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Subduction Initiation May Depend on a Tectonic Plate's History 22 June 2021, by David Shultz
Subduction initiation may depend on a tectonic plate's history 22 June 2021, by David Shultz geological history makes it an ideal location to study how subduction starts. The team's seismic structural analysis showed that subduction zone initiation begins along existing weaknesses in Earth's crust and relies on differences in lithospheric density. The conditions necessary for the subduction zone's formation began about 45 million years ago, when the Australian and Pacific plates started to pull apart from each other. During that period, extensional forces led to seafloor spreading and the creation of new high-density oceanic lithosphere in the south. However, in the north, the thick and buoyant continental crust of Zealandia was merely stretched and slightly thinned. Over the next several million years, the plates rotated, and strike- The Puysegur Trench follows the natural curvature of slip deformation moved the high-density oceanic New Zealand’s South Island, extending southwest from lithosphere from the south to the north, where it the island’s southern tip. Credit: NASA slammed into low-density continental lithosphere, allowing subduction to begin. Subduction zones are cornerstone components of The researchers contend that the differences in plate tectonics, with one plate sliding beneath lithospheric density combined with existing another back into Earth's mantle. But the very weaknesses along the strike-slip boundary from the beginning of this process—subduction previous tectonic phases facilitated subduction initiation—remains somewhat mysterious to initiation. The team concludes that strike-slip might scientists because most of the geological record of be a key driver of subduction zone initiation subduction is buried and overwritten by the because of its ability to efficiently bring together extreme forces at play. -
Geophysical Structure of the Southern Alps Orogen, South Island, New Zealand
Regional Geophysics chapter 15/04/2007 1 GEOPHYSICAL STRUCTURE OF THE SOUTHERN ALPS OROGEN, SOUTH ISLAND, NEW ZEALAND. F J Davey1, D Eberhart-Phillips2, M D Kohler3, S Bannister1, G Caldwell1, S Henrys1, M Scherwath4, T Stern5, and H van Avendonk6 1GNS Science, Gracefield, Lower Hutt, New Zealand, [email protected] 2GNS Science, Dunedin, New Zealand 3Center for Embedded Networked Sensing, University of California, Los Angeles, California, USA 4Leibniz-Institute of Marine Sciences, IFM-GEOMAR, Kiel, Germany 5School of Earth Sciences, Victoria University of Wellington, Wellington, New Zealand 6Institute of Geophysics, University of Texas, Austin, Texas, USA ABSTRACT The central part of the South Island of New Zealand is a product of the transpressive continental collision of the Pacific and Australian plates during the past 5 million years, prior to which the plate boundary was largely transcurrent for over 10 My. Subduction occurs at the north (west dipping) and south (east dipping) of South Island. The deformation is largely accommodated by the ramping up of the Pacific plate over the Australian plate and near-symmetric mantle shortening. The initial asymmetric crustal deformation may be the result of an initial difference in lithospheric strength or an inherited suture resulting from earlier plate motions. Delamination of the Pacific plate occurs resulting in the uplift and exposure of mid- crustal rocks at the plate boundary fault (Alpine fault) to form a foreland mountain chain. In addition, an asymmetric crustal root (additional 8 - 17 km) is formed, with an underlying mantle downwarp. The crustal root, which thickens southwards, comprises the delaminated lower crust and a thickened overlying middle crust. -
SEASAT Geoid Anomalies and the Macquarie Ridge Complex Larry Ruff *
