| 裂变径迹法在研究造山带隆升过程中的应用介绍 |
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| 引用本文： | 吴中海,吴珍汉.裂变径迹法在研究造山带隆升过程中的应用介绍[J].地质科技情报,1999,18(4):27-32. |
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| 作者姓名： | 吴中海 吴珍汉 |
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| 作者单位： | 中国地质科学院地质力学研究所,北京,100081 |
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| 基金项目： | 国家“九五”攀登项目!(95-S-05-03-02)“东亚大陆地球动力学研究”的子课题“东亚地壳运动与动力学过程”成果 |
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| 摘 要： | 介绍了４种类型的造山带隆升－冷却模式，不同模式对应不同的磷灰石裂变径年龄－－高程图特征；了不同构造造背景下的热历史特征一裂变径迹年龄序列。裂变径变宅遮挡同统计分布型式对应于不同的热历史，具有不同的年代学意义。
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| 关 键 词： | 裂变径迹 部分退火带 封闭温度 山脉隆升 热历史 |
| 修稿时间： | 1999-02-06 |
USE OF FISSION TRACK DATING IN STUDYING THE UPLIFT HISTORY OF OR OGENIC BELT |
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| Wu Zhonghai,Wu Zhenhan.USE OF FISSION TRACK DATING IN STUDYING THE UPLIFT HISTORY OF OR OGENIC BELT[J].Geological Science and Technology Information,1999,18(4):27-32. |
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| Authors: | Wu Zhonghai Wu Zhenhan |
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| Abstract: | Fission track dating is an important means for studying orogenic belt's uplift history.The different pattern of length distribution of confined tracks well corresponds to the diversed of thermal history and have different chronologic implication.There are four types of uplift cooling patterns corresponding to different apatite fission track age depth profiles.Different kinds of tectonic setting possess diverse thermal history and fission track age sequence. |
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| Keywords: | fission track partial annealing zone closure temperature orogenic belt's uplift thermal history |
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