| 福州盆地断层擦痕构造解析及其应力场反演 |
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| 引用本文： | 强祖基,王洪涛.福州盆地断层擦痕构造解析及其应力场反演[J].地震地质,1991,13(4):317-322. |
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| 作者姓名： | 强祖基 王洪涛 |
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| 作者单位： | 国家地震局地质研究所，国家地震局地质研究所，福建省地震局 北京 100029，北京 100029，福州 350003 |
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| 摘 要： | 本文通过野外测量众多的断层擦痕,经过计算机反演应力场,并结合地质资料分析,认为本区自中生代末至第四纪存在着四期构造应力场
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| 关 键 词： | 福州盆地 断层擦痕 主压应力 应力状态 伸展构造 |
STRUCTURAL STRIATION ANALYSIS AND INVERSION OF STRESS FIELD IN FUZHOU BASIN |
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| Qiang Zu-ji,Wang Hui.STRUCTURAL STRIATION ANALYSIS AND INVERSION OF STRESS FIELD IN FUZHOU BASIN[J].Seismology and Geology,1991,13(4):317-322. |
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| Authors: | Qiang Zu-ji Wang Hui |
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| Abstract: | Fuzhou basin is one of the typical basins on southeastern margin of China continent In the basin two groups of faults have been found. There are NNW-NW-and NNE-NE-trending faults. The NNW-trending Ba'yi reservoir-Wangjuan fault is active and also is a well-known heat-flow anomaly zone.The calculation of striats along the faults on the bedrock outcrops within the basin and its boundaries by using Etchecopar's computerized method shows that there were four important stress fields since Yanshanian phase. The first stress field was compressive in NW-SE orientation, which caused reverse fault, schistosity and mylonite zone to be formed. The second was compressive in SN or NNE orientation, but in the state of compression which produced Paleogene diabase dykes along NNE-trending faults. The third was compressive in nearly EW or WNW orientation, R = 1, σ2=σ3, but in a extension state. The evidence for the third stress field is tension-shear horizontal striation on the walls of the basic dyke |
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| Keywords: | Fuzhou basin Fault striation Maximum principal compressive stress stress field Extensional tectonics |
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