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SEG 45 Final_qx4 - Society of Economic Geologists

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18 <strong>SEG</strong> NEWSLETTER No 55 • OCTOBER 2003<br />

... from 17<br />

Tectonics and Metallogeny in China: The IGCP Field Trip and Symposium (Continued)<br />

<strong>SEG</strong> NEWS<br />

belt <strong>of</strong> Devonian rocks. Controversy at<br />

both deposits included whether these<br />

were indeed VMS systems, or perhaps a<br />

manto-like and skarn deposit, respectively.<br />

However, as the trip moved to<br />

the northwest, continuing within the<br />

Devonian rocks, there was little doubt<br />

that the Ashele copper deposit was a<br />

significant VMS orebody hosted by<br />

mafic volcanic rocks. The deposit, discovered<br />

in 1984, contains 900,000 t Cu<br />

(@2.3% Cu) and 400,000 t Zn (@2.7%<br />

Zn), with significant gold and silver. A<br />

large underground mining operation<br />

should begin by next year at Ashele.<br />

Two orogenic gold deposits, Saidu<br />

and Duolanasayi) were also visited<br />

within the more western part <strong>of</strong> the<br />

southern Altay. These deposits <strong>of</strong> probable<br />

late Paleozoic age are presently each<br />

recognized as containing perhaps<br />

200,000 to 300,000 oz Au and are yielding<br />

a few thousand ounces <strong>of</strong> gold each<br />

year. However, additional resource<br />

potential may exist in the deposits and<br />

in surrounding areas. In fact, gold<br />

placer workings from the 1970s and<br />

1980s are found along many <strong>of</strong> the<br />

rivers in the southern Altay. From the<br />

southwestern Altay, a lengthy two-day<br />

journey across the western Junggar<br />

basin took most participants to the<br />

western Tianshan and a visit to the 50-t<br />

Au Axi gold deposit, the largest gold<br />

deposit in northwestern China and the<br />

8 th largest gold producer in China.<br />

These Early Carboniferous low-sulfidation<br />

epithermal veins and breccias have<br />

been yielding about 40,000 oz Au/year<br />

since mine start-up in 1995. Although<br />

not visited, smaller high sulfidation<br />

epithermal gold deposits are scattered<br />

elsewhere in this region.<br />

This field symposium was collectively<br />

recognized as a successful and productive<br />

program by all attendees, in large<br />

part due to the outstanding organization<br />

by Mao Jingwen from the Chinese<br />

Academy <strong>of</strong> Geological Sciences, many<br />

<strong>of</strong> Dr. Mao’s colleagues at the academy,<br />

and their collaborators from the<br />

Xinjiang Bureau <strong>of</strong> Geology,<br />

Exploration, and Development. Visits to<br />

outstanding geological exposures and<br />

ores in this frontier region <strong>of</strong> China,<br />

were mixed with wonderful cultural<br />

experiences that included dances with<br />

the colorful local Uighur people, sampling<br />

<strong>of</strong> the varied local cuisine and<br />

brands <strong>of</strong> Maotai, and a trip to Kanas<br />

National Park centered around China’s<br />

deepest glacial lake. Much <strong>of</strong> our present<br />

understanding <strong>of</strong> the economic<br />

geology <strong>of</strong> this prospective region is<br />

detailed in a new book published for<br />

the symposium on “Tectonic Evolution<br />

and Metallogeny <strong>of</strong> the Chinese Altay<br />

and Tianshan” (Mao, Goldfarb,<br />

Seltmann, Wang, Xiao, and Hart, eds.,<br />

2003, IAGOD Guidebook Series v. 10,<br />

282 p.). The book is available from CER-<br />

CAMS at the National History Museum<br />

in London (R.Seltmann@nhm.ac.uk).1<br />

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