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Relevant bibliographies by topics / Geology of Sumatra

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Academic literature on the topic 'Geology of Sumatra'

Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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Journal articles on the topic "Geology of Sumatra"

1

Syuaib Intan, Muhammad Fadhlan. "Geologi situs paleolitik das kikim, kabupaten lahat, provinsi sumatra selatan." KALPATARU 26, no. 2 (2018): 73. http://dx.doi.org/10.24832/kpt.v26i2.273.

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Lahat is one of the districts within the province of South Sumatra, the site of research, saving many cultural remains, one of them from the paleolithic period, which for so long received no attention from environmental researchers. This is the basis of the main problems that cover geology in general. Therefore, the purpose of this study is to conduct surface geology mapping in general as an effort to present geological information, while the aim is to know the geomorphological aspects, stratigraphy, geological structures associated with existence in paleolithic sites of research area. The res

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2

Li, Shan, Sun-Lin Chung, Yu-Ming Lai, Azman A. Ghani, Hao-Yang Lee, and Sayed Murtadha. "Mesozoic juvenile crustal formation in the easternmost Tethys: Zircon Hf isotopic evidence from Sumatran granitoids, Indonesia." Geology 48, no. 10 (2020): 1002–5. http://dx.doi.org/10.1130/g47304.1.

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Abstract Prior to the collision of India with Asia, the evolution of island arcs and resultant crustal formation in the now-disrupted easternmost Tethys are poorly constrained. Here, we report for the first time zircon U-Pb and Hf isotopic data from Mesozoic granitoids in Sumatra, Indonesia. Our analyses identified three magmatic episodes at 214–201 Ma, 148–143 Ma, and 102–84 Ma, respectively, with a drastic change in magmatic zircon εHf(t) values from −13.1 to +17.7 in the Late Triassic granitoids, which reveals a fundamental restructuring of the arc system in Sumatra. Subsequently, all Juras

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Crow, M. J., and A. J. Barber. "Map: Structural map of Sumatra." Geological Society, London, Memoirs 31, no. 1 (2005): NP.3—NP. http://dx.doi.org/10.1144/gsl.mem.2005.031.01.18.

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4

Van Gorsel, J. T. (Han), and Bernhard Gunzenhauser. "August Tobler, the Swiss Pioneer of South Sumatra Geological Mapping, 1900-1912." Berita Sedimentologi 47, no. 1 (2021): 63–78. http://dx.doi.org/10.51835/bsed.2021.47.1.54.

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Dr. August Tobler was a well-known Swiss geologist, who, as one of the very first petroleum field geologists in the Netherlands Indies, did more than ten years of geological mapping in the tiger-infested jungles of South Sumatra. He first worked for the Koninklijke/Royal Dutch and Moeara Enim oil companies in South Sumatra from 1900 to 1904. This was followed by six more years of geological mapping in the Jambi basin, as the first non-Dutch geoscientist at the Dienst van het Mijnwezen (Geological Survey). His thoroughly documented monographs and geologic maps of his geological fieldwork in the

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Crow, M. J., and A. J. Barber. "Map: Simplified geological map of Sumatra." Geological Society, London, Memoirs 31, no. 1 (2005): NP.2—NP. http://dx.doi.org/10.1144/gsl.mem.2005.031.01.17.

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6

Bellon, Hervé, René C. Maury, Sutanto, Rubini Soeria-Atmadja, Joseph Cotten, and Mireille Polvé. "65 m.y.-long magmatic activity in Sumatra (Indonesia), from Paleocene to Present." Bulletin de la Société Géologique de France 175, no. 1 (2004): 61–72. http://dx.doi.org/10.2113/175.1.61.

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Abstract Sumatra is the largest volcanic island of the Indonesian archipelago. The oblique subduction of the Indian Ocean lithosphere below the Sundaland margin is responsible for the development of a NW-SE trending volcanic arc, the location of which coincides approximately with the Great Sumatran Fault Zone (GSFZ). We present in this paper ca. 80 new 40K-40Ar ages measured on Cenozoic calc-alkaline to shoshonitic magmatic rocks sampled all along this arc from Aceh to Lampung. The results show that magmatic activity started during the Paleocene (ca. 63 Ma) all along the arc, and was more or l

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7

Hochstein, M. P., and Sayogi Sudarman. "Geothermal resources of Sumatra." Geothermics 22, no. 3 (1993): 181–200. http://dx.doi.org/10.1016/0375-6505(93)90042-l.

