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INDONESIA
BULLETIN OF THE MARINE GEOLOGY
Published by Marine Geological Institute of Indonesia
ISSN : 14106175     EISSN : 25278843     DOI : -
Core Subject : Science,
Earth & Planetary Sciences
Bulletin of the Marine Geology is a scientific journal of Marine geoscience that is published periodically, twice a year (June and December). The publication identification could be recognized on the ISSN 1410-6175 (print) and e-ISSN: 2527-8843 (on-line) twice a year (June & December) and it has been accredited by Lembaga Ilmu Pengetahuan Indonesia (Indonesian Institute of Sciences) by Decree Number: 818/E/2015. As an open access journal, thus all content are freely available without any charge to the user. Users are allowed to download, and distribute the full texts of the articles without permission from the publisher.
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Articles 5 Documents
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Search results for , issue "Vol 31, No 2 (2016)" : 5 Documents clear
Rare Earth Elements Vapor Transport By Fumaroles in the Post Caldera Complex of Weh Island Submarine Volcano, Aceh Province Northern Sumatra Hananto Kurnio; Ediar Usman
BULLETIN OF THE MARINE GEOLOGY Vol 31, No 2 (2016)
Publisher : Marine Geological Institute of Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3017.456 KB) | DOI: 10.32693/bomg.31.2.2016.317

Abstract

Research found out that fumaroles and solfataras are rare earth element (REE) vapor transport agents in Weh Island submarine volcano – Aceh. Shallow high resolution single channel seismic was used to map the distribution of seafloor fumaroles surrounding the submarine volcano. Samples of REE depositions were taken from Jaboi geothermal field, and mineralization zone at Pria Laot coast; as well as seafloor surrounding active fumaroles by divers.  Rare earth elements (REE) were analysed using ICP – MS (inductively coupled plasma – mass spectrometry) with detection limits ranged from 0.05 to 0.1 ppm (part per million).The central part of Weh submarine volcano is the most active REE deposition. This area is build by normal faults and grabens oriented north – south of open character which acted as channel for hydrothermal fluids reaching seafloor surface.Some REE abundances such as La, Ce, Pr, and Nd due to its location in the central of hydrothermal activity. This proximity explains such abundances of this andesitic component sample of agglomerate.  Keywords: REE, vapor transport, fumaroles, Weh Island, Aceh.Penelitian mendapatkan bahwa fumarole dan solfatara adalah sebagai agen transportasi uap Logam Tanah Jarang (LTJ) di gunungapi bawah laut Pulau Weh – Aceh, Provinsi Nanggroe Aceh Darussalam (NAD). Seismik saluran tunggal dangkal resolusi tinggi digunakan untuk memetakan fumarole dasarlaut di sekitar gunungapi bawah laut tersebut.Bagian tengah gunungapi bawah laut Pulau Weh merupakan area paling aktif pengendapan LTJ. Bagian ini dibangun oleh sesar-sesar normal dan graben berorientasi utara – selatan dengan karakter terbuka sebagai saluran untuk fluida hidrotermal mencapai permukaan dasar laut.Kelimpahan unsur tanah jarang La, Ce, Pr dan Nd dikarenakan posisinya pada pusat aktivitas hidrotermal. Kedekatan dengan pusat hidrotermal ini menjelaskan kelimpahan REE dari contoh komponen andesitic yang diambil dari aglomerat ini.Kata kunci: UTJ (Unsur Tanah Jarang), transportasi uap, fumarol, PulauWeh, Aceh.
Geological Structures Appearances and Its Relation to Mechanism of Arc-Continent Collision Northen Alor-Wetar Islands Subarsyah Subarsyah; Riza Rahardiawan
BULLETIN OF THE MARINE GEOLOGY Vol 31, No 2 (2016)
Publisher : Marine Geological Institute of Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2864.767 KB) | DOI: 10.32693/bomg.31.2.2016.326

