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And S-Wave Velocity Structures and the in Uence Of
P- and S-wave Velocity Structures and the Inuence of Volcanic Activities in the East Java Area from Seismic Tomography Syawaldin Ridha Department of Physics, Universitas Brawijaya, Indonesia Sukir Maryanto ( [email protected] ) Universitas Brawijaya https://orcid.org/0000-0002-1882-6818 Agustya A. Martha Meteorological, Climatological, and Geophysical Agency, Indonesia Vanisa Syahra Department of Physics, Universitas Brawijaya, Indonesia Muhajir Anshori Meteorological, Climatological, and Geophysical Agency, Indonesia Pepen Supendi Meteorological, Climatological, and Geophysics Agency, Indonesia Sri Widiyantoro Bandung Institute of Technology: Institut Teknologi Bandung Research Letter Keywords: seismic tomography, East Java, Vp/Vs, Vp, Vs, partial melting Posted Date: May 6th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-438689/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Page 1/24 Abstract Indonesia is one of the most interesting targets for seismic tomographic studies due to its tectonic complexity. The subduction zone was formed when the Indian oceanic plate was subducted beneath the Eurasian continental plate. This activity caused the formation of volcanoes along the Sunda Arc, including the area of East Java. In this study, we aim to identify the inuence of volcanic activities which extends from the west to the east of East Java. We used the data of 1,383 earthquakes, recorded by the 22 stations of the Indonesia Tsunami Early Warning System (InaTEWS) seismic network. We relocated the earthquakes and conducted a tomographic study using SIMULPS12. We then explored the anomalies of P- and S-wave velocities and Vp/Vs ratio. The low-velocity zone was observed in the volcanic area related to the partial melting zone or magma chamber with high Vp/Vs. -
Volcanic Eruption Impacts Student Worksheet
Volcanic Eruption Impacts Student Worksheet Explosive and Effusive Volcanoes The type of volcanic eruption is largely determined by magma composition. Flux-mediated melting at subduction zones creates a felsic magma with high levels of carbon dioxide and water. These dissolved gases explode during eruption. Effusive volcanoes have a hotter, more mafic magma with lower levels of dissolved gas, allowing them to erupt more calmly (effusive eruption). Sinabung (Indonesia) Mount Sinabung is a stratovolcano located 40 km from the Lake Toba supervolcano in North Sumatra. It lies along the Sunda Arc, where the Indo-Australian plate subducts beneath the Sunda and Burma plates. After 1200 years of dormancy, Sinabung began erupting intermittently in 2010. Major eruptions have occurred regularly since November 2013. In November and December 2015, ash plumes reached 6 – 11 km in height on multiple occasions. Pyroclastic flows and ashfall blanketed the region in January 2014 and lava flows travelled down the south flank, advancing 2.5 km by April 2014. Pyroclastic flows in February 2014 killed 17 people in a town 3 km from the vent. In June 2015, ash falls affected areas 10 – 15 km from the summit on many occasions. A lahar in May 2016, caused fatalities in a village 20 km from Sinabung. Pyroclastic flows occurred frequently throughout 2016 and 2017 Eruption of Sinabung 6 October 2016 Major eruptions occurred in 2018 and 2019. In (Y Ginsu, public domain) February 2018, an eruption destroyed a lava dome of 1.6 million cubic metres. At least 10 pyroclastic flows extended up to 4.9 km and an ash plume rose more than 16 km in altitude. -
Title Characteristics of Seismicity Distribution Along the Sunda Arc