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8

Damanik, Muhammad Ridha Syafii, Ali Nurman, Muhammad Yuliansyah Aminy, and Ilham Ritonga. "Analisis Potensi Longsor Sungai di Daerah Aliran Sungai (DAS) Padang Sumatera Utara." Tunas Geografi 8, no. 2 (2020): 141. http://dx.doi.org/10.24114/tgeo.v8i2.16139.

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AbstractThe occurrence of flash floods in 2017 that hit Tebing Tinggi City in North Sumatra Province caused 33,825 lives to be affected. That shows that the potential for flash floods disasters in the North Sumatra region, including in the Padang River Basin, is classified as very high. The purpose of this study is to determine the location of potential riverbank landslides that cause river flow obstructions (natural dams) in the Padang River Basin. The method used in this study is a qualitative method using geographic information systems. The data analysis technique used is the cone stacking

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9

OKAL, E. A., H. M. FRITZ, and A. SLADEN. "2004 SUMATRA-ANDAMAN TSUNAMI SURVEYS IN THE COMORO ISLANDS AND TANZANIA AND REGIONAL TSUNAMI HAZARD FROM FUTURE SUMATRA EVENTS." South African Journal of Geology 112, no. 3-4 (2009): 343–58. http://dx.doi.org/10.2113/gssajg.112.3-4.343.

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10

Kopp, H., W. Weinrebe, S. Ladage, et al. "Lower slope morphology of the Sumatra trench system." Basin Research 20, no. 4 (2008): 519–29. http://dx.doi.org/10.1111/j.1365-2117.2008.00381.x.

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Dissertations / Theses on the topic "Geology of Sumatra"

1

Wajzer, Marek Roman. "The geology and tectonics of the Woyla Group, Natal Area, North Sumatra." Thesis, Royal Holloway, University of London, 1986. http://repository.royalholloway.ac.uk/items/452e1d33-ee8d-4678-997c-bc85eac06a27/1/.

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The Batang Natal River flows across the Western Barisan Mountains of North Sumatra, exposing a section through the Woyla Group, a major unit of Sumatran island arc basement. Detailed field mapping of the section, followed up by thin section petrology, structural analysis and radiometric dating, was undertaken in order to investigate the geology, structure, origin and tectonic evolution of the Woyla Group. The Woyla Group outcropping in the section is divided into eighteen lithotectonic units, each with distinctive lithological characteristics, including basalts, volcanogenic turbidites and deb

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2

Collings, Rachel Elizabeth. "The Sumatra subduction zone : seismicity, velocity structure and seismic anisotropy." Thesis, University of Liverpool, 2012. http://livrepository.liverpool.ac.uk/7233/.

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On September 12 2007, an Mw 8.4 earthquake occurred within the southern section of the Mentawai segment of the Sumatra subduction zone, where the subduction thrust had previously ruptured in 1833 and 1797. Following the 2007 rupture, a temporary local network was installed in the Mentawai region between December 2007 and October 2008 to record the aftershocks. Additionally, a second network was installed in central Sumatra between April 2008 and February 2009. In this study the data obtained from the Mentawai network were used to determine 2D and 3D Vp and Vp/Vs models, first motion polarity f

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3

Jobson, David Hamilton. "Genesis of the gold-bearing breccia bodies at the Lebong Tandai Mine, Sumatra." Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.241251.

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4

Nukman, Mochamad [Verfasser], Wilhelm [Akademischer Betreuer] Dominik, and Inga [Akademischer Betreuer] Moeck. "Geothermal exploration involving structural geology and hydrochemistry in the Tarutung Basin, Northern Central Sumatra (Indonesia) / Mochamad Nukman. Gutachter: Inga Moeck. Betreuer: Wilhelm Dominik." Berlin : Technische Universität Berlin, 2014. http://d-nb.info/1065669704/34.

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Pethe, Swardhuni. "Subsurface analysis of Sundaland basins : source rocks, structural trends and the distribution of oil fields." 2013. http://liblink.bsu.edu/uhtbin/catkey/1741652.

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According to the Ade observation (Ade, W., pers. Comm.) “95% of all commercial oil fields in the Sumatra region occur within 17 km of seismically mappable structural grabens in the producing basins”. The Ade observation proposes a link between the subsidence of the source rocks (the Talang Akar Formation) in the grabens and the maturity of the organic material. To test the validity of the Ade observation, subsurface mapping of the region was carried out using geophysical logs. Using the well log information, the basement and the formation tops have been mapped with a special emphasis on Talang

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Onasanya, Sherifat Olayemi. "Geological evaluation of a part of the Jambi Trough, Sumatra, Indonesia." 2013. http://liblink.bsu.edu/uhtbin/catkey/1741650.

