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双语推荐:重力异常

研究基于Airy—Heiskanen均衡理论构建重力控制点稀少区域平均空间重力异常参考场的方法。利用区域高分辨率地形数据构建平均空间重力异常数值模型;针对均衡理论构建重力异常存在系统性误差的问题,研究了布设少量重力观测点作为约束,对所构建的平均空间重力异常数值模型的系统性误差进行修正,并与基于EGM2008重力场模型以及基于少量离散点直接内插推估构建区域平均空间重力异常的方法进行对比。结果表明,该方法得到的计算值精度明显优于后两者,同时能大大减少重力测量的工作量,且适宜于困难地区平均空间重力异常的填补。
The method of establishing the mean free-air gravity anomaly reference field with rare gravity data has been studied based on the Airy and Heiskanen isostatic theory.The numerical model of the mean free-air gravity anomalies has been established using the regional high-resolution topographic data; then for the problem that the systematic errors existed in the computational area,a few of gravimetric points have been chosen as constraint points in order to eliminate errors.Finally,the comparisons have been made among the gravity field model of EGM2008 and interpolation using separate points.As a result,the method could get better precision than two other methods as well as could reduce workloads in gravity measurement in the fields,the method is suitable for establishing the mean free-air gravity anomalies in difficult conditions.
为了研究大震(Ms≥7)和巨震(Ms≥8)与重力异常和活动断裂的关系.利用EIGEN-6C重力模型计算了相关地区的自由空气重力异常,查阅了相关地区的布格重力异常和活动断裂构造.分析了重力异常突变带和活动断裂带与这些地震的空间分布.发现大震和巨震常在重力异常突变带和活动断裂带交汇处发生.结合前人对地球深部构造特征的研究,提出了一种流变模型来解释大地震发生于重力异常突变带和活动断裂带交汇处的原因:地壳深部流变层(体)流动受阻碍而引起重力异常和能量积累与释放.
In order to find the relationship among a large (Ms ≥7)earthquake,or a giant earthquake (Ms ≥8)and the steepest gradient of gravity field and active fault,the free air gravity anomaly map by EIGEN-6C gravity model was calculated,the bouguer gravity anomaly and active fault of the region trends to occur large or giant earthquake is consulted.The spatial distribution of large and giant earthquakes and active fault,gravity anomaly is analyzed.We come to a conclusion that a large or giant earthquake trends to occur at the intersection area of steepest gradient of gravity field and active fault.With the previous study of deep structures in those area,we propose a rheological model to interpret the regularity.It is that the flow of the rheological layer (body)blocked by the brittle rocks cause the gravity anomaly and energy accumulation and release.

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异常的复杂性对资料处理和解释带来了一定的困难,而重力异常相对更为简单、更易处理和解释。通过运用空间域的泊松公式,可以在频率域内推导出由磁异常换算重力异常的计算公式,这种由磁异常换算所得到的重力异常称为磁源重力异常。这里对理论模型的磁异常数据进行了计算与实验分析,并对实际航测的磁异常资料进行了计算与处理,取得了良好的应用效果,表明了磁源重力技术的可行性、正确性和精确性。
The complexity of magnetic anomaly will cause some difficulties for the data processing and interpretation.However, gravity anomaly is relatively simple and easier processing and interpretation.We deduce the mathematical formulae of gravity a-nomaly which is converted by magnetic anomaly in frequency domain by using Poisson formula,and this gravity anomaly is called pseudo-gravity anomaly.Next,we put the pseudo-gravity anomaly to the test on the magnetic anomaly data of theo-retical model and the magnetic anomaly by aerial survey with satisfactory results,showing that the method is viable,correct-ness and accuracy.

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重力场是一个高度叠加的场,任何重力异常都是目标物与其旁侧的和深部的地质体重力异常的叠加,后者即成为目标物重力异常的背景场。重力场的分解和位场转换在重力资料的解释中起到了非常重要的作用。
The gravity field is a highly stacked field, any gravity anomalies are gravity anomaly superimposition of target objects with their lateral and deep geologic bodies, and the latter becomes the background ifeld of object gravity anomaly. It plays a very important role that gravity ifeld decomposition and potential ifeld conversion in the gravity data interpretation.