Physics of the Earth and Planetary Interiors, 38 (1985) 59-69 59 Elsevier Science Publishers B.V., Amsterdam - Printed in The Netherlands SEASAT geoid anomalies and the Macquarie Ridge complex Larry Ruff * Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109 (U.S.A.) Anny Cazenave CNES-GRGS, 18Ave. Edouard Belin, Toulouse, 31055 (France) (Received August 10, 1984; revision accepted September 5, 1984) Ruff, L. and Cazenave, A., 1985. SEASAT geoid anomalies and the Macquarie Ridge complex. Phys. Earth Planet. Inter., 38: 59-69. The seismically active Macquarie Ridge complex forms the Pacific-India plate boundary between New Zealand and the Pacific-Antarctic spreading center. The Late Cenozoic deformation of New Zealand and focal mechanisms of recent large earthquakes in the Macquarie Ridge complex appear consistent with the current plate tectonic models. These models predict a combination of strike-slip and convergent motion in the northern Macquarie Ridge, and strike-slip motion in the southern part. The Hjort trench is the southernmost expression of the Macquarie Ridge complex. Regional considerations of the magnetic lineations imply that some oceanic crust may have been consumed at the Hjort trench. Although this arcuate trench seems inconsistent with the predicted strike-slip setting, a deep trough also occurs in the Romanche fracture zone. Geoid anomalies observed over spreading ridges, subduction zones, and fracture zones are different. Therefore, geoid anomalies may be diagnostic of plate boundary type. We use SEASAT data to examine the Maequarie Ridge complex and find that the geoid anomalies for the northern Hjort trench region are different from the geoid anomalies for the Romanche trough. -
The Age and Origin of Miocene-Pliocene Fault Reactivations in the Upper Plate of an Incipient Subduction Zone, Puysegur Margin
RESEARCH ARTICLE The Age and Origin of Miocene‐Pliocene Fault 10.1029/2019TC005674 Reactivations in the Upper Plate of an Key Points: • Structural analyses and 40Ar/39Ar Incipient Subduction Zone, Puysegur geochronology reveal multiple fault reactivations accompanying Margin, New Zealand subduction initiation at the K. A. Klepeis1 , L. E. Webb1 , H. J. Blatchford1,2 , R. Jongens3 , R. E. Turnbull4 , and Puysegur Margin 5 • The data show how fault motions J. J. Schwartz are linked to events occurring at the 1 2 Puysegur Trench and deep within Department of Geology, University of Vermont, Burlington, VT, USA, Now at Department of Earth Sciences, University continental lithosphere of Minnesota, Minneapolis, MN, USA, 3Anatoki Geoscience Ltd, Dunedin, New Zealand, 4Dunedin Research Centre, GNS • Two episodes of Late Science, Dunedin, New Zealand, 5Department of Geological Sciences, California State University, Northridge, Northridge, Miocene‐Pliocene reverse faulting CA, USA resulted in short pulses of accelerated rock uplift and topographic growth Abstract Structural observations and 40Ar/39Ar geochronology on pseudotachylyte, mylonite, and other Supporting Information: fault zone materials from Fiordland, New Zealand, reveal a multistage history of fault reactivation and • Supporting information S1 uplift above an incipient ocean‐continent subduction zone. The integrated data allow us to distinguish • Table S1 true fault reactivations from cases where different styles of brittle and ductile deformation happen • Figure S1 • Table S2 together. Five stages of faulting record the initiation and evolution of subduction at the Puysegur Trench. Stage 1 normal faults (40–25 Ma) formed during continental rifting prior to subduction. These faults were reactivated as dextral strike‐slip shear zones when subduction began at ~25 Ma. -
50 Archaeological Salvage at El Chiquirín, Gulf Of
50 ARCHAEOLOGICAL SALVAGE AT EL CHIQUIRÍN, GULF OF FONSECA, LA UNIÓN, EL SALVADOR Marlon Escamilla Shione Shibata Keywords: Maya archaeology, El Salvador, Gulf of Fonseca, shell gatherers, Salvage archaeology, Pacific Coast, burials The salvage archaeological investigation at the site of El Chiquirín in the department of La Unión was carried out as a consequence of an accidental finding made by local fishermen in November, 2002. An enthusiast fisherman from La Unión –José Odilio Benítez- decided, like many other fellow countrymen, to illegally migrate to the United States in the search of a better future for him and his large family. His major goal was to work and save money to build a decent house. Thus, in September 2002, just upon his arrival in El Salvador, he initiated the construction of his home in the village of El Chiquirín, canton Agua Caliente, department of La Unión, in the banks of the Gulf of Fonseca. By the end of November of the same year, while excavating for the construction of a septic tank, different archaeological materials came to light, including malacologic, ceramic and bone remains. The finding was much surprising for the community of fishermen, the Mayor of La Unión and the media, who gave the finding a wide cover. It was through the written press that the Archaeology Unit of the National Council for Culture and Art (CONCULTURA) heard about the discovery. Therefore, the Archaeology Unit conducted an archaeological inspection at that residential place, to ascertain that the finding was in fact a prehispanic shell deposit found in the house patio, approximately 150 m away from the beach. -
