太古宙—元古宙过渡分界及成矿动力体制转换

邓军; 孙忠实; 王建平; 王庆飞; 王喜臣; 燕长海

太古宙—元古宙过渡分界及成矿动力体制转换

1.
中国地质大学地球科学与资源学院，北京 100083
2.
岩石圈构造、深部过程及探测技术教育部重点实验室，北京 100083
3.
吉林大学地球科学学院，吉林长春 130061

基金项目:

国家自然科学基金 40172036

国家重点基础研究发展规划项目 1999043206

教育部“科学技术研究重点项目 01037

详细信息

作者简介:
邓军（1958—），男，教授，博士生导师，构造地质学和矿床学专业，主要从事区域构造、成矿流体及成矿动力学的教学和科研工作

中图分类号: P541;P61
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出版历程
- 收稿日期: 2002-03-11
- 刊出日期: 2003-01-25

Demarcating Interval between Archean Group and Proterozoic Group and Ore-Forming Dynamical Transformation

1.
Department ofEarth Science and Resource, China University of Geosciences, Beijing 100083, China
2.
The Key LaboratoryofLithosphere Tectonics and Exploration(KLLTE), MinistryofEducation, Beijing 100083, China
3.
Department ofEarth Science, Jilin University, Changchun 130026, China

摘要

摘要: 太古宙与元古宙之间分界时限较窄、测年数据偏新和混乱, 极大遏制了地球早期基础地质的深入研究.通过太古宙与元古宙分界标志和过渡标志的确定, 将太古代—元古代间动力体制转换类型划分为4种: 挤压体制向扩张体制转换; 垂直运动与水平运动间转换; 水平主压应力场转换; 地幔柱体制向板块构造体制转换.太古代与元古代间动力体制转换产物主要为真核生物、放射性元素、岩浆、矿产, 各自形成时限可达(3~5) × 10⁸ a.太古宙与元古宙之间分界不应以单一年代划分, 而是一个渐变过渡的界线, 可初步确定在2.2 0~2.80Ga之间.太古宙—元古宙界线的划分应与地球动力学和构造体制等重大事件相联系, 此研究为探求早期深部成矿作用带来新的启迪
- 太古宙—元古宙 /
- 过渡分界 /
- 成矿动力 /
- 体制转换
Abstract: The narrowness and confusion of demarcating time between Archean and Proterozoic have kept deepening research on the early geology within great limits. Through determination demarcating and transiting criteria, the transformation of geo-dynamics system between Archean and Proterozoic can be divided into four types: transformation from compressional to extensional system, from vertical to horizontal, of principal stress, from mantle plume to plate tectonics. The relatively outcomes which formed within 0.3~0.5 billions year of transformations includes eucaryote, radioelements, magma and ores. The partition between Archean and Proterozoic should have a transiting line, that can be limited in 2.20~2.80 Ga. The partition has close relation with major geological events, and this work brings a new edification to ore-formation in depth.
- Archean-Proterozoic /
- transiting line /
- ore-forming dynamics /
- system transformation

HTML全文

图 1 吉林板石沟地区地质图

1.古元古代盖层; 2.变黑云钾长花岗岩及角闪-绿片岩相韧变带; 3.中粒英云闪长岩角闪岩相线韧变带; 4.断裂及产状; 5.绿片岩相韧变带; 6.地质界线

Fig. 1. Geology sketch of Banshigou area, Jilin Province

下载: 全尺寸图片幻灯片

图 2 变质上壳岩系Sm-Nd等时线

Fig. 2. Sm-Nd isochronism graph of metamorphic supracrust systems

下载: 全尺寸图片幻灯片

表 1 变质上壳岩系Sm-Nd年龄测试与计算结果

Table 1. Sm-Nd age-dating and calculating values in metamorphic supracrustal systems

表 2 黑云长英片麻岩锆石年龄测定与计算结果

Table 2. Acorite age-dating and calculating values of biotite felsite gneiss

表 3 变黑云母钾长花岗岩锆石年龄测定与计算结果

Table 3. Acorite age-dating and calculating values of metamorphic biotite potash feldspar granite

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