chalcedony, and barite. The fluorite occurs as lodes, crusts around fragments of rock, and replacements of fine breccia. The lodes range in size from veinlets to vein zones several hundred feet long and as much as 20 feet wide and contain ore that ranges in grade from 40 percent to 85 percent CaF2; the average grade is about 50 percent CaF2.
Author: Doak C. Cox
Publisher:
ISBN:
Category :
Languages : en
Pages : 0
Get Book Here
Book Description
Author: D. C. Cox
Publisher:
ISBN:
Category :
Languages : en
Pages :
Get Book Here
Book Description
Author:
Publisher:
ISBN:
Category : Barite
Languages : en
Pages : 512
Get Book Here
Book Description
Prepared on behalf of the U.S. Atomic Energy Commission.
Author: United States. Bureau of Mines
Publisher:
ISBN:
Category : Mines and mineral resources
Languages : en
Pages : 502
Get Book Here
Book Description
Author: United States. Bureau of Mines
Publisher:
ISBN:
Category :
Languages : en
Pages : 444
Get Book Here
Book Description
Author: Basil G. Dean
Publisher:
ISBN:
Category : Barite
Languages : en
Pages : 54
Get Book Here
Book Description
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 350
Get Book Here
Book Description
