Newcastle University Eprints
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Along the Sumatran Fault System Derived from GNSS
Ito et al. Earth, Planets and Space (2016) 68:57 DOI 10.1186/s40623-016-0427-z LETTER Open Access Co‑seismic offsets due to two earthquakes (Mw 6.1) along the Sumatran fault system derived from GNSS measurements Takeo Ito1* , Endra Gunawan2, Fumiaki Kimata3, Takao Tabei4, Irwan Meilano2, Agustan5, Yusaku Ohta6, Nazli Ismail7, Irwandi Nurdin7 and Didik Sugiyanto7 Abstract Since the 2004 Sumatra–Andaman earthquake (Mw 9.2), the northwestern part of the Sumatran island has been a high seismicity region. To evaluate the seismic hazard along the Great Sumatran fault (GSF), we installed the Aceh GNSS network for the Sumatran fault system (AGNeSS) in March 2005. The AGNeSS observed co-seismic offsets due to the April 11, 2012 Indian Ocean earthquake (Mw 8.6), which is the largest intraplate earthquake recorded in history. The largest offset at the AGNeSS site was approximately 14.9 cm. Two Mw 6.1 earthquakes occurred within AGNeSS in 2013, one on January 21 and the other on July 2. We estimated the fault parameters of the two events using a Markov chain Monte Carlo method. The estimated fault parameter of the first event was a right-lateral strike-slip where the strike was oriented in approximately the same direction as the surface trace of the GSF. The estimated peak value of the probability density function for the static stress drop was approximately 0.7 MPa. On the other hand, the co-seis- mic displacement fields of the second event from nearby GNSS sites clearly showed a left-lateral motion on a north- east–southwest trending fault plane and supported the contention that the July 2 event broke at the conjugate fault of the GSF. -
Buidling Response to Long-Distance Major Earthquakes
13th World Conference on Earthquake Engineering Vancouver, B.C., Canada August 1-6, 2004 Paper No. 804 BUILDING RESPONSE TO LONG-DISTANCE MAJOR EARTHQUAKES T.-C. PAN1, X. T. YOU2 and K. W. CHENG3 SUMMARY Singapore is believed to be located in an aseismic region. However, tremors caused by distant Sumatra earthquakes have reportedly been felt in Singapore for many years. Based on previous studies for Singapore, the maximum credible earthquakes (MCEs) from Sumatra have been hypothesized to be a subduction earthquake (Mw = 9.0) and a strike-slip earthquake (Mw = 7.5). Response at a soft soil site in Singapore to the synthetic bedrock motions corresponding to these maximum credible earthquakes are simulated using a one-dimensional wave propagation method based on the equivalent-linear technique. A typical high-rise residential building in Singapore is analyzed to study its responses subjected to the MCE ground motions at both the rock site and the soft soil site. The results show that the base shear force ratios would exceed the local code requirement on the notional horizontal load for buildings. Because of the large aspect ratio of the floor plan of the typical building, the effects of flexible diaphragms are also included in the seismic response analyses. INTRODUCTION The 1985 Michoacan earthquake, in which a large earthquake (Ms = 8.1) along the coast of Mexico, caused destructions and loss of lives in Mexico City, 350 km away from the epicenter. Learning from the Michoacan earthquake, it has been recognized that urban areas located rather distantly from earthquake sources may not be completely safe from the far-field effects of earth tremors. -
Tsunamigenic Earthquakes
Fifteen Years of (Major to Great) Tsunamigenic Earthquakes F Romano, S Lorito, and A Piatanesi, Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy T Lay, Earth and Planetary Sciences Department, University of California Santa Cruz, Santa Cruz, CA, United States © 2020 Elsevier Inc. All rights reserved. Tsunamis, Seismically Induced 1 Fifteen Years of Major to Great Tsunamigenic Earthquakes 3 The Study of Tsunamigenic Earthquakes 3 Megathrust Tsunamigenic Earthquakes 4 The Sunda 2004–10 Sequence in the Indian Ocean 4 Peru 2007 5 Maule 2010 5 Tohoku 2011 5 Santa Cruz 2013 6 Iquique 2014 6 Illapel 2015 6 Tsunamigenic Doublets 7 Kurils 2006–07 7 Samoa 2009 