| 郯庐断裂带的基本特征及其对沉积盆地的控制 |
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| 引用本文： | 赵世英. 郯庐断裂带的基本特征及其对沉积盆地的控制[J]. 山东科技大学学报(自然科学版), 1986, 0(4) |
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| 作者姓名： | 赵世英 |
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| 摘 要： | 郯庐断裂带是我国东部的一条巨型断裂带。在山东境内是不同大地构造单元的分界线,使东西两侧的深部、基底和盖层在地质和地球物理方面,都有很大的差异。该断裂成生于太古代中期,并开始对两侧的沉积与剥蚀起控制作用。在长期的活动中,表现出间歇性、继承性和差异性。运动特点则主要以差异升降为主,没有发生大规模的水平运动。
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| 关 键 词： | 断裂带 构造控制 古陆剥蚀 地壳升降运动 地壳水平运动 古构造带 山东临沂 |
THE BASIC CHAR ACTERISTICS OF TANLU FRACTURE BELT AND ITS CONTROLLING ON THE SEDIMENTARY BASIN |
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| Zhao Shiying. THE BASIC CHAR ACTERISTICS OF TANLU FRACTURE BELT AND ITS CONTROLLING ON THE SEDIMENTARY BASIN[J]. Journal of Shandong Univ of Sci and Technol: Nat Sci, 1986, 0(4) |
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| Authors: | Zhao Shiying |
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| Affiliation: | Zhao Shiying |
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| Abstract: | The Tanlu fracture belt, acting as a boundary of various tectonic units within the province of ShangDong is especially large scale. It makes a great difference in geological and geophysical characteristics of both the eastern and the western sides. This fracture was formed at the middle of Archeozoic era, and then began to control the depositions and erosions of the both sides. The function of its controlling is continuing to the recent times. During long period movement it has been showing ephemeral, successive and differential proper ties. Differential rising and subsiding is its mainly feature, no existing a large scale horizontal movement |
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| Keywords: | fracture belt structural control paleontinental erosion crustal movement rising and subsiding crustal horizontal movement palaeoteetonic belt Shandong Linyi |
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