| 鲁西徂徕山地区新太古代岩浆作用——锆石SHRIMP U-Pb定年证据 |
| |
| 引用本文： | 万渝生,王世进,任鹏,颉颃强,董春艳,刘敦一.鲁西徂徕山地区新太古代岩浆作用——锆石SHRIMP U-Pb定年证据[J].地球学报,2015,36(5):634-646. |
| |
| 作者姓名： | 万渝生 王世进 任鹏 颉颃强 董春艳 刘敦一 |
| |
| 作者单位： | 中国地质科学院地质研究所, 北京离子探针中心,山东省地质调查院,中国地质科学院地质研究所, 北京离子探针中心,中国地质科学院地质研究所, 北京离子探针中心,中国地质科学院地质研究所, 北京离子探针中心,中国地质科学院地质研究所, 北京离子探针中心 |
| |
| 基金项目： | 中国地质调查局地质大调查项目“华北克拉通太古宙早期陆核形成与演化”(编号: 12120114021301);“中国地质构造区划与区域地质调查综合集成”(编号: 121201081103);科技部重点项目(编号: SQ2015FY3340051) |
| |
| 摘 要： | 徂徕山是鲁西新太古代岩石的重要出露区。在野外地质基础上,本文对3个岩石样品进行了锆石SHRIMP U-Pb定年研究。英云闪长质片麻岩遭受一定重结晶影响的岩浆锆石年龄为(2711±11)Ma,变质作用时代可能为~2.6 Ga。变质石英闪长岩遭受强烈重结晶影响的岩浆锆石年龄为2.51 Ga,被解释为更接近构造热事件的时代,而岩浆锆石年龄可能在2.53~2.55 Ga之间。二长花岗岩锆石普遍存在强烈铅丢失,根据数据点在谐和线上的分布特征,二长花岗岩的形成时代应为~2.5 Ga。结合地球化学研究和前人工作,确定了徂徕山地区新太古代地质演化历史及新太古代早期古老岩石带(B带)和新太古代晚期新生岩石带(C带)之间的界线。
|
| 关 键 词： | 新太古代 岩浆作用 鲁西 徂徕山 锆石SHRIMP定年 |
Neoarchean Magmatism in the Culaishan Area, Western Shandong: Evidence from SHRIMP Zircon U-Pb Dating |
| |
| WAN Yu-sheng,WANG Shi-jin,REN Peng,XIE Hang-qiang,DONG Chun-yan and LIU Dun-yi.Neoarchean Magmatism in the Culaishan Area, Western Shandong: Evidence from SHRIMP Zircon U-Pb Dating[J].Acta Geoscientia Sinica,2015,36(5):634-646. |
| |
| Authors: | WAN Yu-sheng WANG Shi-jin REN Peng XIE Hang-qiang DONG Chun-yan and LIU Dun-yi |
| |
| Institution: | Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences,Shandong Geological Survey Institute,Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences,Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences,Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences and Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences |
| |
| Abstract: | Culaishan is one of the most important areas with well-exposed Neoarchean rocks in western Shandong. In this paper, the authors carried out SHRIMP U-Pb zircon dating on three samples. Tonalitic gneiss has a weighted mean 207Pb/206Pb age of (2711±11) Ma for magmatic zircon with some recrystallization. It is inferred that a metamorphic event occurred at ~2.6 Ga. Zircons from a meta-quartz diorite sample show banded zoning with strong recrystallization, the age of 2.51 Ga is considered to be closer to the metamorphic time, and the intrusive time of the quartz diorite should be between 2.53 Ga and 2.55 Ga. Magmatic zircons from monzogranite show lead loss to different degrees, but the crystallization age might be ~2.5 Ga, as shown by the distribution of age data on concordia. Combined with geochemical study and previous work, the authors determined the Neoarchean geological evolution in the Culaishan area and redefined the boundary between the early Neoarchean (2.60~2.75 Ga) rock belt and the late Neoarchean (2500~2550 Ma) belt of juvenile rocks in the northwestern portion of western Shandong. |
| |
| Keywords: | Neoarchean magmatism western Shandong Culaishan SHRIMP zircon dating |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《地球学报》浏览原始摘要信息 |
| 点击此处可从《地球学报》下载免费的PDF全文 |
|
