STUDY OF SOIL GEOCHEMISTRY AND ITâS RELATIONSHIP WITH THE PRESENCE OF METAL MINERALIZATION IN KETUNGAU HULU AREA, SINTANG REGENCY, WEST KALIMANTAN PROVINCE
Ketungau Hulu is a gold prospect plan area in Sintang-Silantek Block on the island of Kalimantan which is a collaboration program between Indonesia (Geological Agency) and Malaysia (Jabatan Mineral and Geoscience). Administratively, the research area is located in Sintang Regency, West Kalimantan...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/69776 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Ketungau Hulu is a gold prospect plan area in Sintang-Silantek Block on the island
of Kalimantan which is a collaboration program between Indonesia (Geological
Agency) and Malaysia (Jabatan Mineral and Geoscience). Administratively, the
research area is located in Sintang Regency, West Kalimantan with an area of 18
km2. This study aims to identify the geological conditions, structure, alteration, and
mineralization of the study area as well as potential anomalies for base metal
elements (Au, Cu, Pb, Zn, and Mn) based on soil geochemistry data and its
relationship with the presence of mineralization. The study was conducted using
soil samples from 84 points in the ridge and spur areas. In addition to soil samples,
48 rock samples and one sample from pan concentrate were also obtained.
Furthermore, all samples were analyzed for chemical, geochemistry, statistic,
petrology, petrographic, grain mineralogy, and mineragraphy.
The research area consists of Greywacke Sandstone Unit, Arenite Sandstone Unit,
and Diorite Intrusion Unit. Geological structure that developed in the area has
relatively NNW-SSE and NW-SE trends. The alteration zones present in the
research area are argillic zone and propylitic zone. Mineralization is found in
dogtooth, crustiform, colloform, and assicular textured quartz veins with relative
orientation directions NW-SE and NNE-SSW that presence of ore minerals such as
native Au, chalcopyrite, pyrite, sphalerite, covellite, and from base metal contents
abundance in the rock samples. The results of soil sample analysis showed that the
Au had an anomaly value of log 1.90 ppb, Pb of sqrt 7.44 ppm, Zn of log 1.92 ppm,
Cu of log 1.69 ppm, and Mn of log 2.46 ppm. Base metal elements anomaly is
controlled by lithology, structure, and topography. Analysis using Pearson's
product on base metal elements states that there are two groups of elements i.e., Au
and Pb-Zn-Cu-Mn. Based on the anomaly distribution of base metal elements in
soil and the presence of mineralization, it can be interpreted that there are four
prospect area i.e., KU-1, KU-2, BE-1, and BE-2 prospects. |
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