%0 Journal Article
%T MIOCENE FORAMINIFERA OF TARIM BASIN, XINJIANG AND THEIR GEOLOGICAL SIGNIFICANCE<br>新疆塔里木盆地中新世有孔虫及其地质意义
%A HAO Yi-chun
%A ZENG Xue-lu
%A QIU Song-yu
%A HE Xi-xian
%A <br>郝诒纯
%A 曾学鲁
%A 裘松余
%A 何希贤
%J 地球学报
%D 1982
%I 
%X The miocene beds in Tarim Basin are characterized by variegated clasticdeposits comprising mainly sandstone, siltstone, arenaceous mudstone and mu-dstone with intercalations of gypsum and occasionally of conglomeratic beds.The whole sequence is predominated by dark brownish, brownish, reddish andyellowish strata intercalated with subordinate dark grey, grey and greyishgreen beds. Gypsum deposits are better developed in the middle and lowerparts.
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=1DF69A47DE80569EC8F859DF61571180&aid=8A5BBB6F6CE57A269A8B045ECF71D16E&yid=3F3D540C9B7906DE&vid=E158A972A605785F&iid=CA4FD0336C81A37A&sid=CB423C9A71560A74&eid=0D0D661F0B316AD5&journal_id=1006-3021&journal_name=地球学报&referenced_num=0&reference_num=0