| 吉林省东部主要北东向断裂带地质特征及地壳演化 |
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| 引用本文： | 邵建波,毕守业.吉林省东部主要北东向断裂带地质特征及地壳演化[J].吉林地质,1995,14(1):35-39. |
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| 作者姓名： | 邵建波 毕守业 |
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| 作者单位： | 吉林省地质科学研究所 |
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| 摘 要： | 吉林省东部主要北东向断裂带包括伊舒断裂带，敦密断裂带及鸭绿江断裂带，对吉林省东部地质构造环境划分重要意义，本文概述了这些断裂带的地质特征，讨论了断裂带地壳演化，其演化历史可划分为韧脆性剪性阶段，边缘断裂阶段，左行走滑阶段，造山阶段，盆岭阶段及逆冲推覆阶段等六个阶段。
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| 关 键 词： | 伊舒断裂带 断裂带 地壳演化 地质特征 吉林 |
GEOLOGIC FEATURES OF NE FAUL TED XONE IN THE EASTERN PART OF JILIN PROVINCE AND ITS CRUSTAL EVOLUTION |
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| Shao Jianbo Bi Shouve.GEOLOGIC FEATURES OF NE FAUL TED XONE IN THE EASTERN PART OF JILIN PROVINCE AND ITS CRUSTAL EVOLUTION[J].Jilin Geology,1995,14(1):35-39. |
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| Authors: | Shao Jianbo Bi Shouve |
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| Abstract: | The main NE faulted zone in the eastern part of Jilin province,including Yisu, Dunmiand Yalujiang ,has an important significance for the division of geological structures in theeastern part of Jilin province. In this paper,the geologic features of the faulted zones and itscrustal evolution are summarize.The evolutionary process can be divided 6 stages,i.e. ductile-brittle shear,marginal fracture ,left-handed slip,orogenic, basin-range as wellas progressive shock-nappe. |
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| Keywords: | Yisu faulted zone Dunmi faulted zone Yalujiang faulted zone Crustalevolution |
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