Characteristics of Shizhuzi Complex in Kuandian, Eastern Liaoning and Its Metallogeny

• 责任者：Liu Xuewen (Liaoning Survey Academy of Geology and Mineral Resources ; Shenyang 110032 ; China) ; Hong Xiuwei
• 刊名：Jilin Geology
• 出版年：2010
• 卷期：29(2)
• 关键词：杂岩 ; complexes ; 成矿物质来源 ; source of ore material ; I型花岗岩 ; I-type granite ; 辽宁 ; Liaoning Province
• 页码：p.16-22
• 图表：11 illus., 1 table, 7 refs.
• 分类号：0801
• issnNo：ISSN1001-2427
• isbnNo：CN22-1099/P

Shizhuzi complex, which is situated in the contact zone between Jiao-Liao platform-uplift and platform-subsidence, is distributed at east area of Kuandian. Its isotope dating of zircon U-Pb is 129 Ma represented its intrusive age of Cretaceous in Mesozoic era. According to petrology and age, the Shizhuzi complex can be grouped into Dalazigou quartz diorite, Zhenjiang granodiorite, Chiyudingzi adamellite. This cell is belonged to the calc-alkaline series and I-type granite. The evolution trend of magma is obviously completed evolution series. The diagenesis environment of tectonics is in mobile belt of continent edge.