| 湖北省随州三里岗地区二长花岗岩Rb-Sr、40Ar/39Ar同位素年龄 |
| |
| 引用本文： | 石玉若,张宗清,刘敦一,唐索寒,王进辉,陈文,张思红,刘新宇. 湖北省随州三里岗地区二长花岗岩Rb-Sr、40Ar/39Ar同位素年龄[J]. 地球学报, 2005, 26(1): 17-20 |
| |
| 作者姓名： | 石玉若 张宗清 刘敦一 唐索寒 王进辉 陈文 张思红 刘新宇 |
| |
| 作者单位： | 中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037;中国地质科学院地质研究所,北京,100037 |
| |
| 基金项目： | 国家自然科学基金资助项目(编号:49732080) |
| |
| 摘 要： | 三里岗二长花岗岩与花山蛇绿混杂岩中的基性火山岩呈侵入接触关系,其年龄的确定可解决花山蛇绿混杂岩中基性岩形成年龄的上限问题. 本文对三里岗二长花岗岩分别进行了Sm、Nd同位素研究及Rb-Sr、40Ar/39Ar同位素年龄测定.3个全岩样品的Nd模式年龄平均值为1 064±105 Ma;12个全岩样品的Rb-Sr等时线年龄为422±53(2σ)Ma;二长花岗岩中所含角闪石矿物的40Ar/39Ar坪年龄为141.4±0.3 Ma,等时线年龄为142±2 Ma.这些结果暗示了花山蛇绿混杂岩中基性火山岩的形成年龄不可能晚于422 Ma.
|
| 关 键 词： | 三里岗 二长花岗岩 同位素年代 |
Rb-Sr and 40Ar/39Ar Ages of the Adamellite in Sanligang Area |
| |
| SHI Yu-ruo,ZHANG Zong-qing,LIU Dun-yi,TANG Suo-hai,WANG Jin-hui,CHEN Wen,ZHANG Si-hong and LIU Xin-yu. Rb-Sr and 40Ar/39Ar Ages of the Adamellite in Sanligang Area[J]. Acta Geoscientica Sinica, 2005, 26(1): 17-20 |
| |
| Authors: | SHI Yu-ruo ZHANG Zong-qing LIU Dun-yi TANG Suo-hai WANG Jin-hui CHEN Wen ZHANG Si-hong LIU Xin-yu |
| |
| Affiliation: | Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037;Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037 |
| |
| Abstract: | The Sanligang adamellite is one of the main tectonic blocks of the Huashan ophiolitic melange and has an intrusive contact with the basic volcanic rocks. The determination of the isotopic age of this adamellite can lead to determining the upper limit of the isotopic chronology of the Huashan ophiolitic melange. The ages of the adamellite in Sanligang area were measured by Sm-Nd, Rb-Sr and 40Ar/39Ar methods. The mean age of the model ages tDM determined by 3 samples is 1 064±105 Ma. 12 whole-rock samples present a Rb-Sr isochron age of 422±53(2o)Ma. Hornblende picked out from the adamellite gives an 40Ar/39Ar age of 141.4±0.3 Ma. The results indicate that the age of the volcanic rocks of the Huashan ophiolitic melange is older than 422 Ma. |
| |
| Keywords: | Sanligang adamellite isotopic chronology |
| 本文献已被 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》下载全文 |
|
