Titlebook: Geostatistics Valencia 2016; J. Jaime Gómez-Hernández,Javier Rodrigo-Ilarri,Jos Book 2017 Springer International Publishing AG, part of Sp

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书目名称Geostatistics Valencia 2016被引频次学科排名




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书目名称Geostatistics Valencia 2016年度引用学科排名




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书目名称Geostatistics Valencia 2016读者反馈学科排名

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征兵

Modelling Asymmetrical Facies Successions Using Pluri-Gaussian Simulations Triassic vertical facies succession in the Latemar carbonate platform (Dolomites, Northern Italy) composed of shallowing-upward cycles. The model is flexible enough to capture the different transition probabilities between the environments of deposition and to generate realistic facies successions.

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A New High-Order, Nonstationary, and Transformation Invariant Spatial Simulation Approach on the similarity of the high-order statistics of the data event of the hard data compared to those of the training image. The high-order similarity measure introduced herein is effectively invariant under all linear spatial transformations..Following the sequential simulation paradigm, the templat

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New Approach to Recoverable Resource Modelling: The Multivariate Case at Olympic Damr discusses a different approach to recoverable resource estimation based on conditional simulation methods..The Olympic Dam deposit is one the world’s largest polymetallic deposits. The resource estimation practices at the Olympic Dam are comprised of a combination of linear and non-linear techniqu

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Comparison of Two Multivariate Grade Simulation Approaches on an Iron Oxide Copper-Gold Depositluding some of the significant geological risks. A short summary of different multivariate simulation techniques is given. The process and results of multivariate simulation of total copper, acid-soluble copper, gold, and iron within the deposit using the two methodologies are presented. The focus i

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Complexities in the Geostatistical Estimation of Besshi-Type Mineral Deposits on the Northwest of Pi better results in basic and moving windows statistics. Semivariograms showed defined structures with anisotropy in the 0° and 90° directions (considering 0 to the north). To apply the lognormal kriging estimation is the main objective of this work, because of the complexities of the geology in the

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