京津唐地区地壳形变及现代构造运动 |
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引用本文: | 应绍奋. 京津唐地区地壳形变及现代构造运动[J]. 地震地质, 1982, 4(2): 3 |
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作者姓名: | 应绍奋 |
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作者单位: | 国家地震局测量大队 |
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摘 要: | 本文通过近年来,在京津唐地区取得的大地测量资料,研究本区现代构造运动,指出了北北东—北东向、北西向及东西向三组构造最为活动。它们是受近于水平方向北北西—南南东向主张应力和北东东—南西西向主压应力的应力场所控制,并以主张应力大于主压应力的作用方式出现;而又受深部构造的断块上拱和断陷的影响
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关 键 词: | 京津唐地区 现代构造运动 地壳形变 水平形变 唐山地区 北东向 北西向 东西向构造 唐山地震 断褶带 |
CRUSTAL DEFORMATION AND RECENT TECTONIC MOTION IN THE BEIJING-TIANJING-TANGSHAN REGION |
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Abstract: | This paper deals with the recent tectonic motion in this region using the geodetic data, indicating three groups of the most active structures in NNE-NE-NW directions. They have been subjected either to influence of uprising and downfaulting blocks at depth in the earth or to constraint of principal extensional stress field in NNW-SSE direction and principal compressional stress field in ENE-WSW direction, the former being larger than the latter |
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