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利用电阻率成像和激发极化地球物理勘探进行潜在金矿成矿制图的数据。

Data for the potential gold mineralization mapping with the applications of Electrical Resistivity Imaging and Induced Polarization geophysical surveys.

作者信息

Arifin Mohd Hariri, Kayode John Stephen, Izwan Muhammad Khairel, Zaid Hussein Ahmed Hasan, Hussin Hamzah

机构信息

School of Environmental Science and Natural Resources, Department of Geology, Universiti Kebangsaan Malaysia, Bangi, Selengor, Malaysia.

Environmental Technology, School of Industrial Technology, Universiti Sains Malaysia, 11800 Pulau-Pinang, Malaysia.

出版信息

Data Brief. 2018 Dec 31;22:830-835. doi: 10.1016/j.dib.2018.12.086. eCollection 2019 Feb.

DOI:10.1016/j.dib.2018.12.086
PMID:30766903
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6362863/
Abstract

To identify the potential zones for gold mineralization at the Felda Chiku 3, Gua Musang, Kelantan, East coast Malaysia, twenty-one (21) geophysical survey lines were conducted at the proposed mineral exploration site using the pole - dipole of the electrical resistivity and induced polarization arrays to get the maximum depth of 150 m with 400 m survey length. From the resistivity and chargeability concentration maps, the potential mineralized zones as delineated, was observed to be dominantly concentrated towards the southwest and northern part of the area. The 3D resistivity and chargeability slice model present low resistivity values and high chargeability values that are well correlated which is palpable especially at the depths of 25 m and 50 m respectively. The data showed that the potential mineralized zones are trending approximately north-south directions. Forty (40) drilling locations were proposed for follow-up drilling based on the resistivity and chargeability models.

摘要

为确定马来西亚东海岸吉兰丹瓜穆桑联邦土地发展局芝古3号金矿的潜在矿化区域,在拟建的矿产勘探场地进行了21条地球物理测量线,采用电阻率和激发极化阵列的偶极装置,测量长度为400米,最大深度达150米。从电阻率和充电率浓度图来看,所划定的潜在矿化区域主要集中在该区域的西南部和北部。三维电阻率和充电率切片模型显示出低电阻率值和高充电率值,二者具有良好的相关性,在25米和50米深度处尤为明显。数据表明,潜在矿化区域大致呈南北走向。基于电阻率和充电率模型,提出了40个后续钻探的钻孔位置。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/ed7268b1d472/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/86b9d968a607/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/2db577837064/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/259cce5567bc/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/ed7268b1d472/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/86b9d968a607/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/2db577837064/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/259cce5567bc/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ccff/6362863/ed7268b1d472/gr4.jpg

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