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The research involves mapping of subsurface at a scale of 1:25,000 the top of three geological formations in the Southern Part of Sumatra – the Airbenakat Formation, the top of the Talangakar Formation, and the top of structural basement in the Jambi Trough. Isopach maps of the formations will be constructed. These maps will form the basis of a basin analysis and hydrocarbon source rock assessment of the Jambi Trough using Basin Mod basin modeling software (Rockworks Software). The studies utilize the L. Bogue Hunt Southeast Asia database housed in the Department of Geological Sciences at Ball

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7

Muskin. "Understanding the seismic structure beneath Sumatra and its surrounding regions." Master's thesis, 2010. http://hdl.handle.net/1885/150636.

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The main objective of this research is to understand the seismic structure beneath Sumatra and its surrounding regions by using seismic tomography. The structure is interpreted as P wavespeed velocity anomalies relative to the ak135 model. The main data source is P wave traveltimes up to 2006 obtained from the International Seismological Centre with relocation using the EHB scheme. Summary rays are constructed for these ISC data to decrease the number of data and to give a more even rays distribution so that we obtain 1,750,070 ISC residuals. We also include arrivals reported to Geoscience Aus

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Andrade, Vanessa Mary Rachel. "Seismotectonics Of The Andaman-Nicobar Plate Boundary And Evaluation Of 2004 Deformational And Depositional Features Towards Assessing Past Tsunamigenic Earthquakes." Thesis, 2012. http://hdl.handle.net/2005/2548.

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Tsunami hazards were greatly underestimated along the coasts of countries bordering the northeastern Indian Ocean until the occurrence of the 26 December 2004, Mw 9.2 earthquake and its ensuing tsunami. Sourced off the coast of northern Sumatra, on the plate boundary between the Indo-Australian and Eurasian plates, the rupture of the 2004 earthquake propagated ~1300 km northward. The magnitude of this earthquake and the reach of its tsunami exceeded all known precedents, based on instrumental and historic records. The coseismic deformational and post-tsunami depositional features facilitated o

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Books on the topic "Geology of Sumatra"

1

Fontaine, Henri. The pre-Tertiary fossils of Sumatra and their environments. Issued by CCOP Technical Secretariat, 1989.

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2

Gupta, Harsh K. Three Great Tsunamis: Lisbon (1755), Sumatra-Andaman (2004) and Japan (2011). Springer Netherlands, 2013.

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3

Simandjuntak, T. O. Evolusi tektonik pra-tersier Sumatera bagian Selatan. Departemen Pertambangan dan Energi, Direktorat Jenderal Geologi dan Sumberdaya Mineral, Pusat Penelitian dan Pengembangan Geologi, 2000.

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4

PT, Trimikon Barasakti. Laporan pemetaan geologi dan pemboran daerah KP eksplorasi KW.25.02.LHT.2008 PT Bima Putra Abadi Citranusa di Kecamatan Merapi Selatan, Kabupaten Lahat, Propinsi Sumatera Selatan. Trimikon Barasakti, 2009.

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5

Volz, Wilhelm. Zur Geologie Von Sumatra: Beobachtungen und Studien. Creative Media Partners, LLC, 2018.

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6

(Editor), A. J. Barber, M. J. Crow (Editor), and J. S. Milsom (Editor), eds. Sumatra: Geology, Resources and Tectonic Evolution (Geological Society Memoirs). Geological Society of London, 2005.

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7

Geological Survey (U.S.), ed. Mineralogical and microstructural investigations of core samples from the vicinity of the Great Sumatran Fault, Indonesia. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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Book chapters on the topic "Geology of Sumatra"

1

Wikarno, D. A. D. Suyatna, and S. Sukardi. "Granitoids of Sumatra and the Tin Islands." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_44.

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2

Johari, S. "Geochemistry and Tin Mineralization in Northern Sumatra, Indonesia." In Geology of Tin Deposits in Asia and the Pacific. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72765-8_42.

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3

Orihara, Keiji, Tomohiro Yasuda, Koji Nishida, Koki Kimura, Achmad Sri Fadli, and Reza Ardiansyah Suyono. "Geological investigation of the excavation-induced landslide in a geothermal area in Sumatra, Indonesia." In Rock Mechanics and Engineering Geology in Volcanic Fields. CRC Press, 2022. http://dx.doi.org/10.1201/9781003293590-9.