7 Tsunami Earthquakes 7 Java 2006 8 Mentawai 2010 8 Recent Special Cases 8 Sumatra 2012 8 Solomon 2007 8 Haida Gwaii 2012 9 Kaikoura 2016 9 Mexico 2017 9 Palu 2018 9 Conclusions 10 References 10 Further Reading 12 Tsunamis, Seismically Induced Tsunamis are a series of long gravity waves generated by the displacement of a significant volume of water that propagating in the sea, under the action of the gravity force, returns in its original equilibrium position. Differently from the common wind waves, tsunamis are characterized by large wavelengths (ranging from tens to hundreds of km) and long periods (ranging from minutes to hours). Several natural phenomena such as earthquakes, landslides, volcanic eruptions, the rapid change of atmospheric pressure (meteotsunami), or asteroids impacts can be the source of a tsunami; among these, the most frequent is represented by the earthquakes. Most of the very tsunamigenic earthquakes occur nearby the Earth convergent boundaries (Fig. -
Waves of Destruction in the East Indies: the Wichmann Catalogue of Earthquakes and Tsunami in the Indonesian Region from 1538 to 1877
Downloaded from http://sp.lyellcollection.org/ by guest on May 24, 2016 Waves of destruction in the East Indies: the Wichmann catalogue of earthquakes and tsunami in the Indonesian region from 1538 to 1877 RON HARRIS1* & JONATHAN MAJOR1,2 1Department of Geological Sciences, Brigham Young University, Provo, UT 84602–4606, USA 2Present address: Bureau of Economic Geology, The University of Texas at Austin, Austin, TX 78758, USA *Corresponding author (e-mail: [email protected]) Abstract: The two volumes of Arthur Wichmann’s Die Erdbeben Des Indischen Archipels [The Earthquakes of the Indian Archipelago] (1918 and 1922) document 61 regional earthquakes and 36 tsunamis between 1538 and 1877 in the Indonesian region. The largest and best documented are the events of 1770 and 1859 in the Molucca Sea region, of 1629, 1774 and 1852 in the Banda Sea region, the 1820 event in Makassar, the 1857 event in Dili, Timor, the 1815 event in Bali and Lom- bok, the events of 1699, 1771, 1780, 1815, 1848 and 1852 in Java, and the events of 1797, 1818, 1833 and 1861 in Sumatra. Most of these events caused damage over a broad region, and are asso- ciated with years of temporal and spatial clustering of earthquakes. The earthquakes left many cit- ies in ‘rubble heaps’. Some events spawned tsunamis with run-up heights .15 m that swept many coastal villages away. 2004 marked the recurrence of some of these events in western Indonesia. However, there has not been a major shallow earthquake (M ≥ 8) in Java and eastern Indonesia for the past 160 years. -
An Overview of Heavy Metal Contamination in Coastal Sediments of Sri Lanka A.M.N.M. Adikaram1 and H.M.T.G.A. Pitawala2
Adikaram and Pitawala. /Journal of Tropical Forestry and Environment Vol. 07, No. 02 (2017) 1-13 Feature Article An overview of heavy metal contamination in coastal sediments of Sri Lanka A.M.N.M. Adikaram1 and H.M.T.G.A. Pitawala2 1Department of Physical Sciences, Faculty of Applied Sciences, South Eastern University, Sri Lanka 2Department of Geology, Faculty of Science, University of Peradeniya, Sri Lanka Summary Coastal sediments are often subjected to heavy metal contamination as they reside at the marginal environments of anthropological water releases. These sediments provide the habitat for marine aquatic life of seafood. Therefore, heavy metal contamination in coastal sediments is one of the major environmental concerns. The coastal belt of Sri Lanka is highly urbanized with high population (59% of Sri Lankan population) and is mostly depend on the sea. Therefore, anthropogenic inputs of pollutants in to the marine environments have been increased during last decades. Heavy metal contamination of the coastal sediments of Sri Lanka has been discussed by several studies, focusing on selected coastal regions. In this article, previous studies have been reviewed in order to understand the contamination status and ecological risks due to heavy metal accumulations. Despite the sampling location, the elemental distribution of coastal lagoonal sediments shows similar trend indicating the dominance of natural elemental sources rather the anthropogenic influences. The concentrations of As and Cr in sediments are high compared to the upper continental crust values which is a characteristic feature in possible source rocks, soils and sediments of Sri Lanka. The results of the previous studies indicate that coastal sediments are low to moderately contaminated but not at ecological risk. -