Characteristics of Seismicity Distribution along the Sunda Arc: Title Some New Observations Author(s) GHOSE, Ranajit; OIKE, Kazuo Bulletin of the Disaster Prevention Research Institute (1988), Citation 38(2): 29-48 Issue Date 1988-06 URL http://hdl.handle.net/2433/124954 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University Bull. Disas. Prey. Res. Inst., Kyoto Univ., Vol. 38, Part 2, No. 332, June, 1988 29 Characteristics of Seismicity Distribution along the Sunda Arc: Some New Observations By Ranajit GHOSEand Kazuo OIKE (Manuscript received March 7, 1988) Abstract Spatio-temporal variations of earthquake activity along the Sunda arc were investigated. We prepared a strain release map for this century. Adjacent to the zones of high strain release, presence of seismically quiet zones was noted. A careful inspection of the depth distribution of the earthquakes revealed that in the eastern Sunda arc, possibly there exists a zone of scarce seismicity at an interme- diate depth. We discussed the probable implications. We also analysed the patterns of temporal distributions of earthquakes at the three different seismotectonic provinces of the Sunda arc—Sumatra, Java, and the Lesser Sunda Islands. We could clearly see that, although the causative geodynamic situations for seismicity vary significantly in space along the length of the arc, the period of increase or decrease in seismicity is largely space invariant. The locally differing levels of seismicity are superposed on the common background of long period seismicity fluctuation. Finally, clustering of seismicity at some patches along the Sunda arc was studied with respect to the altimetric gravity anomaly data. We noted some apparent conformities. -
Seismic Activity Around and Under Krakatau Volcano, Sunda Arc: Constraints to the Source Region of Island Arc Volcanics
SEISMIC ACTIVITY AROUND AND UNDER KRAKATAU VOLCANO, SUNDA ARC: CONSTRAINTS TO THE SOURCE REGION OF ISLAND ARC VOLCANICS ALEŠ ŠPI ČÁK , VÁCLAV HANUŠ AND JIŘÍ VAN ĚK Geophysical Institute, Academy of Sciences of the Czech Republic, Prague, Czech Republic * ABSTRACT There is general agreement that calc-alkaline volcanic rocks at convergent plate margins are genetically related to the process of subduction (Ringwood, 1974; Maaloe and Petersen, 1981; Hawkesworth et al., 1997). However, opinions on the mode and site of generation of primary magma for island arc volcanism differ substantially. The site of generation of calc-alkaline magma is thought to be either in the mantle wedge (Plank and Langmuir, 1988; McCulloch and Gamble, 1991) or in the subducting slab (White and Dupré, 1986; Defant and Drummond, 1990; Edwards et al., 1993; Ryan and Langmuir, 1993). We present seismological evidence in favour of the latter concept. A distinctive seismicity pattern around and under the Krakatau volcano was identified during systematic studies of the SE Asian convergent plate margins by means of global seismological data. A column-like cluster of events, probably associated with the dynamics of the volcano, is clearly separated from the events in the Wadati-Benioff zone. The accuracy of hypocentral determinations of the events of the cluster does not differ from the accuracy of the events belonging to the subducting slab. The depths of the cluster events vary from very shallow to about 100 km without any apparent discontinuity. On the other hand, there is a pronounced aseismic gap in the Wadati-Benioff zone directly beneath the volcano at depths between 100-150 km. -
Petrogenesis of Rinjani Post-1257-Caldera-Forming-Eruption Lava Flows
Indonesian Journal on Geoscience Vol. 3 No. 2 August 2016: 107-126 INDONESIAN JOURNAL ON GEOSCIENCE Geological Agency Ministry of Energy and Mineral Resources Journal homepage: hp://ijog.geologi.esdm.go.id ISSN 2355-9314, e-ISSN 2355-9306 Petrogenesis of Rinjani Post-1257-Caldera-Forming-Eruption Lava Flows Heryadi Rachmat1,2, Mega Fatimah Rosana1, A. Djumarma Wirakusumah3, and Gamma Abdul Jabbar4 1Faculty of Geology, Padjadjaran University Jln. Raya Bandung - Sumedang Km. 21, Jatinangor, Sumedang, Indonesia 2Geological Agency Jln. Diponegoro No. 57, Bandung, Indonesia 3Energy and Mineral