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Identifikasi Struktur Geologi dan Petrografi di sekitar Observatorium Astronomi Lampung Gunung Betung

Journal of Science and Applicative Technology · Vol. 4 No. 2 (2020)

DOI
10.35472/jsat.v4i2.265
ISSN
2581-0545
Terbit
2020-12-20
Penerbit
Institut Teknologi Sumatra

Abstrak

Lampung Astronomical Observatory (LAO) is located on Betung Mountain which is quite close to the Semangko active fault zone. Betung Mountain is part of the Bukit Barisan which is located west of the city of Bandar Lampung. This mountain has an altitude of about 1200 meters above sea level. There are 6 interesting stations. Most of the stations are located on the upper slopes of Betung Mountain. In the Talang Aji area, there are 2 springs. The other 4 stations consist of waterfalls with varying heights: Talang Teluk waterfall (30 m), Talang Rabun waterfall (20 m), Betung waterfall consists of two minor terraced waterfalls with a height of 5 and 10 m respectively, and Kubu Jambu waterfall (12 m). In general, the orientation of the faults of Mt. Betung was northeast-southwest. The faults are also associated with several waterfalls found in the field. From the joint data processing, it can be interpreted that the fault formed on Betung Mountain is normal. The lithology of Betung Mountain is dominated by volcanic deposits in the form of tuffs. In certain rivers, there are outcrops of lava igneous rock in the form of Andesites. Andesite lava in the northern and southern parts of Betung Mountain has different characteristics.

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Erlangga IbrahimAfiliasi tidak diketahui3
Hikhmadhan GultafAfiliasi tidak diketahui3
Virgian RahmandaAfiliasi tidak diketahui3
M. R. P. SudibyoAfiliasi tidak diketahui3
Reza RizkiAfiliasi tidak diketahui3
nirmawana SimarmataAfiliasi tidak diketahui2
Zulfikar Adlan NadzirAfiliasi tidak diketahui2
La Ode ArhamAfiliasi tidak diketahui1
Fika Rofiek MufakhirAfiliasi tidak diketahui1
Muhammad SafriAfiliasi tidak diketahui1
Rosyani RosyaniAfiliasi tidak diketahui1
Amalia ZahraBinus University1
Fathur RahmanAfiliasi tidak diketahui1
Faldi FaldiAfiliasi tidak diketahui1
Ferry Fadzlul RahmanAfiliasi tidak diketahui1
Sayekti HaritsAfiliasi tidak diketahui1
Wawan Joko PranotoAfiliasi tidak diketahui1
Rinaldi RinaldiAfiliasi tidak diketahui1
Khusnul Setia WardaniNational Research and Innovation Agency1
Koichi YamamotoAfiliasi tidak diketahui1
Sigit SutiknoAfiliasi tidak diketahui1
Muhamad YusaAfiliasi tidak diketahui1
Ahmad MuhammadAfiliasi tidak diketahui1
Muhammad Ario Eko RahadiantoAfiliasi tidak diketahui1
Ratna Mustika SariAfiliasi tidak diketahui1
Choirun Nisa NabilaAfiliasi tidak diketahui1

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Sumber metadata: Crossref API (cadangan, berdasarkan ISSN) https://api.crossref.org/journals/2581-0545/works, pertama di-harvest 5 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata sebagai oai_dc, dikonversi dari Crossref
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/"><dc:title>Identifikasi Struktur Geologi dan Petrografi di sekitar Observatorium Astronomi Lampung Gunung Betung</dc:title><dc:creator>Saputra, Hendra</dc:creator><dc:creator>Siringorongo, Luhut P.</dc:creator><dc:creator>Suhendi, Cahli</dc:creator><dc:creator>Agustina, Lea Kristi</dc:creator><dc:description>&lt;jats:p&gt;Lampung Astronomical Observatory (LAO) is located on Betung Mountain which is quite close to the Semangko active fault zone. Betung Mountain is part of the Bukit Barisan which is located west of the city of Bandar Lampung. This mountain has an altitude of about 1200 meters above sea level. There are 6 interesting stations. Most of the stations are located on the upper slopes of Betung Mountain. In the Talang Aji area, there are 2 springs. The other 4 stations consist of waterfalls with varying heights: Talang Teluk waterfall (30 m), Talang Rabun waterfall (20 m), Betung waterfall consists of two minor terraced waterfalls with a height of 5 and 10 m respectively, and Kubu Jambu waterfall (12 m). In general, the orientation of the faults of Mt. Betung was northeast-southwest. The faults are also associated with several waterfalls found in the field. From the joint data processing, it can be interpreted that the fault formed on Betung Mountain is normal. The lithology of Betung Mountain is dominated by volcanic deposits in the form of tuffs. In certain rivers, there are outcrops of lava igneous rock in the form of Andesites. Andesite lava in the northern and southern parts of Betung Mountain has different characteristics.&lt;/jats:p&gt;</dc:description><dc:publisher>Institut Teknologi Sumatra</dc:publisher><dc:date>2020-12-20</dc:date><dc:type>info:eu-repo/semantics/article</dc:type><dc:format>application/pdf</dc:format><dc:identifier>https://doi.org/10.35472/jsat.v4i2.265</dc:identifier><dc:identifier>10.35472/jsat.v4i2.265</dc:identifier><dc:source>Journal of Science and Applicative Technology; Vol 4 No 2 (2020); 91</dc:source><dc:source>2581-0545</dc:source><dc:relation>https://journal.itera.ac.id/index.php/jsat/article/download/265/123</dc:relation></oai_dc:dc>