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| 新疆西天山查岗诺尔铁矿床成矿时代——来自石榴子石Sm-Nd等时线年龄的信息 | |
| 引用本文： | 洪为,张作衡,李华芹,李凤鸣,刘兴忠.新疆西天山查岗诺尔铁矿床成矿时代——来自石榴子石Sm-Nd等时线年龄的信息[J].矿床地质,2012,31(5):1067-1074. |
| 作者姓名： | 洪为 张作衡 李华芹 李凤鸣 刘兴忠 |
| 作者单位： | 1. 中国地质科学院矿产资源研究所国土资源部成矿作用与资源评价重点实验室,北京,100037 2. 武汉地质矿产研究所,湖北武汉,430205 3. 新疆维吾尔自治区地质矿产勘查开发局,新疆乌鲁木齐,830000 4. 新疆维吾尔自治区地质矿产勘查开发局第三地质大队,新疆库尔勒,841000 |
| 基金项目： | 本文得到国家重点基础研究发展计划(2012CB416803);国家科技支撑计划(2011BAB06B02-05)和地质矿产调查评价项目(1212011085060)联合资助 |
| 摘 要： | 查岗诺尔铁矿床赋存在大哈拉军山组中-上部的安山质火山碎屑岩和火山熔岩内,主矿体FeⅠ周围发育大量以石榴子石为代表的高温热液蚀变,精确厘定高温热液蚀变的时间是确定成矿作用是与火山作用有关还是由岩体侵入作用所导致的关键。石榴子石与磁铁矿体的关系最为密切,其形成时间稍早或同时于磁铁矿。石榴子石Sm-Nd同位素测试结果表明,147Sm/144Nd值为0.2792~0.5481,143Nd/144Nd值为0.512950~0.513501,7个样品拟合的线性关系良好,获得的Sm-Nd等时线年龄为(316.8±6.7)Ma,指示了高温热液蚀变的时间,表明主要磁铁矿体的形成时代为早石炭世晚期,成矿作用及高温热液蚀变可能不是矿区内二叠纪岩体侵入携带的岩浆热液与大理岩发生矽卡岩化所导致,而可能是大哈拉军山组火山岩喷发后的岩浆期后热液与下伏大理岩发生接触交代反应引起的。 |
| 关 键 词： | 地球化学 成矿时代 石榴石Sm-Nd等时线年龄 查岗诺尔铁矿 西天山 新疆 |
| 收稿时间： | 2012/4/15 0:00:00 |
| 修稿时间： | 2012/8/23 0:00:00 |
Metallogenic epoch of Chagangnuoer iron deposit in western Tianshan Mountains, Xinjiang: Information from garnet Sm-Nd isochron age |
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| HONG Wei,ZHANG ZuoHeng,LI HuaQin,LI FengMing and LIU XingZhong.Metallogenic epoch of Chagangnuoer iron deposit in western Tianshan Mountains, Xinjiang: Information from garnet Sm-Nd isochron age[J].Mineral Deposits,2012,31(5):1067-1074. | |
| Authors: | HONG Wei ZHANG ZuoHeng LI HuaQin LI FengMing and LIU XingZhong |
| Institution: | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China;MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, CAGS, Beijing 100037, China;Wuhan Institute of Geology and Mineral Resources, Wuhan 430205, Hubei, China;Xinjiang Bureau of Geology and Mineral Resources Development, Urumqi 830000, Xinjiang, China;No.3 Geological Party of Xinjiang Bureau of Geology and Mineral Resources Development, Korla 841000, Xinjiang, China |
| Abstract: | The large-size Chagangnuoer iron deposit is hosted in andesite and andesitic volcaniclastic rocks in the middle-upper part of Carboniferous Dahalajunshan Formation, with widespread high hydrothermal alteration (represented by garnet) distributed extensively around the uppermost ore body FeI. The precise formation age of high hydrothermal alteration is the key to judging whether iron metallogeny was related to volcanism or intrusive activity. Garnet, which had a closely genetic relationship with magnetite, was formed simultaneously with or slightly earlier than magnetite. Garnet Sm-Nd isotope analyses reveal that 147Sm/144Nd values vary between 0.2792 and 0.5481 while 143Nd/144Nd ratios vary between 0.512950 and 0.513501. Data of seven isotope samples form a good linear fitting relationship, yielding the Sm-Nd isochron age of (316.8±6.7) Ma, which represents the formation epoch of high-temperature hydrothermal alteration. The result indicates that magnetite intergrown with garnet was formed at the late stage of Early Carboniferous period. Therefore, the iron metallogeny and high hydrothermal alteration might have resulted from the metasomatism between the post-magmatic hydrothermal solution derived from eruption of Dahalajunshan Formation volcanic rocks and the underlying marble, rather than the skarnization caused by the reaction between magmatic hydrothermal solution from Permian intrusion and marble in the ore district. |
| Keywords: | geochemistry metallogenic epoch garnet Sm-Nd isochron age Chagangnuoer iron ore deposit Western Tianshan Mountains Xinjiang |
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