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Regional Lineament Pattern and Morphotectonic Analysis: The Investigation of Geological Structures and Present-Time Relative Tectonic Activity in the Tin Granite Area of Belitung Island, Indonesia

JURNAL GEOCELEBES · Vol. 8 No. 1 (2024) · pp. 83–97

DOI
10.20956/geocelebes.v8i1.33887
ISSN
2579-5546, 2579-5821
Published
2024-04-29
Publisher
Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar
Language
en

Abstract

Belitung Island is located on the East Coast of Sumatra and is the southernmost extension of the Southeast Asian granite belt. Despite the flat terrain of the island, numerous granite outcrops provide insight into the past tectonic activities that caused the uplift in the region. This study analyzes the current state of Belitung's tectonic activity by examining its morphotectonic index and lineament pattern. A National Digital Elevation Model (DEMNAS) dataset with a resolution of up to 8.1 m will be used to assess the geological patterns and relative tectonic activity from the surface. The relationship between the regional lineament system and morphotectonic quantification throughout the landforms of Belitung Island will also be considered. The modified Segmented Tracing Algorithm (m-STA) technique extracted the lineament features. The Index of Relative Active Tectonic (IATR) was calculated by averaging several morphotectonic indices, such as asymmetry factors (AF), stream-length index (SL), mountain-front sinuosity (Smf), and valley floor width-height ratio (VF) factors, to quantify the relative tectonic activity of the area. The combination of the two methods shows that Belitung is currently experiencing relatively weak tectonic activity compared to the past. This is supported by the surface appearance, which is mainly composed of lowlands. Several granite outcrops and highlands are aligned along the NW-SE and NE-SW directions, corresponding to the main geological structures in the area.

Keywords

Collaboration network of the authors

18 authors · 36 co-authorship links

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Co-authorOrganisationJoint articles
Muh Resky AriansyahAffiliation unknown1
Novita Reskiyah SariAffiliation unknown1
Muh Reza PahleviAffiliation unknown1
Bambang HarimeiAffiliation unknown1
Syamsuddin SyamsuddinAffiliation unknown1
Muhammad NasriAffiliation unknown1
Marcelino N. YonasAffiliation unknown1
Harsan Ingot HasudunganAffiliation unknown1
Rahmat IndrajatiAffiliation unknown1
Harnanti Y. HutamiAffiliation unknown1
Nova Triyani SiagianAffiliation unknown1
Egie WijaksonoAffiliation unknown1
Chikita Mery YulianiAffiliation unknown1
Renita Dwi VadilaAffiliation unknown1
Mokhammad Puput ErlanggaAffiliation unknown1

Affiliations come from OpenAlex; journal OAI-PMH metadata carries none. Authors without an OpenAlex ID are matched by name, which can merge or split people.

Metadata source: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/geocelebes/oai, first harvested 3 Nov 2026, last seen 3 Nov 2026.
Original metadata (oai_dc)
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	<dc:title xml:lang="en">Regional Lineament Pattern and Morphotectonic Analysis: The Investigation of Geological Structures and Present-Time Relative Tectonic Activity in the Tin Granite Area of Belitung Island, Indonesia</dc:title>
	<dc:creator xml:lang="en">Hutami, Harnanti Yogaputri</dc:creator>
	<dc:creator xml:lang="en">Anas, Nur Ayu</dc:creator>
	<dc:creator xml:lang="en">Fattah, Erlangga Ibrahim</dc:creator>
	<dc:subject xml:lang="en">lineament</dc:subject>
	<dc:subject xml:lang="en">morphotectonic index</dc:subject>
	<dc:subject xml:lang="en">relative tectonic activity</dc:subject>
	<dc:subject xml:lang="en">structural geology</dc:subject>
	<dc:description xml:lang="en">Belitung Island is located on the East Coast of Sumatra and is the southernmost extension of the Southeast Asian granite belt. Despite the flat terrain of the island, numerous granite outcrops provide insight into the past tectonic activities that caused the uplift in the region. This study analyzes the current state of Belitung's tectonic activity by examining its morphotectonic index and lineament pattern. A National Digital Elevation Model (DEMNAS) dataset with a resolution of up to 8.1 m will be used to assess the geological patterns and relative tectonic activity from the surface. The relationship between the regional lineament system and morphotectonic quantification throughout the landforms of Belitung Island will also be considered. The modified Segmented Tracing Algorithm (m-STA) technique extracted the lineament features. The Index of Relative Active Tectonic (IATR) was calculated by averaging several morphotectonic indices, such as asymmetry factors (AF), stream-length index (SL), mountain-front sinuosity (Smf), and valley floor width-height ratio (VF) factors, to quantify the relative tectonic activity of the area. The combination of the two methods shows that Belitung is currently experiencing relatively weak tectonic activity compared to the past. This is supported by the surface appearance, which is mainly composed of lowlands. Several granite outcrops and highlands are aligned along the NW-SE and NE-SW directions, corresponding to the main geological structures in the area.</dc:description>
	<dc:publisher xml:lang="en">Departemen Geofisika, FMIPA - Universitas Hasanuddin, Makassar</dc:publisher>
	<dc:date>2024-04-29</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Peer-reviewed Article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.unhas.ac.id/index.php/geocelebes/article/view/33887</dc:identifier>
	<dc:identifier>10.20956/geocelebes.v8i1.33887</dc:identifier>
	<dc:source xml:lang="en">JURNAL GEOCELEBES; Vol. 8 No. 1: April 2024; 83–97</dc:source>
	<dc:source>2579-5546</dc:source>
	<dc:source>2579-5821</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/geocelebes/article/view/33887/11426</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2024 JURNAL GEOCELEBES</dc:rights>
</oai_dc:dc>