Analysis of Spatial Association of Mineralization and Faults Through Fry and Fractal Modelling in Anarak Metallogenic Zone, Iran

IF 1.4 4区 综合性期刊 Q2 MULTIDISCIPLINARY SCIENCES
Mohammad Sharifi, Mohammad Ali Rajabzadeh, Alexander L. Peace
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引用次数: 0

Abstract

The Anarak Metallogenic Zone is located in the western part of the Central East Iranian Microcontinent. Paleozoic ultramafic ophiolite and metamorphic complexes are the most common rocks in the Anarak region. Sedimentary and volcanic rocks of the Cretaceous and Eocene age cover the Paleozoic rocks. The polymetallic mineralization of the Anarak is often in related to the listvenitization of ultramafic rocks. These hydrothermal deposits are structurally controlled by basement faults. Rose diagrams and Fry analysis of structural data show an E-W trend in the distribution of faults and mineralization in the region. Analysis of the aeromagnetic data characterizes a west-east and northwest-southeast trend for deep faults that control the boundary of the Paleozoic intrusive and ultramafic rocks. The fusion of the multifractal technique and the lineament factor map identified high-potential zones of hydrothermal polymetallic mineralization in the Anarak region. Fieldwork demonstrates a clear relation between the W-E fault zones and the occurrence of polymetallic deposits in the region. The major faults trending west-east, especially the basement faults, play an important role in the distribution of polymetallic deposits in the Anarak region. In addition to their role as conduits for hydrothermal fluids, these faults were crucial in the emplacement of various host rocks, such as ultramafic and intrusive rocks. This study indicates that the combination of multifractal techniques with lineament factor map processing is an inexpensive and effective method of locating high-potential hydrothermal polymetallic mineralization zones, particularly deposits associated with listvenitization.

伊朗Anarak成矿带成矿与断裂空间关联的Fry和分形模拟分析
Anarak成矿带位于伊朗中东部微大陆的西部。古生代超基性蛇绿岩和变质杂岩是阿纳拉克地区最常见的岩石。白垩纪和始新世的沉积岩和火山岩覆盖了古生代岩石。阿纳拉克的多金属成矿作用往往与超镁质岩石的成岩作用有关。这些热液矿床在构造上受基底断裂控制。构造资料的Rose图和Fry分析显示该区断裂和矿化呈东西向分布。航磁资料分析表明,深断裂控制着古生代侵入岩和超基性岩的边界,具有西东走向和西北-东南走向。多重分形技术与线状因子图的融合识别了阿纳拉克地区热液多金属成矿高潜力区。野外工作表明,东西向断裂带与该地区多金属矿床的赋存关系明显。阿纳拉克地区西东走向的主要断裂,尤其是基底断裂,对多金属矿床的分布起着重要作用。这些断裂除了作为热液流体的管道外,对各种寄主岩石(如超镁质和侵入岩)的侵位也至关重要。该研究表明,多重分形技术与线形因子图处理相结合是一种廉价而有效的高潜力热液多金属成矿带定位方法,特别是与岩石化有关的矿床。
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来源期刊
CiteScore
4.00
自引率
5.90%
发文量
122
审稿时长
>12 weeks
期刊介绍: The aim of this journal is to foster the growth of scientific research among Iranian scientists and to provide a medium which brings the fruits of their research to the attention of the world’s scientific community. The journal publishes original research findings – which may be theoretical, experimental or both - reviews, techniques, and comments spanning all subjects in the field of basic sciences, including Physics, Chemistry, Mathematics, Statistics, Biology and Earth Sciences
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