Developing Community-Based Scientific Priorities and New Drilling
Workshop Reports Sci. Dril., 24, 61–70, 2018 https://doi.org/10.5194/sd-24-61-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Developing community-based scientific priorities and new drilling proposals in the southern Indian and southwestern Pacific oceans Robert McKay1, Neville Exon2, Dietmar Müller3, Karsten Gohl4, Michael Gurnis5, Amelia Shevenell6, Stuart Henrys7, Fumio Inagaki8,9, Dhananjai Pandey10, Jessica Whiteside11, Tina van de Flierdt12, Tim Naish1, Verena Heuer13, Yuki Morono9, Millard Coffin14, Marguerite Godard15, Laura Wallace7, Shuichi Kodaira8, Peter Bijl16, Julien Collot17, Gerald Dickens18, Brandon Dugan19, Ann G. Dunlea20, Ron Hackney21, Minoru Ikehara22, Martin Jutzeler23, Lisa McNeill11, Sushant Naik24, Taryn Noble14, Bradley Opdyke2, Ingo Pecher25, Lowell Stott26, Gabriele Uenzelmann-Neben4, Yatheesh Vadakkeykath24, and Ulrich G. Wortmann27 1Antarctic Research Centre, Victoria University of Wellington, Wellington, 6140, New Zealand 2Research School of Earth Sciences, Australian National University, Canberra, 0200, Australia 3School of Geosciences, The University of Sydney, Sydney, NSW2006, Australia 4Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, 27568 Bremerhaven, Germany 5California Institute of Technology, Pasadena, CA 91125, USA 6College of Marine Science, University of South Florida, Saint Petersburg, FL 33701, USA 7GNS Science, Lower Hutt, 5040, New Zealand 8Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama 236-0001, -
Universidad De El Salvador. Facultad Multidisciplinaria
UNIVERSIDAD DE EL SALVADOR. FACULTAD MULTIDISCIPLINARIA ORIENTAL. DEPARTAMENTO DE CIENCIAS Y HUMANIDADES. SECCIÓN DE LETRAS. TEMA: ―LITERATURA POPULAR Y EXPRESIONES ARTÍSTICAS DEL MUNICIPIO DE CONCHAGUA, DEPARTAMENTO DE LA UNIÓN, DURANTE EL AÑO 2010.‖ PRESENTADO POR: BR. SÁNCHEZ CASTILLO, JUDITH DEL CARMEN. BR. REYES TORRES, EMILIA DEL CARMEN. BR. CAMPOS GÓMEZ, JOSÉ ORLANDO. TRABAJO DE GRADO PARA OPTAR AL TÍTULO DE: LICENCIADO EN LETRAS. DOCENTE DIRECTOR: LIC. RUBÉN EDGARDO SÁNCHEZ TORRES. OCTUBRE DE 2010. SAN MIGUEL, EL SALVADOR, CENTRO AMÉRICA ÍNDICE INTRODUCCIÓN ........................................................................................................... 9i CAPÍTULO I. PLANTEAMIENTO DEL PROBLEMA. ........................................... 11 CAPÍTULO II. JUSTIFICACIÓN. ............................................................................... 14 CAPÍTULO III. OBJETIVOS. ...................................................................................... 15 3.1 OBJETIVO GENERAL. ..................................................................................... 15 3.3 OBJETIVOS ESPECÍFICOS. ............................................................................. 15 CAPÍTULO IV. MARCO DE REFERENCIA. ............................................................ 16 4.1 ANTECEDENTES HISTÓRICOS. .................................................................... 16 4.2 FUNDACIÓN U ORÍGEN DE LA CIUDAD DE CONCHAGUA. .................. 16 4.3 TOPONÍMIA. .................................................................................................... -
Presentation on Pacific Plate and Associated Boundaries
