n Alas - Alaska Division of Geological & Geophysical Surveys - State ...
n Alas - Alaska Division of Geological & Geophysical Surveys - State ...
n Alas - Alaska Division of Geological & Geophysical Surveys - State ...
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
THE UNITED STATES GEOLOGICAL SURVEY IN ALASKA:<br />
This report <strong>of</strong> .accomplhhments <strong>of</strong> the U.S. Geo-<br />
logical Survey in <strong>Alas</strong>ka during I981 mtalns summary<br />
and topical accounts <strong>of</strong> the results <strong>of</strong> studies on a wide<br />
range <strong>of</strong> topics <strong>of</strong> economic and scientific interest. In<br />
addition, many more detailed maps and reports are In-<br />
cluded in the lists <strong>of</strong> references cited for each article<br />
and in the appended compilations <strong>of</strong> 277 reports on Ai-<br />
aska published by the U.S. <strong>Geological</strong> Survey and <strong>of</strong><br />
103 reports by U.S. <strong>Geological</strong> Survey authors in<br />
various other scientific publications.<br />
Rre U.S. <strong>Geological</strong> Survey is engaged in many<br />
scientific investigations on various aspects <strong>of</strong> the land<br />
and water in <strong>Alas</strong>ka. Pmlucts <strong>of</strong> the Surveyt investl-<br />
gations include reports describing the phydcal findings<br />
and their significance. This volume includes summmy<br />
discussions, topid rcwults, and some nerratives <strong>of</strong> the<br />
course <strong>of</strong> the studles on just a few <strong>of</strong> the various<br />
Earth-science subjects currently being Investigated in<br />
<strong>Alas</strong>ka. POT the reader's convenience h peruslng<br />
reports that cover specific areas <strong>of</strong> interest, the<br />
articles are grouped by areas corresponding to the SIX<br />
regional geographic onshore subdivisions shown in fig-<br />
ure 1, by <strong>of</strong>fshore average, and by those article that<br />
cover more than one geographical region or are <strong>State</strong>-<br />
wide in scope. Index maps showing the study areas or<br />
sites discussed are Lncluded near the beginning <strong>of</strong> each<br />
subdivision (figs. 1, 5, 13, 19, 23, 44, 72, 90). An<br />
author index at the back <strong>of</strong> the volume should amkt in<br />
identifying and locating work by specific authors<br />
reported herein or in the appended compilations <strong>of</strong><br />
current reports on <strong>Alas</strong>ka by U.S. <strong>Geological</strong> Survey<br />
authors and their associates.<br />
(Ffgure 1 shows the quadrangles and regions<br />
referred to in this volume)<br />
ACCOMPLlSHMENTS DURING 1981<br />
Warren L. Coonrad and Raymond 1. Elliott, Editors<br />
rangles (fig. 2) have been completed. These maps are<br />
the major summary prdcts <strong>of</strong> the U.S. Geologlcal<br />
Survey's Branch <strong>of</strong> <strong>Alas</strong>kan Geology's telegeologlc<br />
research effort, funded under the auspices <strong>of</strong> the <strong>Alas</strong>-<br />
kan Mineral Resource Assessment Program. Synthesfs<br />
<strong>of</strong> the data compiled from these studies indicates that<br />
the major features oommonly observable on Landsat<br />
images <strong>of</strong> <strong>Alas</strong>ka are lineaments, circular and arcuate<br />
features, and anomalously colored areas.<br />
Lineaments<br />
Lineaments observed in <strong>Alas</strong>ka can gener* be<br />
divided into three groups on the basis <strong>of</strong> scale: (1)<br />
<strong>State</strong>wide Uneament trends (northwest, north-south,<br />
northeast, and east-west; see Lathram and molds,<br />
1977), corresponding to the regmatic shear pattern,<br />
that not only transect tectonic and stratigraphic<br />
boundaties but also coincide with these boundaries in<br />
places; (2) regional trends, such as for the set <strong>of</strong> lin-<br />
eaments along the DenaU fault in the Talkeetna quad-<br />
rangle (Steele land Albert, 1978a) or along the Coast<br />
Range megallneament in the Ke tchikan quadrangle;<br />
and (3) local trends that ere commonly restricted to<br />
specific terranes and various geologic phenomena, or<br />
to structures caused by unknown (local) tectonlo<br />
events.<br />
That many lineaments (generally from several<br />
Wlorneters to several tens <strong>of</strong> kllometers long) which<br />
make up sets <strong>of</strong> subparallel to parellel Uneaments<br />
detected on Landset images may reflect relatively<br />
narrow (generay less than 10 krn wide) zones <strong>of</strong><br />
associated(?) fractures is particularly well shown in<br />
the Ketch- quadrangle (Steele and Albert, 1978b;<br />
Le Compte, 1981b). Only a few (1-10 percent) <strong>of</strong> the<br />
Uneaments there are faults, although many faults that<br />
are mappable at 1:250,000 scale can be detected on<br />
Landsat images. Lineament extensions beyond the<br />
terminations <strong>of</strong> the many faults mapped by field<br />
methods are also evident in places.<br />
Circular and Arcuate Features<br />
8nmlwrgat~t~e~~~lnAlngkn Circular and arcuate features detected on Land-<br />
sat Images <strong>of</strong> <strong>Alas</strong>ka can generally be divided into two<br />
BY Jam- R CMnpte, Willhrn Cltntaa b ebi and goups. The first group consists <strong>of</strong> circular and arcu-<br />
lUairnRD.Albeet ate features larger than 50 km in diameter, such as<br />
several circular features Ln the eastern Brooks hnge<br />
Landsat-image interpretation and (or) Landsat- (Le Compte, 1970a); few logical explanations have<br />
feature map for 27 Aleakan 1:250,000-scale quad- been found for features this Large. The second group