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Metallogenesis and Tectonics of the Russian Far East, Alaska, and ...

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Figure 49 Generaltzed map Of mbjm Lab &as$& b * * ~ ~ ( b r ~ t . d * c m ~ m - ~ a - ~ ~<br />

<strong>of</strong>hhon m. b m Ibr dac- d -. khptd mkldmrg <strong>and</strong> ahrS(MWb, W). Ww l*<br />

3 for explanation<br />

<strong>the</strong> Wrangellia isl<strong>and</strong>-arc supertem. 'I&k bdl is &*dd a h thp &&IU =-*.&* la<br />

<strong>the</strong> below descriptions <strong>of</strong> metallogsaio bdm, II hv d & a 6- kda (et%)m.M-M - .+- .,., bsh. .<br />

Metallogenic-Tectonic Model for<br />

Late Jurassic (163 to 144 Ma; Figur, !Bj<br />

hrbg <strong>the</strong> Latc Jarnssic (Oxfpr6r~ hhtoryb -; 1 E4 lo 1 4 e}, <strong>the</strong><br />

were (fig. 50; table 3): ( 1 ) ~ a f ~ c r C ~ ~ ~ ~ h N<br />

fomtion <strong>of</strong> associated mstrllogak kk wqmb -rrrw amd<br />

arc re3d assachd tmme.9 edo Lbe Nost4-h hhn B+#!u$ @ (3)<br />

obductbw <strong>of</strong> tbe ~ L - ~<br />

previous long-lid pcrmd (Late Pmteroeok hugb Early J d c ) ctfpoaaive sdmenMth on &c H&& A9ibsrdM<br />

American Cratons<br />

- -<br />

4 I<br />

Specific Events Lslr J u m<br />

Forming in <strong>the</strong> arc wem <strong>the</strong> T--M (TAM) klt <strong>of</strong> podlfm CT whU ie bid haone<br />

plutons, <strong>and</strong> <strong>the</strong> AaaiRif3 (MI beh afhnroko massive suW depab. Tbtl- Ihbd to UIC wadaccretionary-wedge<br />

tmme (AV) *& h t d km ruWucLim <strong>of</strong>paff <strong>of</strong>- mxuic<br />

t ':<br />

subduction zone m m ~w~ toward <strong>the</strong> Kcmy-Mu@ iald art.<br />

(2) The Modin rn (Madin vvl~ic-pblonic MI, nM) hnb <strong>the</strong> U&km arc ( U m B m - m V-W& .<br />

belt, uo <strong>and</strong> associated units) coslinud acdvicy. F a in Ihp mc mr t& No& Bmym (MI) rnehlbgmk Wt, w&& wmtisw<br />

subduction-related ~ c - depouil$. m A s w~ W ~f~ ~ <strong>of</strong>& ares w& &tbtW@fw bf.<br />

. .<br />

I ? . ..

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