| 庐山筲箕洼组与星子岩群年代地层关系及SHRIMP锆石U-Pb年龄的制约 |
| |
| 引用本文： | 高林志,黄志忠,丁孝忠,刘燕学,张传恒,王自强,庞健峰,韩坤英.庐山筲箕洼组与星子岩群年代地层关系及SHRIMP锆石U-Pb年龄的制约[J].地球学报,2012,33(3):295-304. |
| |
| 作者姓名： | 高林志 黄志忠 丁孝忠 刘燕学 张传恒 王自强 庞健峰 韩坤英 |
| |
| 作者单位： | 中国地质科学院地质研究所;江西省地质调查研究院;中国地质科学院地质研究所;中国地质科学院地质研究所;中国地质大学(北京);中国地质大学(北京);中国地质科学院地质研究所;中国地质科学院地质研究所 |
| |
| 基金项目： | 中国地质调查局地质大调查项目“中国新元古代年代地层格架及其全球对比”(编号: 121201011120131)；科技部科技基础性工作专项“中国地质志欧亚大陆大地构造图编制”(编号: 2011FY120100) |
| |
| 摘 要： | 本文报道在庐山筲箕洼组中获得细碧岩SHIRMP锆石U-Pb年龄(840±6) Ma,MSWD=1.3,流纹岩锆石U-Pb年龄(833±4) Ma,MSWD=1.4,和流纹岩锆石U-Pb年龄(831±3) Ma,对应的MSWD=1.47.而在星子群流纹岩中获得206pb/238U年龄为(825±5)Ma,对应的MSWD=0.46.笔者依据上述精确锆石年龄,首次提出将筲箕洼组明确定位于星子岩群之下.本文结合“江南造山带”锆石U-Pb年龄:东部变质基底的双桥山群,西部变质基底梵净山群和似盖层下江群以及中部变质基底冷家溪群和似盖层板溪群的锆石SHRIMP U-Pb年龄,将筲箕洼组定位于“武陵运动”之下的新元古代地层.依据星子岩群年龄数据,首次将星子岩群明确定位于筲箕洼组之上与双桥山群为同期的深变质岩.该年龄对限定区域地层对比和构造演化都有着重要意义.上述锆石U-Pb年龄标示了赣西北地区同样存在820 Ma界面上下的新元古代地层,为江南古陆变质地层的对比提供了新的年代学数据.
|
| 关 键 词： | 筲箕洼组 星子岩群 锆石SHRIMP定年 “江南造山带” 赣西北地区 |
The Geochronological Relationship between the Shaojiwa Formation and the Xingzi Complex Group in Northwestern Jiangxi and the Constraints on Zircon SHRIMP U-Pb Age |
| |
| GAO Lin-zhi,HUANG Zhi-zhong,DING Xiao-zhong,LIU Yan-xue,ZHANG Chuan-heng,WANG Zi-qiang,PANG Jian-feng and HAN Kun-ying.The Geochronological Relationship between the Shaojiwa Formation and the Xingzi Complex Group in Northwestern Jiangxi and the Constraints on Zircon SHRIMP U-Pb Age[J].Acta Geoscientia Sinica,2012,33(3):295-304. |
| |
| Authors: | GAO Lin-zhi HUANG Zhi-zhong DING Xiao-zhong LIU Yan-xue ZHANG Chuan-heng WANG Zi-qiang PANG Jian-feng and HAN Kun-ying |
| |
| Institution: | Institute of Geology, Chinese Academy of Geological Sciences;Jiangxi Institute of Geological Survey;Institute of Geology, Chinese Academy of Geological Sciences;Institute of Geology, Chinese Academy of Geological Sciences;China University of Geosciences;China University of Geosciences;Institute of Geology, Chinese Academy of Geological Sciences;Institute of Geology, Chinese Academy of Geological Sciences |
| |
| Abstract: | Ages of (840±6) Ma (MSWD=1.3), (833±4) Ma (MSWD=1.4) and (831±3) Ma (MSWD =1.47) were obtained for spilite and rhyolite from the Shaojiwa Formation. The Xingzi Complex Group has the age of 206Pb/238U (825±5) Ma (MSWD =0.46). In combination of the SHRIMP U-Pb dating of the spilite and rhyolite of the Shaojiwa Formation in the Jiangnan oregen, the authors have determined for the first time that the Xingzi Complex Group is of Neoproterozoic period and lies below the Shaojiwa Formation. These isotopic data from the Shaojiwa Formation are very important for regional correlation of the strata of the corresponding period and tectonic evolution. The zircon U-Pb ages mentioned above determine that Neoproterozoic strata around the age of 820 Ma are developed in northwestern Jiangxi Province. These data contribute to the stratigraphic subdivision and correlation of the metamorphosed rocks in whole Jiangnan old land and help geologists investigate the geological background and ore-forming conditions of the Jiangnan Orogen. |
| |
| Keywords: | Shaojiwa Formation Xingzi Complex Group zircon SHRIMP dating Jiangnan orogen northeastern Jiangxi |
| 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 |
