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xuzhipiao木虫 (正式写手)
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| 断裂带控制了福建地区新生代地壳变形和现今地壳运动的南北差异。研究表明，受该断裂带控制，福建现代地壳运动具有南北分区，地壳活动南强北弱、南升北降；历史中强地震基本分布在断裂以南的东部和邻海地区，形成南部地震集中区；环境剪应力值高值区集中分布在台中—晋江横向构造带以南，具有北西向分带的特点。 |
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pitlord999
金虫 (小有名气)
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xuzhipiao(金币+20,VIP+0):好人，谢谢您！ 8-26 19:33
xuzhipiao(金币+20,VIP+0):好人，谢谢您！ 8-26 19:33
| Fracture dominates the north-south difference of neozoic crustal deformation and current crustal movement in Fujian. Research shows that primary characteristics of the crustal movement in Fujian are greatly controlled by this fracture, summarized as follows. The current crustal movement is distinct between north and south Fujian, stronger and more frequent in the south than in the north. Historically, high magnitude earthquakes primarily distribute in the east and coastal area to the south of the fracture, forming a centralized earthquake area in the south. High environmental shear stress area is also centrally distributed to the south of Taizhong-Jinjiang horizontal stratum, exhibiting a northwest-southeast directional feature. |
2楼2009-08-26 18:16:38
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xuzhipiao(金币+20,VIP+0):好人，谢谢您！ 8-26 19:33
xuzhipiao(金币+20,VIP+0):好人，谢谢您！ 8-26 19:33
|
断裂带控制了福建地区新生代地壳变形和现今地壳运动的南北差异。研究表明，受该断裂带控制，福建现代地壳运动具有南北分区，地壳活动南强北弱、南升北降；历史中强地震基本分布在断裂以南的东部和邻海地区，形成南部地震集中区；环境剪应力值高值区集中分布在台中—晋江横向构造带以南，具有北西向分带的特点。 Rupture zone controls the North-South differences of cenozoic diastrophism and present lithosphere movement of Fujian Province. Studies have shown that under this control, crustal movement of Fujian reveal north-south partition modern, which means crustal activities in the south shows strong and rising with weak and falling in north. In history distribution of strong earthquakes are distributed basically the east of southern rupture zone and adjacent sea areas so that centralization of Earthquake in southern area is formed. Environmental shearing strength value is concentrated in the south area of transverse tectonic belt of Taizhong-Jinjiang with the north-west features. |
3楼2009-08-26 19:09:49
xuzhipiao
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4楼2009-08-26 19:34:14
5楼2009-08-26 23:48:09
