Metallogenesis and Tectonics of the Russian Far East, Alaska, and ...
Metallogenesis and Tectonics of the Russian Far East, Alaska, and ...
Metallogenesis and Tectonics of the Russian Far East, Alaska, and ...
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Clark Range Metallogenic Belt ........................................................................................... 24<br />
Cambrian through Silurian Metallogenic Belts (570 to 408 Ma) ................................................................................................................. 24<br />
Overview ................... . ........................................................................................................................................................................ 24<br />
Metallogenic Belts Formed During Early Paleozoic Marine Sedimentation in Rifted Fragments <strong>of</strong> Gondw<strong>and</strong>al<strong>and</strong> Supercontinent .. 24<br />
Voznesenka Metallogenic Belt <strong>of</strong> Korean Pb-Zn Deposits (Belt VZ) Sou<strong>the</strong>rn <strong>Russian</strong> Sou<strong>the</strong>ast .................................................. 24<br />
Voznesenka-I Korean Pb-Zn Dcposit ............................................................................................................................................ 25<br />
Chemyshevskoe Korean Pb-Zn Deposit .................................................................................................................................... 25<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Voznesenka Metatlogenic Belt ......................................................................................... 26<br />
Kabarga Metallogenic Belt <strong>of</strong> Ironstone Superior Fe) Deposits (Belt KB) Sou<strong>the</strong>rn <strong>Russian</strong> Sou<strong>the</strong>ast ........................................... 26<br />
Metallogenic Belts Formed During Early Paleozoic Sedimentation or Marine Volcanism in Manchurid or Altaid Orogenic Systems26<br />
South Khingan Metallogenic Belt <strong>of</strong> Ironstone (Superior Fe) Dcposits (Bclt SK) Sou<strong>the</strong>rn <strong>Russian</strong> Sou<strong>the</strong>ast ............................... 26<br />
Gar Metallogenic Belts <strong>of</strong> Volcanogenic Fe Deposits <strong>and</strong> Stratiform Cu <strong>and</strong> Pb-Zn Deposits (Belt GR) Western Part <strong>of</strong><br />
<strong>Russian</strong> Sou<strong>the</strong>ast .......................................................................................................................................................................... 27<br />
Gar Volcanogenic Fe Deposit ....................................................................................................................................................... 27<br />
Kamenushinskoe Cu Massive Sulfide Deposit .............................................................................................................................. 27<br />
Chagoyan Stratiform Pb-Zn Deposit ............................................................................................................................................. 28<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Gar Metallogenic Belts ....................................................................................................... 28<br />
Metallogenic Belts Formed During Early Paleozoic Sea-Floor Spreading, Regional Metamorphism, or During Subduction-<br />
Related Volcanism in <strong>Russian</strong> <strong>Far</strong> <strong>East</strong> Terranes .............................................................................................................................. 28<br />
Galam Metallogenic Belt <strong>of</strong> Volcanogenic Fe, Volcanogenic Mn, <strong>and</strong> Sedimentary P Deposits (Belt GL) Central Part <strong>of</strong><br />
<strong>Russian</strong> <strong>Far</strong> <strong>East</strong> ............................................................................................................................................................................. 28<br />
Gerbikanskoe Volcanogenic Fe Deposit ....................................................................................................................................... 28<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Galam Metallogenic Belt .................................................................................................... 29<br />
Omulevka River Metallogenic Belt <strong>of</strong> Austrian Alps W <strong>and</strong> Kipushi Cu-Pb-Zn Deposits (Belt OR) Northwest Part <strong>of</strong> <strong>Russian</strong><br />
Nor<strong>the</strong>ast .............................................................................................................................................................................................. 29<br />
Omulev Austrian Alps W Deposit ................................................................................................................................................. 30<br />
Vesnovka Kipushi Cu-Pb-Zn Deposit ........................................................................................................................................... 30<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Omulevka River Metallogenic Belt ..................................................................................... 31<br />
Rassokha Metallogenic Belt <strong>of</strong> Basaltic Cu <strong>and</strong> Sediment-Hosted Cu Deposits (Belt RA) Nor<strong>the</strong>rn Part <strong>of</strong> <strong>Russian</strong> Nor<strong>the</strong>ast ....... 31<br />
Agyndja Basaltic Cu <strong>and</strong> Sediment-Hosted Cu Deposit .......................................................................................................... 31<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Rassokha Metallogenic Belt ................................................................................................ 31<br />