Institute Jln. Gajah Mada, Karangboyo, Cepu, Kabupaten Blora, Indonesia 4Hokkaido University, Kita 10, Nishi 8, Sapporo, Japan Corresponding author: [email protected] Manuscript received: March 7, 2016; revised: May 17, 2016; approved: June 29, 2016; available online: August 2, 2016 Abstract - After the catastrophic 1257 caldera-forming eruption, a new chapter of Old Rinjani volcanic activity began with the appearance of Rombongan and Barujari Volcanoes within the caldera. However, no published petrogenetic study focuses mainly on these products. The Rombongan eruption in 1944 and Barujari eruptions in pre-1944, 1966, 1994, 2004, and 2009 produced basaltic andesite pyroclastic materials and lava flows. A total of thirty-one samples were analyzed, including six samples for each period of eruption except from 2004 (only one sample). The samples were used for petrography, whole-rock geochemistry, and trace and rare earth element analyses. The Rombongan and Barujari lavas are composed of calc-alkaline and high K calc-alkaline porphyritic basaltic andesite. The magma shows narrow variation of SiO2 content that implies small changes during its generation. -
Reconstruction of the 2018 Anak Krakatau Collapse Using Planetscope Imaging and Numerical Modeling
Michigan Technological University Digital Commons @ Michigan Tech Dissertations, Master's Theses and Master's Reports 2020 Reconstruction of the 2018 Anak Krakatau collapse using PlanetScope imaging and numerical modeling Davide Saviano Michigan Technological University, [email protected] Copyright 2020 Davide Saviano Recommended Citation Saviano, Davide, "Reconstruction of the 2018 Anak Krakatau collapse using PlanetScope imaging and numerical modeling", Open Access Master's Thesis, Michigan Technological University, 2020. https://doi.org/10.37099/mtu.dc.etdr/989 Follow this and additional works at: https://digitalcommons.mtu.edu/etdr Part of the Geology Commons, Geomorphology Commons, Tectonics and Structure Commons, and the Volcanology Commons RECONSTRUCTION OF THE 2018 ANAK KRAKATAU COLLAPSE USING PLANETSCOPE IMAGING AND NUMERICAL MODELING By Davide Saviano A THESIS Submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE In Geology MICHIGAN TECHNOLOGICAL UNIVERSITY 2020 © 2020 Davide Saviano This thesis has been approved in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE in Geology. Department of Geological & Mining Engineering & Sciences Thesis Co-Advisor: Dr. Simon A. Carn Thesis Co-Advisor: Dr. Gianluca Groppelli Committee Member: Dr. Roohollah R. Askari Department Chair: Dr. John S. Gierke Table of Contents Abstract ............................................................................................................................... v 1 Introduction .............................................................................................................. -
Java and Sumatra Segments of the Sunda Trench: Geomorphology and Geophysical Settings Analysed and Visualized by GMT Polina Lemenkova
Java and Sumatra Segments of the Sunda Trench: Geomorphology and Geophysical Settings Analysed and Visualized by GMT Polina Lemenkova To cite this version: Polina Lemenkova. Java and Sumatra Segments of the Sunda Trench: Geomorphology and Geophys- ical Settings Analysed and Visualized by GMT. Glasnik Srpskog Geografskog Drustva, 2021, 100 (2), pp.1-23. 10.2298/GSGD2002001L. hal-03093633 HAL Id: hal-03093633 https://hal.archives-ouvertes.fr/hal-03093633 Submitted on 4 Jan 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License ГЛАСНИК Српског географског друштва 100(2) 1 – 23 BULLETIN OF THE SERBIAN GEOGRAPHICAL SOCIETY 2020 ------------------------------------------------------------------------------ --------------------------------------- Original scientific paper UDC 551.4(267) https://doi.org/10.2298/GSGD2002001L Received: October 07, 2020 Corrected: November 27, 2020 Accepted: December 09, 2020 Polina Lemenkova1* * Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Department of Natural Disasters, Anthropogenic Hazards and Seismicity of the Earth, Laboratory of Regional Geophysics and Natural Disasters, Moscow, Russian Federation JAVA AND SUMATRA SEGMENTS OF THE SUNDA TRENCH: GEOMORPHOLOGY AND GEOPHYSICAL SETTINGS ANALYSED AND VISUALIZED BY GMT Abstract: The paper discusses the geomorphology of the Sunda Trench, an oceanic trench located in the eastern Indian Ocean along the Sumatra and Java Islands of the Indonesian archipelago. -