Abstract

Study area is located in South Banda Basin near the triple junction between Eurasian, Pacific and Indo-Australian Plates. This area is part of back-arc thrusting zone that evolved to compensate convergence between Australia Continent and Banda Arc. Based on seismic section in this area, geological structure analysis is characterized into three distinctive zones. There are Thrust Zone (TZ), Proto Thrust Zone (PTZ) and Normal Fault Zone (NFZ). TZ is defined by distribution of numerous of thrust fault, PTZ contains a blind zone or folds instead of thrust fault, and NFZ defined by distribution of numerous normal fault in the upper portion of seismic section. PTZ identified at several seismic section along the bending zone of oceanic crust. The appearances of bending zone will be easily understood by comprehend the driving mechanism of Australia Continent to the Northeast. The bending zone also related to geometry and tectonic stress of collision. Based on this mechanism it was clearly understood why the western end of study area was not identified the bending zone but it probably the initial process of bending. Contradictive to the western end, the eastern part was clearly shown the bending zone that assumed to have the biggest tectonic stress at this moment. Map of structural analysis also explain that PTZ getting narrow towards the west as the indicator of less of tectonic stress.Keywords: Arc-Continent Collision, Proto Thrust Zone, Wetar, Back arc Thrusting, Banda Sea. Lokasi penelitian berada pada Cekungan Banda Selatan sekitar area triple junction antara Lempeng Eurasia, Pasifik dan Indo-Australia.Daerah ini merupakan bagian dari zona back-arc thrusting yang berkembang sebagai kompensasi dari konvergensi antara kontinen Austalia dan Busur Banda.Berdasarkan penampang seismik di daerah ini analisis struktur geologi dikelompokan kedalam tiga zona. Tiga zona tersebut meliputi Thrust Zone (TZ), Proto Thrust Zone (PTZ) and Normal Fault Zone (NFZ). TZ didefinisikan oleh distribusi dari sejumlah sesar naik, PTZ mengandung sejumlah blind thrust atau lipatan pengganti sesar naik dan NFZ didefinisikan oleh distribusi dari sejumlah sesar normal pada bagian atas dari penampang seismik. PTZ teridentifikasi pada beberapa penampang seismic sepanjang zona bending dari lempeng oseanik. Kenampakan dari zona bending akan mudah dipahami dengan mengetahui mekanisme pergerakan dari kontinen Australia ke arah timurlaut. Zona ini umumnya berhubungan dengan bentuk geometri dan besaran dari tectonic stress dari tumbukan. Berdasarkan mekanisme ini dapat dipahami dengan jelas mengapa bagian ujung barat dari daerah penelitian tidak teridentifikasi zona bending. Kontradiktif terhadap ujung barat, ujung timur memperlihatkan zona bending yang sangat jelas yang diperkirakan mempunyai tectonic stress yang paling besar pada saat ini. Peta dari analisis struktur juga menjelaskan bahwa zona PTZ semakin ke arah barat semakin menyempit sebagai indicator dari berkurangnya tectonic stress.Kata Kunci: Tumbukan Busur-Kontinen, Proto Thrust Zone, Wetar, Back arc Thrusting, Banda Sea.
The Study of Seafloor Tin Placer Resources of Quaternary Sediment at Toboali Waters, South Bangka Muhammad Zulfikar; Noor CD Aryanto
BULLETIN OF THE MARINE GEOLOGY Vol 31, No 2 (2016)
Publisher : Marine Geological Institute of Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3115.513 KB) | DOI: 10.32693/bomg.31.2.2016.285

