Lead, zinc, and silver deposits at Bowser Creek, McGrath A-2 quadrangle, Alaska

Circular ◽  
1968 ◽  
Author(s):  
Bruce L. Reed ◽  
R.L. Elliott
Keyword(s):  
Silver Deposits ◽  
Lead Zinc

Chapter 27 Lead–zinc–silver deposits of Myanmar

2017 ◽  
Vol 48 (1) ◽  
pp. 589-623 ◽  
Author(s):  
Than Htun ◽  
Aung Kyin ◽  
Khin Zaw
Keyword(s):  
Silver Deposits ◽  
Lead Zinc

Mineral Deposits of Myanmar (Burma)

10.5382/gb.62 ◽  
2021 ◽  
Author(s):  
Laurence Robb ◽  
Andrew Mitchell
Keyword(s):  
Massive Sulfide ◽  
Gold Deposits ◽  
Late Triassic ◽  
Mineral Deposits ◽  
Magmatic Arc ◽  
Silver Deposits ◽  
Copper Gold ◽  
Lead Zinc ◽  
Lead Nickel ◽  
Complex Geology

Myanmar is richly endowed in natural resources that include tin, tungsten, copper, gold, zinc, lead, nickel, and silver, as well as gemstones. The material covered over a nine-day field trip explores the country’s complex geology, which reflects a collisional history stretching from the Late Triassic to at least Miocene, sited at the eastern end of the India-Asia suture. The country can be divided into three principal metallotects: the Wuntho-Popa magmatic arc, with granites and associated porphyry-type and epithermal Cu-Au mineralization; the Slate Belt (also called the Mogok-Mandalay-Mergui Belt), with multiple precollisional I-type and postcollisional S-type crustal melt granites that host significant tin-tungsten mineralization, and which also are host to a number of orogenic gold deposits; and the Shan Plateau with massive sulfide-type and also MVT-style lead-zinc-silver deposits.

scholarly journals Microbes, organic matter and ore deposits

2004 ◽  
Vol 25 (1) ◽  
pp. 36 ◽  
Author(s):  
Craig P Marshall ◽  
Karen L Mackenzie ◽  
Junhong Chen ◽  
Dorothy Z Oehler ◽  
Graham A Logan ◽  
...  
Keyword(s):  
Organic Matter ◽  
Northern Territory ◽  
Ore Deposits ◽  
Silver Deposits ◽  
The World ◽  
Lead Zinc

The 1640 Ma (million years old) Here?s Your Chance (HYC) deposit at McArthur River, Northern Territory, Australia is one of the largest and least metamorphosed lead-zinc-silver deposits in the world. The mineralised interval has been divided into several orebodies and is separated by relatively barren sediment.

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