| 浅论地震震源区及地震动力源 |
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| 引用本文： | 曲金虞. 浅论地震震源区及地震动力源[J]. 甘肃地质, 1995, 4(1): 91-92 |
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| 作者姓名： | 曲金虞 |
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| 作者单位： | 甘肃省科学院 |
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| 摘 要： | 根据超深钻探的初步成果，提出大陆壳内高温、高压的水压破裂带是地壳内最危险的震源区，同时认为地幔波动是地震的根本动力源。
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| 关 键 词： | 超深钻探 水压破裂带 地震 |
DISSERTATE ON THE AREA OF EARTHQUAKE SOURCE AND POWER SOURCE |
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| Qu Jinyu. DISSERTATE ON THE AREA OF EARTHQUAKE SOURCE AND POWER SOURCE[J]. Acta Geologica Gansu, 1995, 4(1): 91-92 |
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| Authors: | Qu Jinyu |
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| Affiliation: | The Academy of Sciences of Gansu Prtivince Lanzhou 730000 |
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| Abstract: | In accordance with the data of ultra-deep drill,the author considers that high-tempretureand high-pressure hydraulic fracturing zone witmn land-crust is the most dangerous focalarea and waved motion of mentle is essential power source of earthquake. |
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| Keywords: | Ultra-deep drill Hydraulic fracturing zone Earthquake |
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