| 郯庐断裂带江苏段晚新生代沉积与断裂活动 |
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| 引用本文： | 朱永正. 郯庐断裂带江苏段晚新生代沉积与断裂活动[J]. 防灾减灾工程学报, 1991, 0(4) |
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| 作者姓名： | 朱永正 |
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| 作者单位： | 江苏省地震局 |
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| 摘 要： | 本文从晚新生代各时期沉积的分布、厚度及间断情况,分析郯庐断裂带各主干断层(F_1-F_4)及 F_5在相应时期对沉积所起的控制作用,以揭示该断裂带具有长期活动性及活动的多期性、间歇性、突发性等特征。此外,本文对全新世活动还补充了地貌、水系、地裂缝等方面的依据。
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LATE CENOZOIC ERA SEDIMENT AND ACTIVITY OF THE JIANGSU SEGMENT OF THE TAN-LU FAULT ZONE |
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| Abstract: | This paper has showed that the sediment in the study area were controlled by theTanlu faulu zone (F_1-F_4 and F_5) based on Late Cenozoic era sediment distribution,thick-ness and discontinuity.It is put in that the fault activity is of long-term,many-term,intermittence and sudden.Besides,this paper supplies Holocene active evidence aboutlandform,water system and ground fissure at the same time. |
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