%0 Journal Article
%T LEAD ISOTOPIC COMPOSITIONS OF NATIVE SULFUR CHIMNEYS FROM NEARBY KUEISHANTAO ISLAND IN NORTHEAST OF TAIWAN AND ITS GEOLOGICAL IMPLICATIONS<br>台湾东北部龟山岛附近海域自然硫烟囱体的铅同位素组成及地质意义
%A LIU Chang-Hu
%A WANG Xiao-Mei
%A ZENG Zhi-Gang
%A JIANG Xue-Jun
%A YIN Xue-Bo
%A CHEN Chen-tung A
%A <br>刘长华
%A 汪小妹
%A 曾志刚
%A 姜学均
%A 殷学博
%A 陈镇东
%J 海洋与湖沼
%D 2009
%I 
%X For determining the origin of the hydrothermal native sulfur chimney nearby Kueishantao Island, off the northeast Taiwan, geochemistry of lead isotope of native sulfur in the chimneys was studied. The result indicates that the lead isotopic composition is very homogeneous, indicative of a small field of the origin. However, the source of lead is different from those in deeper hydrothermal deposits. Moreover, the lead isotopic scope does not match with the Northern Hemisphere lead isotopic reference line (NHRL). Although the native sulfur chimney was from seawater, the seawater did not contribute the lead isotopics to the chimney-bearing lead but the continental crust did. Therefore, the continental crust beneath the island must have played an important role in material transfer and exchange during the formation of the chimney in the past geological history, which bears implication for understanding the regional complex geological structure and tectonic evolution.
%K Lead isotopic composition
%K Native sulfur chimney
%K Seafloor hydrothermal activity
%K Kueishantao Island<br>铅同位素组成
%K 自然硫烟囱体
%K 海底热液活动
%K 龟山岛
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=2D9C75573FA3E416&jid=10F18692CD69EACA2DF7FC109993D35C&aid=1A95663E4E163731FF9133383D6598CD&yid=DE12191FBD62783C&vid=1371F55DA51B6E64&iid=E158A972A605785F&sid=23F20F9780C3579E&eid=87545994EC2C1F12&journal_id=0029-814X&journal_name=海洋与湖沼&referenced_num=0&reference_num=29