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1.Before the earthquake, the results show that the gravity field decreased nearby the epicenter and a high gravity gradient belt occured along the active fault.
结果表明,震前震中附近出现了重力减小的现象,沿活动断裂有重力高梯度带产生;收藏指正
2.By using known analytic expressions of the displacement due to a slip of a fault of any dipping angle in an elastic or visco-elastie half-space, we have calculated by three-dimensional numerical integration, the additional gravity field on the ground surface, resulting from various types of fault movements in an elastic or genera lized Kelvin medium, as well as the tendency of gravity change with time given rise by the rheological behavior of the medium.
应用已有的弹性和粘弹性半空间任意倾角断层位错的位移表达式,本文通过三维空间数值积分,计算了弹性介质和广义开尔文介质中断层不同的运动方式所产生的地表附加重力场,以及介质流变性导致的重力随时间的变化趋势.收藏指正
3.According to the geophysical data (mainly gravity and aeromagnetics) from a vast southern part of Hefei city (24°-32°N, 111°-19°E), the extension of Tanchang-Lujiang fault has been approached.
这是一个颇著争论的问题。 本文依据合肥以南广大地区 (24°~32°N,111°~119°E)的地球物理(主要是重力、航磁)资料及其处理结果,探讨了郯庐断裂南延问题。收藏指正
4.The text analyse region characteristic and rule of gravity and magnetism annormity in Chaoshan depression,conclusion think that the Chaoshan depression is tectonic transition belt of join two tectonic element about the dongsha islands to the xisha islands,the fault of turning towards the basin control growth of the Mesozoic group.
本文分析了潮汕坳陷区域重力、磁异常特征及地震地质规律,提出潮汕坳陷是衔接东沙群岛和西沙群岛两个构造单元的构造过渡带的观点,同时盆倾断层控制了中生界发育与分布.收藏指正
5.The authors hold that the joint actions of numerous factors such as the upper mantle uplifted zone (the mantle thinned zone of lithosphere), the upper mantle anomalous area (relatively low-velocity area), the uplifted zone of intracrustal high-conductivity layer, the deep fault (shear zone of lithosphere), the margin of the crust-upper mantle uneven masses, the basement uplifted area reflected by gravity high, the magmatic belt and tectonic intersection reflected by skipped magnetic field, control the distribution of auriferous skarn deposits and copper (associated with gold) skarn deposits.
作者认为,上地幔隆起带(岩石圈地幔减薄带)、上地幔异常区(相对低速区)、壳内高导层隆起带、深断裂(岩石圈剪切带)、地壳上地幔不均匀性块体的边缘、重力高反映的基底隆起区、跳跃磁场反映的岩浆岩带和构造交汇处等诸多因素的共同作用控制著含金夕卡岩矿床和铜伴生金夕卡岩矿床的分布。收藏指正
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