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. -
Using a Genetic Algorithm to Estimate the Details of Earthquake Slip Distributions from Point Surface Displacements
Edinburgh Research Explorer Using a genetic algorithm to estimate the details of earthquake slip distributions from point surface displacements Citation for published version: Lindsay, A, McCloskey, J & Bhloscaidh, MN 2016, 'Using a genetic algorithm to estimate the details of earthquake slip distributions from point surface displacements', Journal of Geophysical Research. Solid Earth, vol. 121, no. 3, pp. 1796-1820. https://doi.org/10.1002/2015JB012181 Digital Object Identifier (DOI): 10.1002/2015JB012181 Link: Link to publication record in Edinburgh Research Explorer Document Version: Publisher's PDF, also known as Version of record Published In: Journal of Geophysical Research. Solid Earth General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 06. Oct. 2021 PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Using a genetic algorithm to estimate the details 10.1002/2015JB012181 of earthquake slip distributions -
Regional Seismic Hazard Posed by the Mentawai Segment of the Sumatran Megathrust by Kusnowidjaja Megawati and Tso-Chien Pan
Bulletin of the Seismological Society of America, Vol. 99, No. 2A, pp. 566–584, April 2009, doi: 10.1785/0120080109 Regional Seismic Hazard Posed by the Mentawai Segment of the Sumatran Megathrust by Kusnowidjaja Megawati and Tso-Chien Pan Abstract Several lines of evidence have indicated that the Mentawai segment of the Sumatran megathrust is very likely to rupture within the next few decades. The present study is to investigate seismic hazard and risk levels at major cities in Sumatra, Java, Singapore, and the Malay Peninsula caused by the potential giant earthquakes. Three scenarios are considered. The first one is an Mw 8.6 earthquake rupturing the 280 km segment that has been locked since 1797; in the second scenario, rupture oc- curs along a 600 km segment covering the combined rupture areas of the 1797 and 1833 historical events, producing an Mw 9.0 earthquake; and the third scenario has the same rupture area as the second scenario but with doubled slip amplitude, resulting in an Mw 9.2 earthquake. Simulation results indicate that ground motions produced by the hypothetical scenarios are strong enough to cause yielding to medium- and high- rise buildings in many major cities in Sumatra. It is vital to ensure that the overall strength, stiffness, and integrity of the structures are maintained throughout the entire duration of shaking. However, the ductile detailing in current practice is formulated based on an assumption that ground motions would last from 20 to 40 sec. This has not been tested for longer durations of 3–5 min, expected from giant earthquakes. -
Segmentation of Sumatran Fault Zone in Tanggamus District, Lampung
Segmentation of Sumatran Fault Zone in Tanggamus District, Lampung based on GPS Displacement and SRTM Data Satrio Muhammad Alifa, M Ilvan Ardiansyaha, Syafei Wiyonoa aGeomatics Engineering Department, Institut Teknologi Sumatera, Lampung Selatan, Lampung *Corresponding E-mail: [email protected] Abstract: Sumatran Fault is one of hazard located in Sumatra Island. Southern segment of Sumatran fault is one of sources of earthquakes in Lampung Province. Hazard map is used as consideration in developing region. The source of hazard comes from stress accumulation of crust which can be derived from movement of points in surface. The study of determining fault location which is source of hazard is important for sustainable development in Lampung Province. The source of hazard is southern segment of Sumatran fault which stretched on Tanggamus, Lampung in south end of Sumatra Island. Tanggamus