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近海航空重力数据在陆海大地水准面统一中起着重要作用。近3年来,利用我国首套航空重力测量系统(CHAGS)完成了渤海湾地区近20万平方千米的5′×5′格网平均重力异常数据的获取。本文首先介绍了渤海湾地区航空重力测量的概况,给出航空重力测量数据的处理要点;然后,详细讨论了航空重力测量的精度评估方法,其中针对该区域的测线布设特点,提出了“重叠格网比较法”以评估格网平均重力异常的内符合精度。结果表明,对于5′的波长分辨率,交叉点重力异常不符值在抗差后的中误差约为15. mGal ,重叠格网法获得的5′×5′格网平均重力异常的中误差约为16. mGal ;5′×5′格网重力异常与卫星测高和船测重力的比较精度优于30.mGal ;由航空重力测量获得的1°×1°格网平均重力异常与GOCE卫星重力位模型的计算值相比较,其系统性差异小于05. mGal、中误差约为27. mGal。利用航空重力数据后,渤海湾区域大地水准面与16个GPS水准点的比较精度由EGM2008模型的约23 cm提高到约12 cm。
Offshore airborne gravity plays a very important role in the unifying of the land geoid and marine geoid .Airborne gravimetry using Chinese airborne gravimetry system is flown in Bo Hai Bay in the l ast three years .The surveying area extends about two hundred thousand square kilometers and 5′× 5′grid mean gravity anomaly has been obtained .The gravimetry is summarized and its key processing method is introduced firstly .Then ,we discuss the accuracy estimation methods for the airborne gravity in detail ,and introduce so‐called grid‐overlapping method to appropriately evaluate the internal accuracy of the grid mean gravity anomaly .The results indicate that the standard deviation of the crossover errors is about 1 5.mGal at the resolution of 5 arcmin ,the standard deviation of the 5′× 5′grid mean gravity anomaly evaluated by grid‐overlapping method is about 1 6.mGal ,and the accuracy of the 5′× 5′grid mean gravity anomaly are better than 3 0. mGa1 compared with th
根据煤田与围岩存在密度差,会引起重力异常的实际情况,本文采用重力法进行煤田勘探,首先分析了重力勘探的可行性,然后在介绍了拉格斯特重力仪工作原理和技术指标的基础上,使用拉格斯特重力仪进行了煤田勘探,研究了煤田重力勘测的工作过程以及对重力异常的校正。
According to the density difference between coal field and the rocks around, it will lead to the actual abnormal situation of gravity. In this paper,the gravity method for coal exploration is used. Firstly, it analyzes the feasibility of gravity exploration, and then based on the Lacoste &. Romberg gravity meter work principle and technical index, it uses L-R gravimeter coalfield exploration to do the research work in coal gravity survey and the gravity anomaly correction.

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通过对云南武定地区1:5万磁测和重力资料综合分析研究,确定了局部重力异常(带)42个,重力异常41个,5个重力有利找矿远景区;对该区磁异常特征分析,获得磁(ΔT)异常86个,确定了4个有利找矿远景区。结合地质、、重力、磁测资料的综合分析与研究,划分断裂61条,提出了铜、铁找矿找矿有利地段及远景区,为武定地区寻找隐伏铁铜矿床提供了地球物理依据。
42 local gravity high anomalies, 41 gravity low anomalies with 5 gravity anomalous areas favorable ore-searching prospect areas are delineated by 1:50 000 gravity survey, and 86 magnetic anomalies (ΔT) with 4 favorable ore-searching prospect areas are delineated by 1:50 000 magnetic survey in the Wuding region. 61 fracture zones and Cu-Fe prospect areas based on geological, gravity survey and magnetic survey data are determined in the Wuding region.