Weak Tectono-Magmatic Relationships Along an Obliquely
Weak Tectono-Magmatic Relationships along an Obliquely Convergent Plate Boundary: Sumatra, Indonesia Valerio Acocella, Olivier Bellier, Laura Sandri, Michel Sébrier, Subagyo Pramumijoyo To cite this version: Valerio Acocella, Olivier Bellier, Laura Sandri, Michel Sébrier, Subagyo Pramumijoyo. Weak Tectono- Magmatic Relationships along an Obliquely Convergent Plate Boundary: Sumatra, Indonesia. Fron- tiers in Earth Science, Frontiers Media, 2018, 6, pp.3. 10.3389/feart.2018.00003. hal-01780318 HAL Id: hal-01780318 https://hal.archives-ouvertes.fr/hal-01780318 Submitted on 27 Apr 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License ORIGINAL RESEARCH published: 09 February 2018 doi: 10.3389/feart.2018.00003 Weak Tectono-Magmatic Relationships along an Obliquely Convergent Plate Boundary: Sumatra, Indonesia Valerio Acocella 1*, Olivier Bellier 2, Laura Sandri 3, Michel Sébrier 4 and Subagyo Pramumijoyo 5 1 Dipartimento di Scienze, Università Roma Tre, Rome, Italy, 2 Aix Marseille -
Sunda Arc Mantle Source δ18O Value Revealed by Intracrystal Isotope
ARTICLE https://doi.org/10.1038/s41467-021-24143-3 OPEN Sunda arc mantle source δ18O value revealed by intracrystal isotope analysis ✉ Frances M. Deegan 1 , Martin J. Whitehouse 2, Valentin R. Troll 1,3, Harri Geiger 1,4, Heejin Jeon2, Petrus le Roux 5, Chris Harris 5, Marcel van Helden6 & Osvaldo González-Maurel 5 Magma plumbing systems underlying subduction zone volcanoes extend from the mantle through the overlying crust and facilitate protracted fractional crystallisation, assimilation, 1234567890():,; and mixing, which frequently obscures a clear view of mantle source compositions. In order to see through this crustal noise, we present intracrystal Secondary Ion Mass Spectrometry (SIMS) δ18O values in clinopyroxene from Merapi, Kelut, Batur, and Agung volcanoes in the Sunda arc, Indonesia, under which the thickness of the crust decreases from ca. 30 km at Merapi to ≤20 km at Agung. Here we show that mean clinopyroxene δ18O values decrease concomitantly with crustal thickness and that lavas from Agung possess mantle-like He-Sr- Nd-Pb isotope ratios and clinopyroxene mean equilibrium melt δ18O values of 5.7 ‰ (±0.2 1 SD) indistinguishable from the δ18O range for Mid Ocean Ridge Basalt (MORB). The oxygen isotope composition of the mantle underlying the East Sunda Arc is therefore largely unaf- fected by subduction-driven metasomatism and may thus represent a sediment-poor arc end-member. 1 Department of Earth Sciences, Natural Resources and Sustainable Development (NRHU), Uppsala University, Uppsala, Sweden. 2 Department of Geosciences, Swedish Museum of Natural History, Stockholm, Sweden. 3 Faculty of Geological Engineering, Universitas Padjajaran (UNPAD), Bandung, Indonesia. 4 Institute of Earth and Environmental Sciences, University of Freiburg, Freiburg, im Breisgau, Germany. -
Tectonic Features of the Southern Sumatra-Western Java Forearc of Indonesia
