| 安徽宁芜地区铁氧化物-磷灰石矿床中金云母Ar-Ar定年及其地球动力学意义 |
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| 引用本文： | 袁顺达,侯可军,刘敏.安徽宁芜地区铁氧化物-磷灰石矿床中金云母Ar-Ar定年及其地球动力学意义[J].岩石学报,2010,26(3):797-808. |
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| 作者姓名： | 袁顺达 侯可军 刘敏 |
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| 作者单位： | 1. 中国地质大学地质过程与矿产资源国家重点实验室,北京,100083;中国地质科学院矿产资源研究所,北京,100037
2. 中国地质科学院矿产资源研究所,北京,100037 |
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| 基金项目： | 国家重点基础研究课题(2007CB411405和2007CB411407)、国土资源大调查项目(1212010634001)、国家自然基金项目(40903020)、中央级公益性科研院所基本业务费专项资金(K2007-1-12)及中国博士后科学基金联合资助 |
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| 摘 要： | 铁氧化物-磷灰石型铁矿床是长江中下游成矿带的重要组成部分,对其成岩成矿时限的精确厘定,是理解长江中下游地区中生代大规模成矿作用的动力学演化的关键。本文分别对宁芜盆地南部白象山、和睦山及中部的陶村三个大-中型铁矿床中与磁铁矿密切共生的金云母单矿物进行了Ar-Ar同位素测年,获得白象山矿床金云母Ar-Ar坪年龄为134.9±1.1Ma,对应的反等时线年龄为133±2Ma;和睦山矿床金云母Ar-Ar坪年龄为132.9±1.1Ma,对应的反等时线年龄为133.9±2.4Ma;陶村矿床金云母的反等时线年龄为128±14Ma。该区铁氧化物-磷灰石型矿床与该区火山-次火山岩具有密切的时间联系,成岩成矿时限主要集中于135～126Ma。综合研究表明,长江中下游第二期成岩成矿作用的时限为135～126Ma,对应于岩石圈的大规模快速减薄的地球动力学背景。
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| 关 键 词： | 铁氧化物-磷灰石矿床 金云母Ar-Ar年龄 宁芜 长江中下游成矿带 地球动力学背景 |
| 收稿时间： | 8/9/2009 12:00:00 AM |
| 修稿时间： | 1/9/2010 12:00:00 AM |
Timing of mineralization and geodynamic framework of iron-oxide-apatite deposits in Ningwu Cretaceous basin in the Middle-Lower Reaches of the Yangtze River,China: Constraints from Ar-Ar dating on phlogopites |
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| Yuan SD,Hou KJ and Liu M.Timing of mineralization and geodynamic framework of iron-oxide-apatite deposits in Ningwu Cretaceous basin in the Middle-Lower Reaches of the Yangtze River,China: Constraints from Ar-Ar dating on phlogopites[J].Acta Petrologica Sinica,2010,26(3):797-808. |
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| Authors: | Yuan SD Hou KJ and Liu M |
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| Institution: | State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China;Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China |
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| Abstract: | The iron-oxide-apatite deposits located in Ningwu area are important components of the Middle-Lower Yangtze River metallogenic belt. Constraining the timing of petrogenesis and mineralization in this area is crucial to better understand the deep geodynamic processes which controlled the Mesozoic large-scale mineralization of this area. We here present the Ar-Ar dating results for iron-oxide-apatite mineralization conducted on three phlogopites collected from the Baixiangshan, Hemushan, and Taocun iron deposits. Phlogopite from the large-sized Baixiangshan iron deposit yielded a well-defined 40Ar/39Ar plateau age of 134.9±1.1Ma and an inverse isochron age of 133±2Ma. Phlogopite from the medium-sized Hemushan iron deposit yielded a well-defined 40Ar/39Ar plateau age of 132.9±1.1Ma and an inverse isochron age of 133.9±2.4Ma. Phlogopite from the large-sized Taocun iron deposit defined an inverse isochron age of 128±14Ma. These ages are consistent with the published U-Pb ages for zircons separated from volcanic-subvolcanic rocks in this area, suggesting that iron-oxide-apatite deposits are temporally associated with volcanic-subvolcanic rocks in Ningwu area, and constraining that its petrogenesis and metallogenis predominately took place during 135 to 126Ma. A summary of regional geochronological data suggests that the second pulse of petrogenesis and mineralization in the Middle-Lower Yangtze River area mainly concentrated on 135~126Ma, corresponding to a geodynamic setting of rapid thinning of lithosphere. |
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| Keywords: | Iron-oxide-apatite deposit Phlogopite Ar-Ar age Ningwu The Middle-Lower Yangtze River metallogenic belt Geodynamic setting |
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