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基于最新重力场模型对2014年于田Ms7.3地震震区的重力异常特征进行分析,并应用Crust1.0地壳模型计算得到震区的深部构造形态,结果显示:震中位于地壳厚度陡变带上.同2008年于田Ms7.3地震相比,震中虽位于不同位置,但发震机制均与深部地壳结构变化密切相关.统计研究区内历史地震活动性与重力异常之间的关系,发现震中的自由空气异常与地形存在明显的线性相关性,而布格异常和均衡异常的结果则明显不同.进一步地分别计算不同重力异常的水平总梯度和线性信号,结果表明:重力异常梯度量与地形的相关特性更明显.研究表明:Ms7.0以上大震活动与重力异常之间具有明显的统计特性学,这可能与重力异常反映的深部结构和壳内质量分布的不均匀有关.
The latest model of the gravitational field was used in the analysis of the gravity anomaly characteristics in the Yutian seismic zone and surrounding regions.The layered crustal structure model (Crust1.0)has been applied to obtain the deep tectonic structure around the seismic zone.This epicenter occurred in the steep variations of the crustal thickness.Contrast to the Ms 7.3 earthquake in 2008 in this region,although these two epicenter were located in different 3-D spaces,they are closely related to the changes in the deep crustal structures.Besides,based on the statistical analysis of the relationship between the seismicity of historical earthquakes (Ms ≥5.0)and three different gravity anomalies,we found that the free-air gravity anomalies in the seismic zone are in an obvious linear cor-relation to the topography,while the Bouguer anomaly and isostatic anomaly are distinctly different with the topography.In addition, the total gorizontal gradient (HGM)of the anomalies w

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区域重力资料是研究大地构造的基础资料。利用河南省?1∶20?万区域重力调查工作所取得的成果资料,计算了河南省的?1∶20?万剩余重力异常,分析了剩余异常的意义和特征,研究了剩余异常与河南省大地构造要素的对应关系。结果表明,剩余重力异常更好地反映了河南省的大地构造特征,与已知构造单元及构造要素有着良好的对应关系,而且比常用的布格异常对地质构造要素特征的反映更清晰、更细致。
Regional?gravity?data?are?basic?information?for?the?research?of?tectonics.?Using?the?field?data?by?regional?gravity?survey,?the?residual?gravity?anomaly?(scale?1:200,?000)?in?Henan?province?was?computed.?Then?the?characteristic?of?the?residual?anomaly?is?studied,?and?the?relationship?between?the?residual?gravity?anomaly?and?the?geotectonic?is?researched.?From?above,?it?is?concluded?that?the?residual?gravity?anomaly?has?a?close?relationship?with?the?tectonics?and?shows?the?feature?of?tectonics?in?more?detail?than?Bouguar?anomaly?does.

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利用GRACE重力卫星月重力场数据,通过去相关与高斯滤波等方法获取日本大地震震前震源区周缘年度、季度和年度差分重力变化,以及若干点位时间序列重力变化。分析结果表明:日本大地震前5年内在震源区周边出现了比较明显的卫星重力异常正负交替和迁移现象,至震前1~2年,震区周边形成了明显正负异常区,正重力异常重力增加现象明显。点位重力时间序列分布指出日本MW9.0级地震前存在与1976年唐山地震类似的重力变化现象。反映出日本大地震震前震源区周边地下物质运动、质量迁移和能量积累等问题。
The decorrelation and Gaussian smoothing method is implemented in GRACE monthly gravity field products to obtain annual and seasonal gravity changes in Japan and its vicinity,as well as time series gravity changes of several points.Results show regional gravity fields in Japan and its vicinity varied from positively to negatively and from area to area in five years before the Japan MW 9.0 earthquake,obviously positive to negative gravity changes were formed in 1~2 years.Time series gravity changes of several points indicate the Japan earthquake displayed the similar time variation gravity phenomenon with the 1976 Tangshan earthquake in China.These results reflect mass migration,mass movement and energy accumulation in Japan and its vicinity before the earthquake occurred.

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