Metallogenic Belts Formed During Early Paleozoic Rifting <strong>of</strong> Continental Margins or in Continental-Margin Arc Terranes ............. 32<br />
Dzhardzhan River Metallogenic Belt <strong>of</strong> Sou<strong>the</strong>ast Missouri Pb-Zn, Sediment-Hosted Cu <strong>and</strong> S<strong>and</strong>stone-Hosted U deposits<br />
(Belt DZ) Nor<strong>the</strong>rn Part <strong>of</strong> <strong>East</strong>ern Siberia ................................................................................................................................... 32<br />
Manganiler Sou<strong>the</strong>ast Missouri Pb-Zn <strong>and</strong> Deposit ................................................................................................................... 32<br />
Kyongdyoi S<strong>and</strong>stone-Hosted U Deposit ..................................................................................................................................... 32<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Dzhardzhan River metall lo genic Belt .................................................................................. 32<br />
Anvil Metallogenic Belt <strong>of</strong> SEDEX (SEDEX) Zn-Pb-Ag Deposits, Yukon Territory, Canada (Belt AN) ........................................ 33<br />
Anvil District SEDEX Zn-Pb-Ag Deposits .................................................................................................................................. 33<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Anvil Metallogenic Belt ...................................................................................................... 33<br />
Howards Pass Metallogenic Belt <strong>of</strong> Sedimentary Exhalative Zn-Pb Deposits (Belt HP) <strong>East</strong>ern Yukon Territory .......................... 33<br />
Howards Pass (XY) Zn- Pb SEDEX Deposit .................... . .................................................................................................... 34<br />
Anniv (OP) SEDEX Zn- Pb Deposit ........................... . ........................................................................................................... 34<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Setting for Howards Pass Mctallogenic Belt ........................................................................................... 35<br />
Kootenay Metallogenic Belt <strong>of</strong> Carbonate <strong>of</strong> Sediment-Hosted Dcposits (Belt KO) Sou<strong>the</strong>rn British Columbia ............................. 35<br />
Jersey SEDEX Pb-Zn Deposit ....................................................................................................................................................... 36<br />
H.B. (Zincton) Pb-Zn SEDEX Deposit ......................................................................................................................................... 36<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Setting for Kootenay Metallogenic Belt .................................................................................................. 36<br />
Prince <strong>of</strong> Wales Isl<strong>and</strong> Metallogenic Belt <strong>of</strong> Continental-Margin Arc-Related Deposits (Belt PW) Sou<strong>the</strong>astern <strong>Alaska</strong> ................ 36<br />
McLean Arm Porphyry Cu-Mo District ........................................................................................................................................ 37<br />
Polymetallic Vein, Skam, <strong>and</strong> Disseminated Deposits in Paleozoic Plutons at Klakas Inlet <strong>and</strong> Kassan Peninsula ................... 37<br />
Salt Chuck Zoned Mafic-Ultramatic Cu-Au-PGE Deposit .......................................................................................................... 37<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Prince <strong>of</strong> Wales Isl<strong>and</strong> Metallogenic Belt ........................................................................... 40<br />
Middle <strong>and</strong> Late Devonian Metallogenic Belts (387 to 360 Ma; Figures 16. 17) .................................................................................... 40<br />
Overview .................................................................................................................................................................................................. 40<br />
Metallogenic-Tectonic Model for Middle through Late Devonian (387 to 360 Ma; Figure 18) ........................................................... 40<br />
Specific Events for Middle Through Late Devonian .......................................................................................................................... 41<br />
Metallogenic Belt Formed During Collision ............................................................................................................................................ 45<br />
Yaroslavka Metallogenic Belt <strong>of</strong> Fluorite <strong>and</strong> Sn Greisen Deposits (Belt YA) Sou<strong>the</strong>rn Part <strong>of</strong> <strong>Russian</strong> Sou<strong>the</strong>ast ........................ 45<br />
Voznesenka-11 Fluorite Greisen Deposit ....................................................................................................................................... 45<br />
Yaroslavka Sn Greisen Deposit ..................................................................................................................................................... 46<br />
Origin <strong>of</strong> <strong>and</strong> Tectonic Controls for Yaroslavka Mctallogenic Belt ............................................................................................. 47<br />
Metallogenic Belts Formed in a Middle Paleozoic Continental Arc Along North Asian <strong>and</strong> North American Craton Margins ........... 47
Change language