| 塔北中新生代构造演化与砂岩型铀成矿作用关系——来自磷灰石裂变径迹的证据 |
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| 引用本文： | 刘红旭,;董文明,;刘章月,;陈晓林.塔北中新生代构造演化与砂岩型铀成矿作用关系——来自磷灰石裂变径迹的证据[J].国外铀金地质,2009(3):125-133. |
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| 作者姓名： | 刘红旭 ;董文明 ;刘章月 ;陈晓林 |
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| 作者单位： | [1]核工业北京地质研究院,北京100029; [2]中国地质大学（北京）,北京100083 |
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| 基金项目： | 国防科技工业局预先研究项目（DY0603-1）、中国核工业地质局生产中科研项目（地D0604） |
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| 摘 要： | 塔里木盆地北部萨瓦甫齐及塔里克地区4个样品的磷灰石裂变径迹测年以及热史反演结果显示，两个地区的隆升时代不同，其中萨瓦甫齐地区裂变径迹年龄为3．5～3．9Ma，而塔里克地区的裂变径迹年龄为53～59Ma。热史分析揭示出岩体至少记录了自晚白垩世以来的3个显著冷却阶段。同时，结合前人对塔北中新生代隆升剥蚀研究结果，重点对塔北地区中新生代构造隆升阶段进行了详细研究与划分，结合新疆中新生代砂岩型铀成矿年龄，提出了对塔北地区中新生代构造演化与砂岩型铀成矿作用的新认识。
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| 关 键 词： | 磷灰石裂变径迹 构造隆升 构造演化 砂岩型铀成矿作用 |
Mesozoic-Cenozoic tectonic evolution and its relation to sandstone-type uranium mineralization in northern Tarim area --Evidence from apatite fission track |
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| Institution: | LIU Hong-xu, DONG Wen-ming, LIU Zhang-yue, CHEN Xia-lin (1. Beijing Research Institute of Uranium Geology, Beijing 100029, China;2. China University of Geosciences (Beijing), Beijing 100029, China) |
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| Abstract: | The apatite fission track dating and inversion result of geological thermal history of four rock specimens from Sawafuqi area and Talike area in northern Tarim Basin show that two areas uplifted at different ages. The apatite fission track ages of Sawafuqi range from 3.5 to 3.9 Ma, while the ages of Talike range from 53 to 59 Ma. The thermal history recorded by rock samples reveals that there are at least three prominent cooling phases since Late Cretaceous epoch. Detailed study was made on the division of uplifting stages during Mesozoic and Cenozoic tectonic evolution with the existing data in northern Tarim area. And new ideas on tectonic evolution and sandstone-type uranium mineralization have been put forward by combining with the sandstone-type uranium mineralization ages in this area. |
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| Keywords: | apatite fission track tectonic uplift tectonic evolution sandstone-type uranium mineralization |
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