Introduction: an Overview of Ridge-Trench Interactions in Modern and Ancient Settings Virginia B
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Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information
Cambridge University Press 978-1-108-44568-9 — Active Faults of the World Robert Yeats Index More Information Index Abancay Deflection, 201, 204–206, 223 Allmendinger, R. W., 206 Abant, Turkey, earthquake of 1957 Ms 7.0, 286 allochthonous terranes, 26 Abdrakhmatov, K. Y., 381, 383 Alpine fault, New Zealand, 482, 486, 489–490, 493 Abercrombie, R. E., 461, 464 Alps, 245, 249 Abers, G. A., 475–477 Alquist-Priolo Act, California, 75 Abidin, H. Z., 464 Altay Range, 384–387 Abiz, Iran, fault, 318 Alteriis, G., 251 Acambay graben, Mexico, 182 Altiplano Plateau, 190, 191, 200, 204, 205, 222 Acambay, Mexico, earthquake of 1912 Ms 6.7, 181 Altunel, E., 305, 322 Accra, Ghana, earthquake of 1939 M 6.4, 235 Altyn Tagh fault, 336, 355, 358, 360, 362, 364–366, accreted terrane, 3 378 Acocella, V., 234 Alvarado, P., 210, 214 active fault front, 408 Álvarez-Marrón, J. M., 219 Adamek, S., 170 Amaziahu, Dead Sea, fault, 297 Adams, J., 52, 66, 71–73, 87, 494 Ambraseys, N. N., 226, 229–231, 234, 259, 264, 275, Adria, 249, 250 277, 286, 288–290, 292, 296, 300, 301, 311, 321, Afar Triangle and triple junction, 226, 227, 231–233, 328, 334, 339, 341, 352, 353 237 Ammon, C. J., 464 Afghan (Helmand) block, 318 Amuri, New Zealand, earthquake of 1888 Mw 7–7.3, 486 Agadir, Morocco, earthquake of 1960 Ms 5.9, 243 Amurian Plate, 389, 399 Age of Enlightenment, 239 Anatolia Plate, 263, 268, 292, 293 Agua Blanca fault, Baja California, 107 Ancash, Peru, earthquake of 1946 M 6.3 to 6.9, 201 Aguilera, J., vii, 79, 138, 189 Ancón fault, Venezuela, 166 Airy, G. -
Tectonic Influences on the Spatial and Temporal Evolution of the Walker Lane: an Incipient Transform Fault Along the Evolving Pacific – North American Plate Boundary
Arizona Geological Society Digest 22 2008 Tectonic influences on the spatial and temporal evolution of the Walker Lane: An incipient transform fault along the evolving Pacific – North American plate boundary James E. Faulds and Christopher D. Henry Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada, 89557, USA ABSTRACT Since ~30 Ma, western North America has been evolving from an Andean type mar- gin to a dextral transform boundary. Transform growth has been marked by retreat of magmatic arcs, gravitational collapse of orogenic highlands, and periodic inland steps of the San Andreas fault system. In the western Great Basin, a system of dextral faults, known as the Walker Lane (WL) in the north and eastern California shear zone (ECSZ) in the south, currently accommodates ~20% of the Pacific – North America dextral motion. In contrast to the continuous 1100-km-long San Andreas system, discontinuous dextral faults with relatively short lengths (<10-250 km) characterize the WL-ECSZ. Cumulative dextral displacement across the WL-ECSZ generally decreases northward from ≥60 km in southern and east-central California, to ~25 km in northwest Nevada, to negligible in northeast California. GPS geodetic strain rates average ~10 mm/yr across the WL-ECSZ in the western Great Basin but are much less in the eastern WL near Las Vegas (<2 mm/ yr) and along the northwest terminus in northeast California (~2.5 mm/yr). The spatial and temporal evolution of the WL-ECSZ is closely linked to major plate boundary events along the San Andreas fault system. For example, the early Miocene elimination of microplates along the southern California coast, southward steps in the Rivera triple junction at 19-16 Ma and 13 Ma, and an increase in relative plate motions ~12 Ma collectively induced the first major episode of deformation in the WL-ECSZ, which began ~13 Ma along the N60°W-trending Las Vegas Valley shear zone. -
Borehole-Explosion and Air-Gun Data Acquired in the 2011 Salton Seismic Imaging Project (SSIP), Southern California: Description of the Survey
