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Fluctuation Analysis to Sequence of Ore-forming Element Based on Fractal-Jump Model

机译:基于分形跳跃模型的成矿元素序列波动分析

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The self-similarity of ore-forming elements is caused by long-term, multi-period characteristics and the abnormal fluctuation induced by emergency in geological process. In this study, the fractal jump model referred as a combination of fractional Brownian motion and Poisson distributed jumps was built to depict the fluctuation pattern of ore-forming elements and simulate the distribution of Au sequence for three different mineralization intensities in Dayingezhuang gold deposit in the Jiaodong gold province, China. By calculating the fitting error and drawing the comparison diagram between the simulated data and the actual data, the applicability and advantages of the model were verified. The results showed that the fractal jump model can be considered as a reliable and computationally efficient method through the comparison of the statistical characteristics between simulated and real data. In addition, this model can well depict the change of the Au element content sequence, and better simulation was achieved when the intensity of mineralization was higher. The present work provides a new insight on the prediction of mineralized levels in concealed orebody.
机译:成矿元素的自相似性是由于长期的,多期的特征和地质过程中突发事件引起的异常波动引起的。在这项研究中,建立了分数布朗运动和泊松分布跳跃相结合的分形跃迁模型,以描绘成矿元素的波动模式,并模拟了大英阁庄金矿床中三种不同矿化强度的金序列的分布。中国胶东黄金省。通过计算拟合误差并绘制仿真数据与实际数据的对比图,验证了该模型的适用性和优越性。结果表明,通过比较模拟数据与真实数据之间的统计特性,可以将分形跳跃模型视为一种可靠且计算高效的方法。此外,该模型可以很好地描述金元素含量序列的变化,当矿化强度较高时,可以实现更好的模拟。本工作为隐蔽矿体中矿化水平的预测提供了新的见识。

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