ENRICHMENT POTENTIAL OF TIN AND RARE EARTH ELEMENTS IN PLACER DEPOSIT IN SIMPANG PESAK, EAST BELITUNG REGENCY
The study area is located at 823865 – 827977 mE dan 9653722 – 9658725 mS UTM coordinate, Simpang Pesak District, East Belitung Regency, Bangka Belitung Province. The aims of this research are to determine the potential areas of tin and rare earth elements in placer deposits and to provide recomme...
Saved in:
Main Author: | |
---|---|
Format: | Final Project |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/70435 |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | The study area is located at 823865 – 827977 mE dan 9653722 – 9658725 mS UTM
coordinate, Simpang Pesak District, East Belitung Regency, Bangka Belitung
Province. The aims of this research are to determine the potential areas of tin and
rare earth elements in placer deposits and to provide recommendations for further
exploration stages. The research uses primary data such as rock samples and
placer deposit samples.
The analysis of the placer deposits sample was divided into three-grain size
fractions, #48 fraction (297-354 ?m), #100 fraction (149 ?m), and -100 fraction
(<149 ?m). Geochemical data from placer deposit concentrate and rock samples
analyzed by using X-Ray Fluorescence (XRF) Portable to determine the content
value of tin and rare earth elements. Univariate statistic analysis is performed to
determine anomaly value based on the content value of tin and rare earth elements.
Mineral content in placer deposit samples can be identified by using Grain
Counting Analysis (GCA). The rare earth elements that were found in the study
area including yttrium, cerium, and lantanum.
Tin with high content distributed in the southern part and some in the middle of the
study area. REE with high content distributed in the middle of the study area. The
tin and REE anomalies area concentrated in old alluvial placer deposits. There are
three factors that affect the presence of these anomalies area such as forming
process, source rocks, and morphology of the enrichment area. Further exploration
can be done from the western part towards the southeast and then heading to the
north towards the granite area. |
---|