%0 Journal Article
%T THE GEOLOGICAL FEATURES AND ORIGIN OF THE BEILEKUDUK TIN METALLOGENIC BELT<br>贝勒库都克锡矿带地质特征与成因
%A BI Cheng-en
%A SHEN Xiang-yuan
%A XU Qing-sheng
%A MING Quan-hai
%A SUN Hui-li
%A ZHANG Chun-hai
%A <br>毕承思
%A 沈湘元
%A 徐庆生
%A 明奎海
%A 孙惠礼
%A 张春山
%J 地球学报
%D 1993
%I 
%X The Beilekuduk tin metallogenic belt is the first independent tin metallogenic belt discovered in northern China, in which there occur the Beilekuduk, Sareshik, Kamst and Ganliangzi tin deposits and several tin occurrences. It extends a NW direction in the Kalamaili deep fault. Tin-bearing granites are mainly represented by highly differentiated ultraacid and akalirich S-type biotie granite sotcks of Late Hercynian age, but the Sareshik tin deposit is an independent tin deposit related to Hercynian A-type granites discovered for the first time in China.
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=C6A21C25462903091E8244AC8133A8D2&yid=D418FDC97F7C2EBA&vid=F3583C8E78166B9E&iid=38B194292C032A66&sid=987EDA49D8A7A635&eid=5C3443B19473A746&journal_id=1006-3021&journal_name=地球学报&referenced_num=0&reference_num=0