Borehole-Explosion and Air-Gun Data Acquired in the 2011 Salton Seismic Imaging Project (SSIP), Southern California: Description of the Survey Open-File Report 2013–1172 U.S. Department of the Interior U.S. Geological Survey COVER: High-explosives magazine, used for the Salton Seismic Imaging Program, parked in secured, unused private rodeo ground in Imperial Valley, California. Photo by Gary Fuis. Borehole-Explosion and Air-Gun Data Acquired in the 2011 Salton Seismic Imaging Project (SSIP), Southern California: Description of the Survey By Elizabeth J. Rose, Gary S. Fuis, Joann M. Stock, John A. Hole, Annie M. Kell, Graham Kent, Neal W. Driscoll, Sam Crum, Mark Goldman, Angela M. Reusch, Liang Han, Robert R. Sickler, Rufus D. Catchings, Michael J. Rymer, Coyn J. Criley, Daniel S. Scheirer, Steven M. Skinner, Coye J. Slayday-Criley, Janice M. Murphy, Edward G. Jensen, Robert McClearn, Alex J. Ferguson, Lesley A. Butcher, Max A. Gardner, Iain Emmons, Caleb L. Loughran, Joseph R. Svitek, Patrick C. Bastien, Joseph A. Cotton, David S. Croker, Alistair J. Harding, Jeffrey M. Babcock, Steven H. Harder, and Carla M. Rosa Open-File Report 2013–1172 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2013 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call -
Neotectonics Along the Eastern Flank of the North Patagonian Icefield, Southern Chile: Cachet and Exploradores Fault Zones
XII Congreso Geológico Chileno Santiago, 22-26 Noviembre, 2009 S9_053 Neotectonics along the eastern flank of the North Patagonian Icefield, southern Chile: Cachet and Exploradores fault zones Melnick, D.1, Georgieva, V.1, Lagabrielle, Y.2, Jara, J.3, Scalabrino, B.2, Leidich, J.4 (1) Institute of Geosciences, University of Potsdam, 14476 Potsdam, Germany. (2) UMR 5243 Géosciences Montpellier, Université de Montpellier 2, France. (3) Departamento de Ciencias de la Tierra, Universidad de Concepción, Chile. (4) Patagonia Adventure Expeditions, Casilla 8, Cochrane, Chile. [email protected] Introduction In the southern Andes, the North Patagonian Icefield (NPI) is a poorly-known region in terms of geology and neotectonics that marks a major topographic anomaly at the transition between the Austral and Patagonian Andes. The NPI is located immediately east of the Nazca-Antarctic-South America Triple Plate Junction, where the Chile Rise collides against the margin (Fig. 1A). Since 14 Ma, this Triple Junction has migrated northward as a result of oblique plate convergence, resulting in collision and subduction of two relatively short ridge segments in the Golfo de Penas region at 6 and 3 Ma, and at present of one segment immediately north of the Taitao Peninsula [1]. Oblique plate convergence in addition to collision of these ridge segments resulted in the formation of a forearc sliver, the Chiloe block, which is decoupled from the South American foreland by the Liquiñe-Ofqui fault zone. Here we present geomorphic and structural field evidence that indicates neotectonic activity in the internal part of the orogen, along the flanks of the NPI (Fig. -
Geochemistry and Origin of Middle Miocene Volcanic Rocks from Santa Cruz and Anacapa Islands, Southern California Borderland Peter W
Geochemistry and Origin of Middle Miocene Volcanic Rocks from Santa Cruz and Anacapa Islands, Southern California Borderland Peter W. Weigand Department of Geological Sciences California State University Northridge, CA 91330 Cenozoic volcanism that began in the eastern Abstract - Major-oxide and trace-element Mojave Desert about 30 m.y. ago and swept compositions of middle Miocene volcanic rocks irregularly west and north. This extensive from north Santa Cruz and Anacapa Islands are extrusive activity was related closely to complex very similar. In contrast, they are geochemically tectonic activity that included subduction of the distinct from the volcanic clasts from the Blanca Farallon plate whose subduction angle was Formation, of similar age but located south of steepening, and interaction of the Pacific and the Santa Cruz Island fault, which implies North American plates along a lengthening significant strike-slip movement on this fault. transform boundary; this activity additionally The island lavas are also compositionally involved rotation and possible northward distinct from the Conejo Volcanics located translation of crustal blocks. onshore in the Santa Monica Mountains. The The origin of the volcanic rocks in this area island lavas are part of a larger group of about has been variously ascribed to subduction of the 12 similar-aged volcanic suites from the Farallon plate (Weigand 1982; Crowe et al. California Borderland and onshore southern 1976; Higgins 1976), subduction of the Pacific- California that all belong to the calc-alkaline -
