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Reflection seismic investigation of the Dalasandstone area, Central Sweden 瑞典中部达拉砂岩区的反射地震调查
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90038-0
Jonas Lindgren, Trine Dahl-Jensen
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引用次数: 0
Simultaneous interpretation of surface and borehole gravity data from the Siljan area Siljan地区地表和钻孔重力数据的同声解释
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90028-8
Dan Dyrelius
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引用次数: 0
Regional seismic reflection profiling in the caledonides: Data acquisition and preliminary results caledonides区域地震反射剖面:数据采集和初步结果
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90052-5
Hans Palm
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引用次数: 0
A robust maximum likelihood method for gravity and magnetic interpretation 重磁解释的鲁棒极大似然方法
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90017-3
Joāo B.C Silva, Alterêdo O Cutrim

Historically, automatic curve-matching algorithms have employed the least squares method which minimizes the L2 norm of the residuals. The least squares method, however, is very sensitive to the presence of outliers in data, and the alternative robust method employed so far has been the minimum absolute errors which minimizes the L1 norm of the residuals.

Associating the type of residual norm being minimized with the sensitivity of the interpretation method to the presence of outliers may lead, however, to the false impression that there is no method more robust than the minimization of the L1 norm.

Another viewpoint is to associate robustness with the probability density function describing the errors. Long-tailed distributions are related to more robust methods. Both least squares and minimum absolute errors may be derived from a maximum likelihood approach assuming that the errors present in the data follow a Gaussian or Laplace distribution, respectively. In this paper we present a maximum likelihood estimator based on the assumptions of errors following a Cauchy distribution which is more long-tailed than either the Gaussian or the Laplace distribution. As a result, the derived method is more robust than either the least squares or the minimum absolute errors.

The superior performance of the method as compared with the least squares method in the presence of Gaussian and geological noise is demonstrated using synthetic and field data. The results show that the method is less sensitive to the initial guess than the least squares. It produces better and more consistent solutions which are, therefore, less ambiguous. Also, as the method takes into account the presence of geological noise, it may be used to obtain a rough, but reliable outline of the sources, using simple interpretation models. This feature might be useful in designing automatic interpretation algorithms.

历史上,自动曲线匹配算法采用最小二乘法,使残差的L2范数最小化。然而,最小二乘法对数据中异常值的存在非常敏感,迄今为止采用的另一种鲁棒方法是使残差L1范数最小化的最小绝对误差。然而,将最小化残差范数的类型与解释方法对异常值存在的敏感性联系起来可能会导致错误的印象,即没有比L1范数最小化更健壮的方法了。另一种观点是将鲁棒性与描述误差的概率密度函数联系起来。长尾分布与更健壮的方法有关。假设数据中的误差分别服从高斯分布或拉普拉斯分布,则最小二乘误差和最小绝对误差都可以由最大似然方法导出。本文提出了一个基于柯西分布误差假设的极大似然估计。柯西分布比高斯分布和拉普拉斯分布都要长尾。结果表明,该方法比最小二乘法和最小绝对误差法具有更强的鲁棒性。在有高斯噪声和地质噪声的情况下,与最小二乘方法相比,该方法具有更优越的性能。结果表明,与最小二乘法相比,该方法对初始猜测的敏感性较低。它产生更好、更一致的解决方案,从而减少歧义。此外,由于该方法考虑了地质噪声的存在,因此可以使用简单的解释模型来获得震源的粗略但可靠的轮廓。这个特征在设计自动解释算法时可能很有用。
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引用次数: 8
Ground probing radar measurements for water exploration: A case study 水探测的地面探测雷达测量:一个案例研究
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90023-9
Bo Löfroth
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引用次数: 0
Near surface distortion of electrical field in the Siljan impact area 锡尔詹撞击区近地表电场畸变
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90039-2
P. Zhang, L.B. Pedersen, T.M. Rasmussen
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引用次数: 0
Kiirunavaara: A comment on the low-magnetic areas on both sides of the orebody and calculations of probable depths of the ore. Principle of the oreforming process Kiirunavaara:对矿体两侧低磁区的评述和矿体可能深度的计算。改造过程的原理
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90048-3
Mark-Enar Hansson
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引用次数: 0
Densités et anomalies gravimétriques de l'intrusif du mont mégantic mont megantic入侵者的密度和重力异常
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90018-5
Maurice K Seguin, Janusz Frydecki

An accurate estimate of the Bouguer density is needed to make corrections of the gravity data and to interpret the results. Many methods have been used for this purpose. Amongst these, the following can be mentioned: field sampling and laboratory measurements, geophysical logs, data relative to seismic velocities and gravity data. Surface sampling and the relation density-seismic velocity are affected by surficial alteration of the rock units. This is why an indirect determination with the help of gravimetry is often more representative. However, the relation Bouguer anomaly versus altitude for estimate of density is lacking precision. A more rigorous method related to the free air anomaly is proposed. This density determination method is applied to the Mount Megantic area, an intrusive of Cretaceous age belonging to the Monteregian Group. The mean density for the whole of the area investigated is 2647 kg m−3. The density of each geological formation was estimated individually. The results obtained show that the calibration: free air anomaly versus altitude is the most reliable.

要对重力数据进行修正并解释结果,就需要对布格密度进行准确的估计。为此目的使用了许多方法。其中,可以提到以下几点:现场采样和实验室测量、地球物理测井、相对于地震速度和重力数据。地表取样和密度-地震速度关系受地表岩石单元蚀变的影响。这就是为什么借助重力法间接测定通常更具有代表性的原因。然而,用布格异常与海拔高度的关系估计密度缺乏精度。提出了一种更为严格的有关自由空气异常的方法。该密度测定方法应用于Megantic山地区,该地区属于蒙特雷吉亚群,属于白垩纪侵入岩。整个调查区域的平均密度为2647 kg m - 3。每个地质地层的密度分别估算。结果表明,自由空气距平随高度的定标是最可靠的。
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引用次数: 4
Geophysics in kaolin investigations in Finland 芬兰高岭土研究中的地球物理学
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90043-4
Tarmo Jokinen, Jukka Lehtimäki, Tuire Valli
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引用次数: 0
AbstractHigh resolution stacking methods 摘要:三种分辨率叠加方法
Pub Date : 1989-07-01 DOI: 10.1016/0016-7142(89)90050-1
O. E. Næss
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引用次数: 0
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Geoexploration
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