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4

Ito, Hisatoshi. "Resurgent magma characteristics of a super-volcano, the Youngest Toba Tuff, northern Sumatra, inferred from zircon U-Pb geochronology." In Rock Mechanics and Engineering Geology in Volcanic Fields. CRC Press, 2022. http://dx.doi.org/10.1201/9781003293590-8.

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5

Soehaimi, Asdani, Dicky Muslim, Ir Kamawan, and Robby Setia Negara. "Microzonation of the Liwa City on the Great Sumatera Active Fault and Giant Ranau Volcanic Complex in South Sumatera, Indonesia." In Engineering Geology for Society and Territory - Volume 5. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_194.

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6

Umar, Zahrul, Anuar Ahmad, and Wan Aziz Wan Akib. "Prediction of Susceptible Areas of Future Earthquake Induced by Landslides in Padang Pariaman District, West Sumatera, Indonesia." In Engineering Geology for Society and Territory - Volume 2. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_121.

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7

"Geotech and Geology." In Padang, West Sumatra, Indonesia, Earthquake of 2009. American Society of Civil Engineers, 2013. http://dx.doi.org/10.1061/9780784412930.ch02.

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8

Matson, Richard G., and Gregory F. Moore. "Structural Influences on Neogene Subsidence in the Central Sumatra Fore-Arc Basin." In Geology and Geophysics of Continental Margins. American Association of Petroleum Geologists, 1992. http://dx.doi.org/10.1306/m53552c10.

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9

Subekty, A. D., and Sandra G. Neuzil. "General geology and peat resources of the Siak Kanan and Bengkalis Island peat deposits, Sumatra, Indonesia." In Geological Society of America Special Papers. Geological Society of America, 1993. http://dx.doi.org/10.1130/spe286-p45.

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10

Jaya, Bagus. "S Wave Velocity Structure in Non-Tectonic SE Asia by Seismogram Analysis of the Earthquakes in Sumatra-Java at TATO Station, Taiwan." In Earthquake Research and Analysis - Seismology, Seismotectonic and Earthquake Geology. InTech, 2012. http://dx.doi.org/10.5772/27283.

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Conference papers on the topic "Geology of Sumatra"

1

Zhang, Ming, Longxin Mu, Chunlei Li, et al. "Mature Condensated Gas Field Development Strategy: An Integration of Geophysics, Geology and Log for the South Sumatra Basin, Indonesia." In SPE Reservoir Characterisation and Simulation Conference and Exhibition. Society of Petroleum Engineers, 2017. http://dx.doi.org/10.2118/186060-ms.

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2

Livsey, A. "Petroleum Systems Analysis of The Tungkal PSC Area, South Sumatra – A Means of Adding New Life to A Mature Area." In Digital Technical Conference. Indonesian Petroleum Association, 2020. http://dx.doi.org/10.29118/ipa20-g-399.

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South Sumatra is considered a mature exploration area, with over 2500MMbbls of oil and 9.5TCF of gas produced. However a recent large gas discovery in the Kali Berau Dalam-2 well in this basin, highlights that significant new reserve additions can still be made in these areas by the re-evaluation of the regional petroleum systems, both by identification of new plays or extension of plays to unexplored areas. In many mature areas the exploration and concession award history often results in successively more focused exploration programmes in smaller areas. This can lead to an increased emphasis

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3

Nugroho, Susanto Budi, Yedi Hartono, and Reza Nur Ardianto. "Integrated Geology, Geophysics and Petrophysics Data to Describe Lateral and Vertical Reservoir Heterogeneity to Optimize Field Development Plan Limau Field, South Sumatra Basin, Indonesia." In International Oil and Gas Conference and Exhibition in China. Society of Petroleum Engineers, 2010. http://dx.doi.org/10.2118/130653-ms.

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Lamis, N. M. "A Cohesive Approach in Identifying a Missed-pay of Carbonate Reservoir in a Brownfield." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-207.

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L Field is a brownfield located in the South Sumatra Basin with numerous producing wells. Adjacent to this field, there is a large carbonate reservoir with a significant recovery factor. Carbonate is found in L Field but it was deposited in distal environment with different characters. In attempt to prolong the life of L Field, its carbonate reservoir is evaluated. An integration between geology, petrophysics, reservoir and production engineering works has been done to get comprehensive results. The evaluation was put into 2 categories, qualitative and quantitative methods. The qualitative met

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