The Stability and Evolution of Triple Junctions
THE STABILITY AND EVOLUTION OF TRIPLE JUNCTIONS Theodore G. Apotria B.S., The University of Connecticut, 1982 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science at The University of Connecticut 1985 APPROVAL PAGE Master of Science Thesis THE STABILITY AND EVOLUTION OP TRIPLE JUNCTIONS Presented by- Theodore G. Apotria, B.S. Major Adviser Associate Adviser | Peter Dehlrnger Associate Adviser 7 Peter Geiser Associate Adviser Thomas Moran The University of Connecticut 1985 ii DEDICATION This thesis is dedicated to my parents, George and Cleo Apotria, and to my "brother and best friend, John. Their support was essential in completing this work. iii ACKNOWLEDGEMENTS There are several individuals whose assistance and support contributed to this thesis, and to whom I am indebted: I am especially thankful to Dr. Norman Gray, who, as my major adviser, contributed many hours of stimulating discussion and attention. As the thesis topic evolved, his assistance in the theoretical development, computer programming, and critical commentary on the manuscript, all proved invaluable. Dr. Peter Dehlinger, Dr. Peter Geiser, and Dr. Thomas Moran, contributed their time reviewing the text and provided useful perspectives. Dr. Randolph Steinen contributed useful comments on the preliminary research proposal. I am also grateful to the Dept, of Geology and Geophysics for providing financial support in the form of a Teaching Assistantship, and an Amoco sponsored Master's Fellowship in Geophysics. I also thank Dr. Anthony Philpotts for providing a Research Assistantship from K.S.F. grant if EAR8017059* - iv ABSTRACT Triple junction stability, as introduced by McKenzie and Morgan (1969)> assumes constant relative velocities and can only be defined instantaneously. -
4 Three-Dimensional Density Model of the Nazca Plate and the Andean Continental Margin
76 4 Three-dimensional density model of the Nazca plate and the Andean continental margin Authors: Andrés Tassara, Hans-Jürgen Götze, Sabine Schmidt and Ron Hackney Paper under review (September 27th, 2005) by the Journal of Geophysical Research Abstract We forward modelled the Bouguer anomaly in a region encompassing the Pacific ocean (east of 85°W) and the Andean margin (west of 60°W) between northern Peru (5°S) and Patagonia (45°S). The three-dimensional density structure used to accurately reproduce the gravity field is simple. The oceanic Nazca plate is formed by one crustal body and one mantle lithosphere body overlying a sub-lithospheric mantle, but fracture zones divide the plate into seven along-strike segments. The subducted slab was modelled to a depth of 410 km, has the same structure as the oceanic plate, but it is subdivided into four segments with depth. The continental margin consists of one upper-crustal and one lower-crustal body without lateral subdivision, whereas the mantle has two bodies for the lithosphere and two bodies for the asthenosphere that are separated across-strike by the downward prolongation of the eastern limit of active volcanism. We predefined the density for each body after studying its dependency on composition of crustal and mantle materials and pressure-temperature conditions appropriate for the Andean setting. A database containing independent geophysical information constrains the geometry of the subducted slab, locally the Moho of the oceanic and continental crusts, and indirectly the lithosphere-asthenosphere boundary (LAB) underneath the continental plate. Other geometries, especially that of the intracrustal density discontinuity (ICD) in the continental margin, were not constrained and are the result of fitting the observed and calculated Bouguer anomaly during the forward modelling. -
Uplift of Quaternary Shorelines in Eastern Patagonia: Darwin Revisited
