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胶东夏甸金矿成矿期闪长玢岩脉锆石U-Pb年代学研究
引用本文:王硕,孙丰月,孙巍,奥琮,陈俊.胶东夏甸金矿成矿期闪长玢岩脉锆石U-Pb年代学研究[J].世界地质,2014,33(2):376-387.
作者姓名:王硕  孙丰月  孙巍  奥琮  陈俊
作者单位:1. 吉林大学 地球科学学院,长春 130061; 2. 吉林大学 古生物学与地层学研究中心,长春 130026
摘    要:山东夏甸金矿区内深源中—基性脉岩发育,其中以闪长玢岩与矿体间时空关系最为密切,被认为是幔源流体成矿最重要的判别标志。笔者通过对夏甸金矿两个不同中段内成矿期闪长玢岩LA-ICP-MS锆石U-Pb年代学研究,获得了4组较为一致的年龄,它们较为完整地保留了这一期中—基性岩浆活动留下的地质记录。这4组年龄分别为:①五台期:华北地区微陆块拼合,发生大规模岩浆作用,形成华北克拉通基底雏形;②印支期:华南与华北两大板块碰撞拼合,苏鲁—大别造山带出现,区内发生大规模变质作用;③燕山早期:受太平洋板块俯冲影响,太古宙绿岩体发生强烈改造,形成大面积重熔型花岗岩;④燕山晚期:成岩成矿期。

关 键 词:夏甸  闪长玢岩  锆石  U--Pb  年龄  地质记录

Zircon U--Pb age for dioritic porphyrite of Xiadian gold ore-deposit in Jiaodong region
WANG Shuo,SUN Feng-Yue,SUN Wei,AO Cong,CHEN Jun.Zircon U--Pb age for dioritic porphyrite of Xiadian gold ore-deposit in Jiaodong region[J].World Geology,2014,33(2):376-387.
Authors:WANG Shuo  SUN Feng-Yue  SUN Wei  AO Cong  CHEN Jun
Institution:1. College of Earth Sciences,Jilin University,Changchun 130061,China; 2. Research Center of Paleontology and Stratigraphy,Jilin University,Changchun 130026,China
Abstract:Intermediate-basic dikes in Xiadian gold field,particularly its diorite-porphyrite,showed close re- lationship to gold mineralization which has been regarded as the indicator for the mantle-derived fluid mineraliza- tion. LA-ICP-MS zircon U-Pb dating result from two ore-forming period diorte-porphyrite in different depths showed four groups of concordia age. They are records of the geological processes formed by magma transport. The four groups can be recognized as ① Wutai period - the NCC fundamentally amalgamated with large-scale thermal action. Initial ore source bed formed. ② Indosinian - the South China Craton subducted the North China Craton. Dabie- Sulu oregenic belt exposed and large scale metamorphization happened. ③ Early Yanshanian - the subduction of Pacific Plate leaded intensive modification of Archaean greenstone belt and its remelting formed granite. ④ Late Yanshanian - diagenesis and mineralization period.
Keywords:Xiadian  diorite-porphyrite  zircon U--Pb ages  geological records
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