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Variations in a gravity anomaly with respect to the field at a fixed point are used in solving this problem.
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Determination of vertical gradient of gravity anomaly with topographic data
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However, it is difficult to directly observe the vertical gradient of gravity anomaly in mountainous area.
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The vertical gradient of gravity anomaly is calculated by use of topographic data and several problems concerned are investigated and discussed.
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With GPM98C as the reference, the gravity anomaly residuals of several other models, the latest SST global gravity field models (EIGEN series and GGM series), were computed and compared.
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Also, the results were compared with those obtained by conventional techniques, which demonstrated that this method greatly improves the resolution of gravity anomalies.
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The analysis points to a higher (by 20%) value of the measured thermal background of the rise, which is consistent with a high negative gradient of gravity anomalies in this area.
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Minimum vertical gradients of the surface density of spherical sources of gravity anomalies, equivalent to density inhomogeneities of the compaction class, are gravitational indicators of these zones.
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The analysis points to an abnormally high (by approximately 20%) measured heat flow, which agrees with the high negative gradient of gravity anomalies.
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A simple formula for shape and depth determination from residual gravity anomalies
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It is found that there exists some corresponding relation between this distribution and Bouguer gravitational anomaly and seismicity.
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A mixed Lorenz-gravitational anomaly is found in the commutator of Lorentz boosts with world-line reparametrisations.
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Then we show that the gauge and gravitational anomaly in BTZ spacetime is cancelled by the total flux of a 2-dimensional blackbody at the Hawking temperature of the spacetime.
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It is applied (to establish its validity) to the verification of the gravitational anomaly in the divergence of a fermion axial current.
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The gravitational anomaly: An elementary, coordinate-space approach
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| | This paper deals with the method for calculating the regional highorder potential coefficient model by using regional gravity data.The formulas,including all systematic corrections for modifying model coefficients,are developed employing an ellipsoldal coordinate system and ellipsoldal harmonics expansion. Based on the derived formulas, the terrestrial gravity anomalies in the Qinghai-Xizang area are used to obtain a regional potential coefficient model QZ93G (completed to degree 360).The mean anomalies fro... | | 根据当今全球模型研究的Molodensky理论,推导了相应的区域高阶重力场模型系数修正公式.考虑了球近似边值条件引起的各种偏差,使用了椭球坐标系,按椭球调和展开.并利用中国青藏地区地面重力资料对原始全球模型OSU91A1F的高阶部分系数进行修正,获得该地区的局部重力场模型QZ93G(完整到360阶),它对实测平均重力异常的恢复精度为±11.8×10-5m/s2. | | 文摘来源 | | Assuming that regional gravity isostatic anomalies are distributed by the density heterogeneities connected with small-scale convection in the upper mantle and the boundary deformations, we establish a convection model in this paper, which is constrained on the regional isostatic gravity anomaly. The computation models show that a possitive center of isostatic gravity anomaly corresponds to a divergent zone of mantle flow and a negative center corresponds to a convergent zone. The convection patterns are st... | | 假定区域重力均衡异常主要源于由上地幔小尺度热对流相应的物质的不均匀和由此对流动力效应而导致的边界形变,同时将上地幔模拟为一均匀的等粘滞系数的牛顿粘滞流体,其主要的热量来自下地幔.由此建立了以流体力学3个基本方程为基础的热对流模型,并讨论了低瑞利数状态下,以区域重力异常和上地幔小尺度对流相关方程为主要条件,上述方程的基本解.几种模拟重力均衡异常所对应的流场表明;区域重力均衡异常正异常中心对应于上地幔小尺度对流上升流,表现出地幔上隆;相反,负异常中心对应于对流下降流,表现出岩石层(地壳)向下弯曲.结合实际的地质构造形态和重力异常形态,这些结果将有利于对板块内部岩石层动力学的理解. | | 文摘来源 | | This paper proposes an inversed method to inverse the multi-interfaces of density which is applied to the gravity anomaly,and develops certain theoretical basis.Using prior information and geophysical practice to institute the rule of choosing the system of regular parameter, we have generalized. A. H. TNXOHOB's regularized method to solve the system of integral equation of first kind,and have gained the optimal regular solutions.This method has been realized in computer.It is not only corrected for the in... | | 用重力异常数据反演多层介质密度分界面的数值反演方法,把的正则化方法推广到解第一类积分方程组,利用解的先验信息和物探资料,建立了一个优选正则化参数组的原则,从而得到了最优正则解.该方法已在计算机上实现.不仅理论模型反演结果正确,而且已有效地应用于实际重力资料的反演和解释. | | 文摘来源 | |   | | << 更多相关文摘 |
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