District has capital in Kota Agung, one of cities with oldest civilization in Lampung Province so that its natural landscape had sedimentated. It causes the delineation of Sumatran Fault Zone by using Digital Terrain Model conducted on previous research had the flaw. This study uses GPS Displacement Data as tool to determine the location of fault beside Shuttle Radar Topography Mission (SRTM) Data and seismic activity. SRTM Data which is conditional equivalent with Digital Terrain Model has 30 meter resolution and measured in 2018. Seismic activity used in this research is obtained from USGS from last 100 years. Seismic activity used as support data to determine whether the fault delineated with SRTM and GPS displacement is active. GPS displacement is calculated from GPS coordinates measured periodically from 2006 to 2019. -
India and Sunda Plates Motion and Deformation Along Their Boundary In
India and Sunda plates motion and deformation along their boundary in Myanmar determined by GPS Anne Socquet, Christophe Vigny, Nicolas Chamot-Rooke, Wim Simons, Claude Rangin, Boudewijn Ambrosius To cite this version: Anne Socquet, Christophe Vigny, Nicolas Chamot-Rooke, Wim Simons, Claude Rangin, et al.. India and Sunda plates motion and deformation along their boundary in Myanmar determined by GPS. Jour- nal of Geophysical Research : Solid Earth, American Geophysical Union, 2006, 111 (B5), pp.B05406. 10.1029/2005JB003877. hal-01793657 HAL Id: hal-01793657 https://hal-ens.archives-ouvertes.fr/hal-01793657 Submitted on 16 May 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. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, B05406, doi:10.1029/2005JB003877, 2006 India and Sunda plates motion and deformation along their boundary in Myanmar determined by GPS Anne Socquet,1,2 Christophe Vigny,1 Nicolas Chamot-Rooke,1 Wim Simons,3 Claude Rangin,4 and Boudewijn Ambrosius3 Received 8 June 2005; revised 12 January 2006; accepted 15 February 2006; published 6 May 2006. [1] Using a regional GPS data set including 190 stations in Asia, from Nepal to eastern Indonesia and spanning 11 years, we update the present-day relative motion between the Indian and Sundaland plates and discuss the deformation taking place between them in Myanmar. -
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 -
The Tectonic Framework of the Sumatran Subduction Zone
ANRV374-EA37-15 ARI 23 March 2009 12:21 The Tectonic Framework of the Sumatran Subduction Zone Robert McCaffrey Earth and Environmental Sciences, Rensselaer Polytechnic Institute, Troy, New York 12180; email: [email protected] Annu. Rev. Earth Planet. Sci. 2009. 37:345–66 Key Words by University of California - San Diego on 06/16/09. For personal use only. First published online as a Review in Advance on Sumatra, subduction, earthquake, hazards, geodesy December 4, 2008 The Annual Review of Earth and Planetary Sciences is Abstract Annu. Rev. Earth Planet. Sci. 2009.37:345-366. Downloaded from arjournals.annualreviews.org online at earth.annualreviews.org The great Aceh-Andaman earthquake of December 26, 2004 and its tragic This article’s doi: consequences brought the Sumatran region and its active tectonics into the 10.1146/annurev.earth.031208.100212 world’s focus. The plate tectonic setting of Sumatra has been as it is today Copyright c 2009 by Annual Reviews. for tens of millions of years, and catastrophic geologic events have likely All rights reserved been plentiful. The immaturity of our understanding of great earthquakes 0084-6597/09/0530-0345$20.00 and other types of geologic hazards contributed to the surprise regarding the location of the 2004 earthquake. The timing, however, is probably best understood simply in terms of the inevitability of the infrequent events that shape the course of geologic progress. Our best hope is to improve under- standing of the processes involved and decrease our vulnerability to them. 345 ANRV374-EA37-15 ARI 23 March 2009 12:21 INTRODUCTION The island of Sumatra (Figure 1) forms the western end of the Indonesian archipelago and until recently was perhaps best known to the world for its coffee, though perhaps not so much as Java, its neighbor to the east.