PACIFIC PLATE AND ASSOCIATED BOUNDARIES The Pacific Plate • Pacific Plate is the largest plate and an oceanic plate. • It shares its boundaries with numerous plates namely; North American Plate.(Convergent and transform fault) Philippine Plate.(Convergent) Juan de Fuca Plate.(Convergent) Indo – Australian Plate.(Convergent, Transform Fault) Cocos Plate.(Divergent) Nazca Plate.(Divergent) Antarctic Plate.(Divergent,Transform Fault) Types of Plate Boundaries • Convergent Boundary: Subduction zones where two plates converges. Eg; Aleutian Islands(Alaska) • Divergent Boundary: Spreading centres where two plates move away from each other. Eg; East Pacific Rise (MOR, Pacific Ocean). • Transform Faults: Boundary where two plates slide past each other. For Eg. ; San Andreas Fault. BOUNDARY WITH ANTARCTIC PLATE DIVERGENT BOUNDARY • Pacific – Antarctic Ridge TRANSFORM FAULT • Louisville Seamount Chain Pacific – Antarctic Ridge Pacific – Antarctic Ridge(PAR) is located on the seafloor of the South Pacific Ocean. It is driven by the interaction of a mid oceanic ridge and deep mantle plumes located in the eastern portion of East Pacific Ridge. Louisville Seamount Chain It is the longest line of seamount chain in the Pacific Ocean of about 4,300 km, formed along the transform boundary in the western side between Pacific plate and Antarctic plate. It was formed from the Pacific Plate sliding over a long – lived centre of upwelling magma called the Louisville hotspot. BOUNDARY WITH PHILIPPINE PLATE CONVERGENT BOUNDARY • Izu – Ogasawara Trench • Mariana Trench Izu – Ogasawara Trench It is an oceanic trench in the western Pacific Ocean. It stretches from Japan to northern most section of Mariana Trench. Here, the Pacific Plate is being subducted beneath the Philippine Sea Plate. -
Thallium Isotopes As Tracers of Recycled Materials in Subduction
1 2 Thallium isotopes as tracers of recycled materials in subduction 3 zones: review and new data for lavas from Tonga-Kermadec and 4 Central America 5 6 7 Sune G. Nielsen1,2, Julie Prytulak3, Jerzy Blusztajn1,2, Yunchao Shu1,2,4,5, Maureen Auro1,2, Marcel 8 Regelous6 and Jim Walker7 9 10 1NIRVANA Laboratories, Woods Hole Oceanographic Institution, Woods Hole, MA, USA 11 2Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA 12 3Department of Earth Science and Engineering, Imperial College London, UK 13 4Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China 14 5University of Chinese Academy of Sciences, Beijing, China 15 6GeoZentrum Nordbayern, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, Germany 16 7Department of Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL, USA 17 1 18 Abstract - Sediment is actively being subducted in every convergent margin worldwide. 19 Yet, geochemical data for arc lavas from several subduction zones, such as Northern Tonga and 20 Costa Rica have revealed either attenuated or limited evidence for sediment in their mantle 21 source regions. Here we use thallium (Tl) isotopes to trace slab components in lavas from the 22 Tonga-Kermadec and Central American arcs. In general, both arcs display Tl isotope data that 23 are most compatible with addition of sediment to the sub-arc mantle from the subducting slab. 24 This evidence is particular strong in the Tonga-Kermadec arc where pelagic clays dominate the 25 Tl budget along the entire arc. Contributions from altered oceanic crust as well as the Louisville 26 Seamount chain that subducts underneath Northern Tonga are not visible in Tl isotopes, which is 27 likely due to the very high Tl concentrations found in pelagic sediments outboard of the Tonga- 28 Kermadec arc. -
Pdf Completo
ANÁLISIS DE RIESGO NATURALES DE LA SUBREGION LA UNION --------------------------------------------------------------------------------------------------------------------------------------------------------- INDICE 1. CARACTERIZACON Y DIAGNOSTICO 1.1. Características Generales. 1.1.1. Características de la Región. 1.1.2. Identificación y delimitación 1.2. Características Biofísicas 1.2.1. Geomorfología 1.2.2. Suelos 1.2.3. Clima 1.2.4. Hidrología 1.2.5. Amenazas naturales 1.2.6. Biodiversidad 1.3. Características socio-económicos 1.3.1. Demografía 1.3.2. Empleo e ingresos 1.3.3. Pobreza 1.3.4. Educación 1.3.5. Salud 1.3.6. Turismo 1.3.7 Infraestructura y servicios 2. ANÁLISIS Y ESCENARIOS DE RIESGOS 2.1 Consideraciones para el Análisis de Riesgos. 2.2 Mapas de Escenarios 2.3 Aspectos teóricos del riesgo 2.4. Riesgos de la Subregión 2.4.1.Deslizamientos 2.4.1.1. Riesgos por deslizamientos 2.4.2. Sequías 2.4.2.1 Riesgos por sequía 2.4.3. Inundaciones 2.4.3.1. Riesgos por inundaciones 2.4.4. Sismicidad y Geología 2.4.4.1 Sismicidad 2 ANÁLISIS DE RIESGO NATURALES DE LA SUBREGION LA UNION --------------------------------------------------------------------------------------------------------------------------------------------------------- 2.4.4.1.1 Riesgos por sismos 2.4.4.2 Geológica 2.4.4.2.1 Vulcanismo 2.4.4.2.2. Movimientos de Ladera. 2.4.4.2.3.Tsunami 3. PROPUESTA DE ACCIONES DE PLANIFICACIÓN Y DESARROLLO 3.1. Desarrollo Urbano 3.2. Infraestructuras 3.3 Recursos Naturales y Culturales 3.4 Recursos Hidrobiológicos 3.5 Biodiversidad 3.5. Gestión de Riesgos 3 ANÁLISIS DE RIESGO NATURALES DE LA SUBREGION LA UNION --------------------------------------------------------------------------------------------------------------------------------------------------------- INDICE DE CUADROS Cuadro 1. -
