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 ...
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TABLE 2. Summary <strong>of</strong> correlations <strong>and</strong> tectonic linkages for <strong>the</strong> Circum-North Pacific - Continued.<br />
Unit(s) <strong>and</strong> Correlations.<br />
Tectonic Environment(s) Tectonic Linkages.<br />
Age<br />
Comments<br />
MAINLY TRIASSIC TO MID-CRETACEOUS ISLAND-ARC AND CONTINENTAL-MARGIN-ARC TERRANES<br />
AND OVERLAP ASSEMBLAGES, AND LINKED SUBDUCTION-ZONE TERRANES<br />
Monakin Continental-margin Arc<br />
Monakin volcanic-pluotnic belt, granitic<br />
plutonic rocks <strong>of</strong> Korea, <strong>and</strong> volcanicplutonic<br />
belt <strong>of</strong> Sou<strong>the</strong>ast China.<br />
Jurassic.<br />
Badzhal, Khabarovsk, <strong>and</strong> Samarka terranes.<br />
(Also Taukha, <strong>and</strong> Oshima terranes)<br />
Paleozoic to Cretaceous.<br />
Urnlekan-Ogodzhin volcanic-plutonic belt.<br />
Jurassic <strong>and</strong> Earlv Cretaceous<br />
Badzhal, Khabarovsk (older Jurassic part), <strong>and</strong><br />
Samarka terranes.<br />
Paleozoic to Cretaceous.<br />
Khingan continental-margin arc<br />
Khingan-Okhotsk volcanic-plutonic belt.<br />
Early <strong>and</strong> mid-Cretaceous.<br />
Amur River, Khabarovsk, <strong>and</strong> Kiselevka-<br />
Manoma terranes.<br />
Jurassic <strong>and</strong> Early Cretaceous.<br />
Kema terrane, <strong>and</strong> Early to mid-Cretaceous<br />
volcanic rocks <strong>of</strong> Hokkaido Isl<strong>and</strong>.<br />
Mid Cretaceous.<br />
Aniva <strong>and</strong> Kamuikotan terranes.<br />
Cretaceous.<br />
Igneous overlap assemblage.<br />
Discontinuous parts <strong>of</strong> Great Hinggan<br />
arc.<br />
Accretionary wedge. Linked to Monakin continental-margin<br />
arc. Also linked to Umlekan arc<br />
(below). Remnants <strong>of</strong> subduction <strong>of</strong><br />
Ancestral Pacific Ocean plate.<br />
Taukha, <strong>and</strong> Oshima terranes linked<br />
to coeval granitic plutonic rocks <strong>of</strong><br />
Korea <strong>and</strong> volcanic-plutonic belt <strong>of</strong><br />
sou<strong>the</strong>ast China.<br />
Umlekan Continental-Margin Arc<br />
Igneous overlap assemblage.<br />
Accretionary wedge.<br />
Continental-margin arc.<br />
Accretionary wedge.<br />
Kema Continental-Margin Arc<br />
Igneous overlap assemblage.<br />
Transpressional subduction zone.<br />
Nor<strong>the</strong>rn extension <strong>of</strong> Monakin arc.<br />
Linked to Umelkan arc <strong>and</strong> to Monakin<br />
arc (above). Remnants <strong>of</strong> subduction<br />
<strong>of</strong> Ancestral Pacific Ocean plate.<br />
Formed after collision <strong>of</strong> Anui<br />
microcontinent with Samarka terrane<br />
Linked to Khingan continental-margin<br />
arc. Remnants <strong>of</strong> oblique subduction<br />
<strong>of</strong> Ancestral Pacific Ocean plate.<br />
Transpressive continental-margin arc<br />
analogus to Tertiary margin <strong>of</strong><br />
California.<br />
Linked to Kema arc. Remnants <strong>of</strong><br />
subduction <strong>of</strong> Ancestral Pacific<br />
Uda volcanic-plutonic belt, Uniya-Bom<br />
Uda Continental-Margin Arc<br />
I Igneous overlap assemblage. Deposited on <strong>and</strong> adjacent to, <strong>and</strong><br />
turbidite-basin terrane, Umlekan-Ogodzhin<br />
intruded into <strong>the</strong> North Asian Craton<br />
volcanic-plutonic belt, <strong>and</strong> Upper Amur<br />
<strong>and</strong> Stanovoy block <strong>of</strong> <strong>the</strong> North<br />
sedimentary assemblage.<br />
Late Jurassic <strong>and</strong> Earlv Cretaceous.<br />
Asian Craton.<br />
Turkuringra- Dzhagdi, Galam, <strong>and</strong> Ulban Subduction zone or accretionary Linked to Uda arc. Remnants <strong>of</strong><br />
terranes.<br />
wedge.<br />
subduction <strong>of</strong> Mongol-Okhotsk<br />
Jurassic <strong>and</strong> Cretaceous.<br />
Kony-Murgal Isl<strong>and</strong> Arc<br />
Ocean plate.<br />
Kony-Murgal terrane.<br />
Continental-margin <strong>and</strong> isl<strong>and</strong><br />
Late Triassic to Early Cretaceous.<br />
arc.<br />
Talovskiy <strong>and</strong> Penzhina-Anadyr terranes. Subduction zone <strong>and</strong> accretionary Linked to Kony-Murgal arc. Remnants<br />
Mainly Jurassic <strong>and</strong> Early Cretaceous.<br />
wedge.<br />
I<br />
<strong>of</strong> subduction <strong>of</strong> Ancestral Pacific<br />
Ocean plate.<br />
West Pekul'ney terrane.<br />
Pekul'ney isl<strong>and</strong> arc<br />
I Isl<strong>and</strong> arc.<br />
Late Triassic to Early Cretaceous.<br />
Pekul'ney terrane. I Subduction zone. I Linked to Pekul'ney arc. Remnants <strong>of</strong><br />
Mainly Jurassic <strong>and</strong> Early Cretaceous. subduction <strong>of</strong> Ancestral Pacific<br />
Ocean plate.
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