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Mountain ophfolite, Oregon: Arnerloan Journal<br />

& .<br />

<strong>of</strong> Science, v. 280-A, pr. I, p. 232-288.<br />

Loney, R. A., Himmelberg, G. R., and Coleman, lL G.,<br />

1971, Structure and petrology <strong>of</strong> the alpine-type<br />

peridotite at Burro Mountain, California,<br />

U.S.A.: Journal <strong>of</strong> Petrology, v. 12, no. 2, p.<br />

245-309.<br />

Patton, W. W., Jr., 1978, red continental and<br />

oceanic-island are t n the Medfra quad-<br />

rangle, r west-central <strong>Alas</strong>ka, & Johnson, K.<br />

ed-- --., The ... 2 United <strong>State</strong>s <strong>Geological</strong> Survey<br />

Aleska: Accomplishments during 1971: U.S.<br />

<strong>Geological</strong> Survey Circular 772-B, p. B38-839.<br />

Pat to In, W. W., Jt., Tailleur, I. L., Brosg6,W. P., and<br />

Lanphere, M. A., 1977, Preliminary report on the<br />

ophiolite s <strong>of</strong> nor thern and western <strong>Alas</strong>ka, &<br />

Coleman , R. G. and Irwin, W. P., eds., North<br />

America1 n ophioli tes: Oregon Department <strong>of</strong><br />

156'30' 156'00'<br />

EXPLANATION<br />

=<br />

[I SSuIcial deposits (baremary)<br />

Sedlmnlary rocks (Cretaceous)-<br />

.(ng!omerate. un&+ono, mc~<br />

slllslone<br />

Pwidollte, undividsd (Juras!<br />

I<br />

L_1 Harzburgite tectonite<br />

J p c Cumulate ultmmf~c rocks<br />

I T ]<br />

Basall, gabbm, and cherl (Triassic<br />

to Mississippian)<br />

= pz$~ Schlsr and quanzlte (low Palmzoic<br />

and (or) hmmb"an)<br />

64O<br />

30' CCkR (Triassic to Mirsissb<br />

64'<br />

00'<br />

0<br />

10 20 30 KILOMETERS<br />

I . .<br />

1- MMab ( her Paleozoic and<br />

(or) Precambrian)<br />

Contact-Appmximatety localad<br />

- - Rulr-lntaned high angle<br />

r - r Thrust lavlt-Herred; datted<br />

where cmcealed<br />

Plgure 15.-Geologic map <strong>of</strong> southeastern part <strong>of</strong> Nulato quadrangle, <strong>Alas</strong>ka (from<br />

W. W. Pat ton, Jr., written commun. 1981).<br />

I

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