Data used to prepare a map showing the location of significant gold mines in Montana

1990 ◽  
Author(s):  
David Frishman ◽  
J.E. Elliott ◽  
E.E. Foord ◽  
Robert C. Pearson ◽  
W.H. Raymond
Keyword(s):  
Gold Mines

Ultrastructural Changes in Patients With Heat Stroke

1970 ◽  
Vol 28 ◽  
pp. 210-211
Author(s):  
O. T. Minick ◽  
M. C. Kew
Keyword(s):  
Liver Damage ◽  
Heat Stroke ◽  
Free State ◽  
Ultrastructural Changes ◽  
Gold Mines

The effects of heat stroke on hepatic structure were studied in 32 Bantu patients who worked underground in the Transvaal and Orange Free State Gold Mines.Judging from biochemical and morphologic findings, liver damage is an invariable complication of heat stroke. In the milder cases (90 per cent) raised enzyme levels, bromsulphalein retention, and increased prothrombin times were the most common abnormalities.

Information gold mines

2008 ◽  
Author(s):  
Tori DeAngelis
Keyword(s):  
Gold Mines

The Gold Mines of West Africa

1899 ◽  
Vol 47 (1212supp) ◽  
pp. 19424-19425
Author(s):  
James Irvine
Keyword(s):  
West Africa ◽  
Gold Mines

Điều kiện địa động lực hình thành các mỏ vàng khu vực Miền Trung và Tây Nguyên

2003 ◽  
Vol 25 (3) ◽  
pp. 233-242
Author(s):  
Nguyễn Viết Ý ◽  
Trần Trọng Hòa ◽  
Ngô Thị Phượng ◽  
Trần Tuấn Anh ◽  
Vũ Văn Vấn ◽  
...  
Keyword(s):  
Gold Mines

Geodynamics of the formation of gold mines in the Central part and Tay Nguyen areas, Vietnam

A structural reappraisal of the Beardmore–Geraldton Belt at the southern boundary of the Wabigoon subprovince, Ontario, and implications for gold mineralization

2004 ◽  
Vol 41 (2) ◽  
pp. 217-235 ◽  
Author(s):  
Bruno Lafrance ◽  
Jerry C DeWolfe ◽  
Greg M Stott
Keyword(s):  
Gold Mineralization ◽  
Shear Zones ◽  
Axial Plane ◽  
Superior Province ◽  
Southern Boundary ◽  
Gold Mines ◽  
Southern Margin ◽  
Ore Zones

The Beardmore–Geraldton Belt occurs along the southern margin of the Archean Wabigoon subprovince, Superior Province, Ontario. The belt consists of shear-bounded interleaved metasedimentary and metavolcanic units. The units were imbricated from 2696 to 2691 Ma during D1 thrusting and accretion of the Wabigoon, Quetico, and Wawa subprovinces. Post-accretion D2 deformation produced regional F2 folds that transposed lithological units parallel to the axial plane S2 cleavage of the folds. During D3 deformation, the folds were overprinted by a regional S3 cleavage oriented anticlockwise of F2 axial planes, and lithological contacts and S2 cleavage were reactivated as planes of shear within dextral regional shear zones that generally conform to the trend of the belt. D3 is a regional dextral transpression event that also affected the Quetico and Wawa subprovinces, south of the Beardmore–Geraldton Belt. Gold mineralization at the Leitch and MacLeod-Cockshutt mines, the two richest past-producing gold mines in the Beardmore–Geraldton Belt, is associated with D3 shear zones and folds, overprinting regional F2 folds. The plunge of the ore zones is parallel to F3 fold axes and to the intersection of D3 shear zones with F2 and F3 folds.

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