Māui 4D Seismic Survey
Māui 4D Seismic Survey Marine Mammal Impact Assessment Report Number 740.10033-R01 11 January 2018 Shell Taranaki Limited 167 Devon Street West New Plymouth Version: v1.0 Shell Taranaki Limited Report Number 740.10033-R01 Māui 4D Seismic Survey 11 January 2018 Marine Mammal Impact Assessment Version v1.0 Page 2 Māui 4D Seismic Survey Marine Mammal Impact Assessment PREPARED BY: SLR Consulting NZ Limited Company Number 2443058 5 Duncan Street Port Nelson 7010, Nelson New Zealand (PO Box 5061, Port Nelson 7043 Nelson New Zealand) +64 274 898 628 [email protected] www.slrconsulting.com This report has been prepared by SLR Consulting NZ Limited with all reasonable skill, care and diligence, and taking account of the timescale and resources allocated to it by agreement with the Client. Information reported herein is based on the interpretation of data collected, which has been accepted in good faith as being accurate and valid. This report is for the exclusive use of Shell Taranaki Limited. No warranties or guarantees are expressed or should be inferred by any third parties. This report may not be relied upon by other parties without written consent from SLR. SLR disclaims any responsibility to the Client and others in respect of any matters outside the agreed scope of the work. DOCUMENT CONTROL Reference Date Prepared Checked Authorised 740.10033-R01-v1.0 11 January 2018 Helen McConnell and Dan Govier Dan Govier Nicole Pannell 740.10033-R01-v0.2 31 December 2017 Helen McConnell and Dan Govier Dan Govier Nicole Pannell 740.10033-R01-v0.1 8 December 2017 Helen McConnell and Dan Govier Dan Govier Nicole Pannell SLR Consulting NZ Limited Shell Taranaki Limited Report Number 740.10033-R01 Māui 4D Seismic Survey 11 January 2018 Marine Mammal Impact Assessment Version v1.0 Page 3 Executive Summary Shell Taranaki Limited proposes to undertake a marine seismic survey, the ‘Māui 4D Seismic Survey’, in the Taranaki Basin. -
Radiocarbon and Geologic Evidence Reveal Ilopango Volcano As Source of the Colossal ‘Mystery’ Eruption of 539/40 CE
Quaternary Science Reviews xxx (xxxx) xxx Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Radiocarbon and geologic evidence reveal Ilopango volcano as source of the colossal ‘mystery’ eruption of 539/40 CE * Robert A. Dull a, b, , John R. Southon c, Steffen Kutterolf d, Kevin J. Anchukaitis e, Armin Freundt d, David B. Wahl f, g, Payson Sheets h, Paul Amaroli i, Walter Hernandez j, Michael C. Wiemann k, Clive Oppenheimer l a Department of Earth and Environmental Sciences, California Lutheran University, Thousand Oaks, CA, 91360, USA b Environmental Science Institute, University of Texas, Austin, TX, 78712, USA c Department of Earth System Science, University of California at Irvine, Irvine, CA, 92697, USA d GEOMAR, Helmholtz Center for Ocean Research, Wischhofstr. 1-3, D-24148, Kiel, Germany e School of Geography and Development and Laboratory of Tree-Ring Research, University of Arizona, Tucson, AZ, 85721, USA f United States Geological Survey, Menlo Park, CA, 94025, USA g Department of Geography, University of California at Berkeley, CA, 94720, USA h Department of Anthropology, University of Colorado, Boulder, CO, 80309, USA i Fundacion Nacional de Arqueología de El Salvador, FUNDAR, San Salvador, El Salvador j Retired from Ministerio de Medio Ambiente y Recursos Naturales, San Salvador, El Salvador k United States Department of Agriculture Forest Products Laboratory, Madison, WI, 53726, USA l Department of Geography, University of Cambridge, Downing Place, Cambridge, CB2 3EN, UK article info abstract Article history: Ilopango volcano (El Salvador) erupted violently during the Maya Classic Period (250e900 CE) in a Received 24 February 2019 densely-populated and intensively-cultivated region of the southern Maya realm, causing regional Received in revised form abandonment of an area covering more than 20,000 km2.