Abstract

Bangka Island has primary and secondary tin deposit. However, along the history of tin mining has been done the primary tin deposit domination is less than secondary tin deposit. Secondary tin deposit is formed from Granitic S-type source rock weathering and then transported by gravity. After that, Cassiterite mineral (SnO2) accumulates and forms a placer deposit in the study area. The thickness of sediment cover at Toboali Waters is quite diverse, with a range between 5-20 milliseconds, by knowing the quarter sediment thickness using seismic data interpretation results, is expected to give an idea about tin placer deposit potential in Toboali waters. Based on the Isochron map shows patterns of quaternary sediment thickening to the southwest, south and southeast of Bangka Island.Keywords: Quaternary sediment, placer deposit, isochron map, Toboali WatersPulau Bangka memiliki endapan timah primer dan endapan timah sekunder. Namun, sepanjang sejarah penambangan timah yang telah dilakukan endapan timah primer tidak mendominasi jika dibandingkan dengan endapan timah sekunder. Pembentukan endapan timah sekunder berawal dari pelapukan batuan Granit tipe-S yang kemudian mengalami transportasi akibat adanya gravitasi. Setelah itu, mineral kasiterit (SnO2) terakumulasi dan membentuk endapan plaser di daerah penelitian. Ketebalan sedimen penutup di Perairan Toboali berkisar antara 5-20 milidetik, dengan mengetahui ketebalan sedimen kuarter berdasarkan interpretasi data hasil rekaman seismik diharapkan dapat memberikan gambaran tentang potensi endapan timah placer di Perairan Toboali. Berdasarkan atas peta isokron, memperlihatkan bahwa pola penebalan sedimen kuater ke arah baratdaya, selatan dan tenggara Pulau Bangka.Kata kunci : Sedimen kuarter, endapan placer, peta isokron, Perairan Toboali
Tsunami Potential Due To Strike-Slip Earthquake Affected by Submarine Landslide Wiko Setyonegoro
BULLETIN OF THE MARINE GEOLOGY Vol 31, No 2 (2016)
Publisher : Marine Geological Institute of Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1851.66 KB) | DOI: 10.32693/bomg.31.2.2016.283

Abstract

The most of earthquakes in the western part of North of Sumatra, Indonesia have tsunami potential. This paper discuss about tsunami height which was triggered by large energy of earthquake along strike-slip fault and submarine landslide. Beyond of a view historical tsunamis in the western part Sumatra in Aceh, which was occured on April 11, 2012 have given several questions for the majority of earth scientist in relation with the potential for tsunami. The 8.6 M earthquake might have no tsunami potential significantly, with the hypothesis that mechanism of the earthquake source is strike-slip. However BMKG, in accordance with standard operating procedures stated that this earthquake "potential tsunami". But here we will give other parameters that affect a potential tsunami by performing the calculation of the effects of landslides. This paper describes how potential and kinetic energy spread during landslide and analysis of mechanism and underwater structures named as guyot as the cause of the earthquake along strike-slip fault. This paper discuss about scoup study on landslide which give the hypothesis that the type of submarine landslide or landslide of near shore cliff also will have influence to tsunami height or run-up. The key is, how strongly the all of disturbance above will increasing or decreasing of  sea water volume. The result for the first case, strike-slip earthquake without the submarine landslide obtain maximum run-up in Meulaboh  is 1.5864 m, with E~Mo (seafloor deformation). For the second case is strike-slip earthquake influenced by submarine landslide obtained ETotal ~1020 ~ Mo (seafloor deformation) which obtained tsunami run-up in Meulaboh 1.7726 m. So in this case, the landslide under the sea it also affected to the maximum tsunami height, but not significantly influence. For the last case, strike-slip earthquake influenced by landslide of near shore cliff: ETotal is estimated Ekfall ~  1022  ~  Mw ~  8 SR, equivalent with vertical of seafloor deformation and obtain tsunami run-up in Meulaboh 16.9372 m.Keywords: tsunami run-up, fault, strike-slip, submarine landslide, uppper the sea landslide, potential energy, kinetic energySebagian besar gempabumi yang terjadi pada area barat Sumatera Indonesia berpotensi tsunami. Tulisan ini memodelkan kemungkinan ketinggian tsunami yang dipicu oleh gempabumi dengan energi besar sepanjang sesar geser yang dipengaruhi oleh longsoran bawah laut. Gempabumi dengan kekuatan 8,6 Mw pada 11 April 2012 yang terjadi di bagian barat Sumatera telah menimbulkan kepanikan akan tetapi tidak menimbulkan bencana tsunami besar karena terjadi di sepanjang sesar geser kerak Samudera Hindia. Berdasarkan pemodelan, gempabumi sepanjang sesar geser dapat memicu tsunami besar bilamana diikuti oleh longsoran bawah laut. Tujuan dari penelitian ini adalah untuk memodelkan propagasi gelombang tsunami dengan proses mekanisme gempabumi strike-slip yang dipengaruhi oleh kondisi batimetri, volume struktur, jumlah dan jenis tanah longsor bawah laut yang dapat memicu ketinggian gelombang tsunami. Perhitungan dan pemodelan ini melibatkan simulasi energi potensial dan energi kinetik yang mempengaruhi ketinggian gelombang tsunami pada garis pantai. Hasil pemodelan pertama, dengan anggapan gempabumi sesar geser yang tidak dipengaruhi oleh proses longsor bawah laut menghasilkan ketinggian tsunami di Meulaboh 1,5864 m, dengan E ~ Mo (deformasi dasar laut). Untuk kasus pemodelan kedua dengan anggapan gempabumi sesar geser disertai oleh longsoran di bawah permukaan laut diperoleh Etotal ~ 1020 ~ Mo (deformasi dasar laut) yang menghasilkan ketinggian tsunami di Meulaboh 1,7726 m. Untuk pemodelan ketiga, gempabumi sesar geser yang diikuti oleh longsoran di tebing dekat pantai dengan Etotal diperkirakan Ekfall ~ 1022 ~ Mw ~ 8 SR setara dengan jenis mekanisme deformasi vertikal yang dapat menghasilkan ketinggian gelombang tsunami di Meulaboh sampai dengan 16,9372 m. Kata Kunci: run-up tsunami, sesar geser, longsoran bawah laut, longsoran diatas permukaan laut, energi potensial, energi kinetik
Calcareous Nannoplankton (marine algae) Analysis in Subsurface Sediments of Andaman Sea Marfasran Hendrizan; Rainer Arief Troa; Eko Triarso; Rina Zuraida; Shengfa Liu
BULLETIN OF THE MARINE GEOLOGY Vol 31, No 2 (2016)
Publisher : Marine Geological Institute of Indonesia

