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Singular value decomposition (SVD) for extraction of gravity anomaly associated with gold mineralization in Tongshi gold field, Western Shandong Uplifted Block, Eastern China

机译:山东省西部山东省山东省山东省占煤矿矿化与黄金矿化相关的重力异常的奇异值分解(SVD)

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A singular value decomposition (SVD) program on MATLAB platform was effectively used to handle gravity signals for the Tongshi gold field. Firstly, the gravity signals were decomposed into different eigenimages with the help of singular value decomposition method (SVD). Secondly, the thresholds between the eigenvalues reflecting different layers of ore-controlling factors were established by multi-fractal method. Finally images reflecting different layers of ore-controlling factors were rebuilt. This yielded two layers of two-dimensional singular value images that depict regional and local ore-controlling factors, respectively. 1. The regional ore-controlling factor is a saddle valley with the gravity anomaly values varying from ?55 to 51 μm s?2 on the NW trending swell with the gravity anomaly values varying from ?55 to 567 μm s?2 on the SW side of the Mesozoic volcanic sedimentary basin with the gravity anomaly values varying from ?56 to ?974 μm s?2. The saddle valley might be tectonically an extensional area where the Tongshi complex pluton and all gold deposits are located and thus this area is favorable for gold deposits. 2. The local ore-controlling factor is the Tongshi complex pluton with a negative circular gravity anomaly varying from ?339 to ?11 μm s?2 and the ring contact metasomatic mineralization zone around the Tongshi complex with the positive gravity anomaly varying from 37 to 345 μm s?2. The skarn and porphyry types of gold deposits are located within the complex pluton and the Carlin and cryptobreccia types of gold deposits are located within the contact metasomatic mineralization zone. Thus both of them are potential areas for gold deposits. 3. The Tongshi gold field exhibits a typical complexity with multi-layers of ore-controlling factors.
机译:MATLAB平台上的奇异值分解(SVD)程序有效地用于处理桐施金领域的重力信号。首先,在奇异值分解方法(SVD)的帮助下,重力信号被分解成不同的特征范围。其次,通过多分形法建立了反射不同层的特征值之间的阈值。最后重建反映不同层次的矿石控制因子的图像被重建。这产生了两层二维奇异值图像,分别描绘了区域和局部矿石控制因子。 1.区域矿石控制因子是鞍座谷,重力异常值从λ5到51μms?2在趋势趋势上变化,重力异常值从Δ25到567μms?2中生代火山沉积盆的一侧,具有重力异常值,从α56到Δ974μms?2。马鞍谷可能是一个构造一个延伸区域,其中桐当砖和所有金沉积物所在,因此该区域有利于金沉积物。局部矿石控制因子是桐树复合芦苇,具有负圆形重力异常,从α339到α139〜11μmsα2和环形接触态态矿化区,与37到37的正重力异常不同345μms?2。矽卡岩和斑岩类型的金矿床位于复杂的芦苇内,金矿床和Cryptobreccia类型的金沉积物位于接触态矿化区内。因此,它们都是金沉积物的潜在区域。 3.通仕金田表现出典型的复杂性,具有多层矿石控制因子。

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