TECTONICS, VOL. 21, NO. 5, 1047, doi:10.1029/2001TC901048, 2002 Tectonic features of the southern Sumatra-western Java forearc of Indonesia H. U. Schlu¨ter, C. Gaedicke, H. A. Roeser, B. Schreckenberger, H. Meyer, and C. Reichert Bundesanstalt fu¨r Geowissenschaften und Rohstoffe (BGR), Hannover, Germany Y. Djajadihardja Agency for the Assessment and Application of Technology (BPPT), Jakarta, Indonesia A. Prexl Veritas DGC Ltd., Crawley, UK Received 23 November 2001; revised 19 April 2002; accepted 28 May 2002; published 12 October 2002. [1] Multichannel reflection seismic profiles along the Earth: Plate boundary—general (3040); 8158 Tectonophysics: active Sunda Arc, where the Indo-Australian plate Evolution of the Earth: Plate motions—present and recent (3040); subducts under the overriding Eurasian margin 9320 Information Related to Geographic Region: Asia; KEYWORDS: revealed two accretionary wedges: The inner wedge I Indonesia, Sunda forearc, subduction, sediments, seismics, geo- is of assumed Paleogene age, and the outer wedge II is dynamics. Citation: Schlu¨ter H. U., C. Gaedicke, H. A. Roeser, of Neogene to Recent age. The inner wedge I is B. Schreckenberger, H. Meyer, C. Reichert, Y. Djajadihardja, and composed of tectonic flakes stretching from southeast A. Prexl, Tectonic features of the southern Sumatra-western Java forearc of Indonesia, Tectonics, 21(5), 1047, doi:10.1029/ Sumatra across the Sunda Strait to northwest Java, 2001TC901048, 2002. implying a similar plate tectonic regime in these areas at the time of flake development -
Durham Research Online
Durham Research Online Deposited in DRO: 19 February 2014 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Pacey, A. and Macpherson, C.G. and McCarey, K.J.W. (2013) 'Linear volcanic segments in the central Sunda Arc, Indonesia, identied using Hough Transform analysis : implications for arc lithosphere control upon volcano distribution.', Earth and planetary science letters., 369-370 . pp. 24-33. Further information on publisher's website: http://dx.doi.org/10.1016/j.epsl.2013.02.040 Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Earth and planetary science letters. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reected in this document. Changes may have been made to this work since it was submitted for publication. A denitive version was subsequently published in Earth and planetary science letters, 367-370, 2013, 10.1016/j.epsl.2013.02.040 Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. -
Mid-Miocene Volcanic Migration in the Westernmost Sunda Arc Induced by India-Eurasia Collision Yu-Ming Lai1*, Sun-Lin Chung2,3*, Azman A
https://doi.org/10.1130/G48568.1 Manuscript received 25 October 2020 Revised manuscript received 4 January 2021 Manuscript accepted 5 January 2021 © 2021 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 4 March 2021 Mid-Miocene volcanic migration in the westernmost Sunda arc induced by India-Eurasia collision Yu-Ming Lai1*, Sun-Lin Chung2,3*, Azman A. Ghani4, Sayed Murtadha5, Hao-Yang Lee2 and Mei-Fei Chu3 1 Department of Earth Sciences, National Taiwan Normal University, Taipei 11677, Taiwan 2 Institute of Earth Sciences, Academia Sinica, Taipei 11529, Taiwan 3 Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan 4 Department of Geology, University of Malaya, 50603 Kuala Lumpur, Malaysia 5 Department of Geology, Syiah Kuala University, Banda Aceh 23111, Sumatra, Indonesia ABSTRACT zone, however, has attracted little attention. The The migration of arc magmatism that is a fundamental aspect of plate tectonics may reflect Toba caldera that occurs in the transition area the complex interaction between subduction zone processes and regional tectonics. Here we (Fig. 1A) has been a research focus because of report new observations on volcanic migration from northwestern Sumatra, in the westernmost its super-eruptions and environmental impacts Sunda arc, characterized by an oblique convergent boundary between the Indo-Australian (see Chesner [2012] for a review). and Eurasian plates. Our study indicates that in northwestern Sumatra, volcanism ceased at As synthesized by Barber et al. (2005), K-Ar 15–10 Ma on the southern coast and reignited to form a suite of active volcanoes that erupt ages obtained mainly by Bellon et al.