Uplift of Quaternary shorelines in Eastern Patagonia: Darwin revisited Kevin Pedoja, Vincent Regard, Laurent Husson, Joseph Martinod, Benjamin Guillaume, Enrique Fucks, Maximiliano Iglesias, Pierre Weill To cite this version: Kevin Pedoja, Vincent Regard, Laurent Husson, Joseph Martinod, Benjamin Guillaume, et al.. Uplift of Quaternary shorelines in Eastern Patagonia: Darwin revisited. Geomorphology, Elsevier, 2011, 127 (3-4), pp.121-142. 10.1016/j.geomorph.2010.08.003. insu-00610899 HAL Id: insu-00610899 https://hal-insu.archives-ouvertes.fr/insu-00610899 Submitted on 6 Mar 2019 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 Uplift of quaternary shorelines in eastern Patagonia: Darwin revisited Kevin Pedoja a,⁎, Vincent Regard b,c,d, Laurent Husson e,f, Joseph Martinod b,c,d, Benjamin Guillaume g, Enrique Fucks h, Maximiliano Iglesias i, Pierre Weill a a Laboratoire de Morphodynamique Continentale et Côtière, CNRS, Université de Caen, 14000 Caen, France b Université de Toulouse ; UPS (OMP) ; LMTG ; 14 Av Edouard Belin, F-31400 Toulouse, France c IRD ; LMTG ; F-31400 Toulouse, France d CNRS ; LMTG ; F-31400 Toulouse, France e CNRS UMR 6118, Géosciences Rennes, 35042 Rennes, France f CNRS UMR 6112, Laboratoire de Planétologie et Géodynamique de Nantes, France g Dip. -
Crustal Faults in the Chilean Andes: Geological Constraints and Seismic Potential
Andean Geology 46 (1): 32-65. January, 2019 Andean Geology doi: 10.5027/andgeoV46n1-3067 www.andeangeology.cl Crustal faults in the Chilean Andes: geological constraints and seismic potential *Isabel Santibáñez1, José Cembrano2, Tiaren García-Pérez1, Carlos Costa3, Gonzalo Yáñez2, Carlos Marquardt4, Gloria Arancibia2, Gabriel González5 1 Programa de Doctorado en Ciencias de la Ingeniería, Pontificia Universidad Católica de Chile, Avda. Vicuña Mackenna 4860, Macul, Santiago, Chile. [email protected]; [email protected] 2 Departamento de Ingeniería Estructural y Geotécnica, Pontificia Universidad Católica de Chile, Avda. Vicuña Mackenna 4860, Macul, Santiago, Chile. [email protected]; [email protected]; [email protected] 3 Departamento de Geología, Universidad de San Luis, Ejercito de Los Andes 950, D5700HHW San Luis, Argentina. [email protected] 4 Departamento de Ingeniería Estructural y Geotécnica y Departamento de Ingeniería de Minería, Pontificia Universidad Católica de Chile. Avda. Vicuña Mackenna 4860, Macul, Santiago, Chile. [email protected] 5 Departamento de Ciencias Geológicas, Universidad Católica del Norte, Angamos 0610, Antofagasta, Chile. [email protected] * Corresponding author: [email protected] ABSTRACT. The Chilean Andes, as a characteristic tectonic and geomorphological region, is a perfect location to unravel the geologic nature of seismic hazards. The Chilean segment of the Nazca-South American subduction zone has experienced mega-earthquakes with Moment Magnitudes (Mw) >8.5 (e.g., Mw 9.5 Valdivia, 1960; Mw 8.8 Maule, 2010) and many large earthquakes with Mw >7.5, both with recurrence times of tens to hundreds of years. By contrast, crustal faults within the overriding South American plate commonly have longer recurrence times (thousands of years) and are known to produce earthquakes with maximum Mw of 7.0 to 7.5. -
19. Analysis and Correlation of Volcanic
Jørgensen, B.B., D’Hondt, S.L., and Miller, D.J. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 201 19. ANALYSIS AND CORRELATION OF VOLCANIC ASH IN MARINE SEDIMENTS FROM THE PERU MARGIN, OCEAN DRILLING PROGRAM LEG 201: EXPLOSIVE VOLCANIC 1 CYCLES OF THE NORTH-CENTRAL ANDES D. Hart2 and D.J. Miller3 ABSTRACT Although land studies have identified major volcanic centers of his- 1Hart, D., and Miller, D.J., 2006. toric eruptions within the Central Andes, the tephrachronologic record Analysis and correlation of volcanic is disturbed by the high erosion rates in this arid region. Owing to ero- ash in marine sediments from the Peru sion, studies of volcanic cyclicity based on subaerial deposits offer an margin, Ocean Drilling Program Leg incomplete record of the frequency and episodicity of eruptions since 201: explosive volcanic cycles of the north-central Andes. In Jørgensen, the Miocene. However, volcanic material commonly occurs in marine B.B., D’Hondt, S.L., and Miller, D.J. sediment as discrete ash fall layers and/or disseminated ash accumula- (Eds.), Proc. ODP, Sci. Results, 201, 1–43 tions. A detailed investigation of cores from three sites offshore Peru [Online]. Available from World Wide drilled during Ocean Drilling Program (ODP) Leg 201 has been con- Web: <http://www-odp.tamu.edu/ ducted to determine the occurrence of volcanic ash layers and ash accu- publications/201_SR/VOLUME/ CHAPTERS/122.PDF>. [Cited YYYY- mulations within marine sediments along the Peru shelf. These sites MM-DD] were previously occupied during ODP Leg 112, which suffered from 2Department of Geology and poor and/or disturbed core recovery. -