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1509.875 KB) | DOI: 10.32693/bomg.31.2.2016.313

Abstract

Andaman Sea in the Indo-Pacific Warm Pool (IPWP) is influenced by Indo-Australia monsoon winds. Marine sediment cores in this area, BS36 (06°55’50.8”N; 96°07’28.51”E; ; Water depth 1147.1 meters) were acquired by Geomarin III research vessel andanalysed its morphology for nannoplankton occurences. Results from qualitative identification on marine sediment core in Andaman Sea obtained 11 genus of nannoplankton marine algae in this area. Dominated genus discovered in this site is Gephyrocapsa, Emiliania, and Helicosphaera. Although this research is qualitative and preliminary study phase; however, this reference of modern nannoplankton taxonomy and features using Scanning Electron Microscope (SEM) would enhance marine algae biodiversity along Andaman Sea of Indonesian watersKeywords: Nannoplankton, morphology, sediment core, taxonomy, Andaman Sea Kawasan Laut Andaman terletak di wilayah kolam panas Indo-Pasifik sangat dipengaruhi oleh angin musim Indo-Australia. Conto inti sedimen laut di wilayah BS 36 (06°55’50.8” Utara; 96°7’28.51” Timur; kedalaman laut 1147,1 meter) diambil menggunakan wahana kapal riset Geomarin III dan dianalisis morfologi nanoplankton yang ditemukan di wilayah ini. Hasil dari pemerian kualitatif dari conto sedimen inti di Laut Andaman menghasilkan 11 genus nanoplankton sebagai alga laut yang dapat ditemukan pada lokasi ini. Genus yang sangat menonjol di satu lokasi titik pengambilan conto sedimen inti yaitu Gephyrocapsa, Emiliania, dan Helicosphaera. Meskipun kajian ini masih bersifat kualitatif dan tahap studi awal; namun acuan tentang taksonomi nanoplankton modern dan kenampakan dari Scanning Electron Microscope (SEM) akan memperkaya biodivesitas alga laut di sepanjang Laut Andaman dari perairan Indonesia.Kata Kunci: Nanoplankton, morfologi, conto sedimen inti, taxonomi, Laut Andaman

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