1028-2 Holocene Sediments from the Southern Chile Trench a Record Of
Journal of the Geological Society Holocene sediments from the Southern Chile Trench: a record of active margin magmatism, tectonics and palaeoseismicity Bianca Heberer, Georg Röser, Jan H. Behrmann, Meinert Rahn and Achim Kopf Journal of the Geological Society 2010; v. 167; p. 539-553 doi:10.1144/0016-76492009-015 Email alerting click here to receive free email alerts when new articles cite this article service Permission click here to seek permission to re-use all or part of this article request Subscribe click here to subscribe to Journal of the Geological Society or the Lyell Collection Notes Downloaded by National Centre University on 10 May 2010 © 2010 Geological Society of London Journal of the Geological Society, London, Vol. 167, 2010, pp. 539–553. doi: 10.1144/0016-76492009-015. Holocene sediments from the Southern Chile Trench: a record of active margin magmatism, tectonics and palaeoseismicity BIANCA HEBERER1*, GEORG RO¨ SER2, JAN H. BEHRMANN3, MEINERT RAHN4 &ACHIMKOPF5 1Department of Geography and Geology, University of Salzburg, Hellbrunner Strasse 34, 5020 Salzburg, Austria 2Anders Estenstads Veg 22, 7046 Trondheim, Norway 3IFM-GEOMAR, Wischofstrasse 1–3, 24148 Kiel, Germany 4ENSI, 5232 Villigen-ENSI, Switzerland 5RCOM, Universita¨t Bremen, Leobener Strasse, 28539 Bremen, Germany *Corresponding author (e-mail: [email protected]) Abstract: Sedimentology, petrography and the provenance of Holocene sediments from the Southern Chile Trench (36–478S) were investigated in an integrated approach combining description of a collection of gravity cores, measurements of physical properties, quantitative X-ray petrography and modal analysis. The sediments studied were trench hemipelagic sediments, fan deposits, and more distal hemipelagic sediments from the Nazca Plate. -
Miocene to Late Quaternary Patagonian Basalts (46–478S): Geochronometric and Geochemical Evidence for Slab Tearing Due to Active Spreading Ridge Subduction
Journal of Volcanology and Geothermal Research 149 (2006) 346–370 www.elsevier.com/locate/jvolgeores Miocene to Late Quaternary Patagonian basalts (46–478S): Geochronometric and geochemical evidence for slab tearing due to active spreading ridge subduction Christe`le Guivel a,*, Diego Morata b, Ewan Pelleter c,d, Felipe Espinoza b, Rene´ C. Maury c, Yves Lagabrielle e, Mireille Polve´ f,g, Herve´ Bellon c, Joseph Cotten c, Mathieu Benoit c, Manuel Sua´rez h, Rita de la Cruz h a UMR 6112 bPlane´tologie et Ge´odynamiqueQ, Universite´ de Nantes, 2 rue de la Houssinie`re, 44322 Nantes, France b Departamento de Geologı´a. Fac. Cs. Fı´sicas y Matema´ticas, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile c UMR 6538 bDomaines oce´aniquesQ, UBO-IUEM, place Nicolas-Copernic, 29280 Plouzane´, France d CRPG-CNRS UPR A2300, BP 20, 54501 Vandoeuvre-les-Nancy, France e UMR 5573, Dynamique de la Lithosphe`re, Place E. Bataillon, case 60, 34095, Montpellier Cedex 5, France f LMTG-OMP, 14 Avenue E. Belin, 31400 Toulouse, France g IRD-Departamento de Geologia de la Universidad de Chile, Chile h Servicio Nacional de Geologı´a y Minerı´a, Avda. Santa Marı´a 0104, Santiago, Chile Received 18 May 2005; received in revised form 29 August 2005; accepted 14 September 2005 Abstract Miocene to Quaternary large basaltic plateaus occur in the back-arc domain of the Andean chain in Patagonia. They are thought to result from the ascent of subslab asthenospheric magmas through slab windows generated from subducted segments of the South Chile Ridge (SCR). We have investigated three volcanic centres from the Lago General Carrera–Buenos Aires area (46–478S) located above the inferred position of the slab window corresponding to a segment subducted 6 Ma ago.