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  • 1
    Monograph available for loan
    Monograph available for loan
    Washington, DC : US Gov.Print.Off.
    Associated volumes
    Call number: MOP 18250
    In: Monthly weather review
    Type of Medium: Monograph available for loan
    Pages: II, 34 S.
    Series Statement: Monthly weather review : Supplement 47
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Industrial and engineering chemistry 6 (1934), S. 136-138 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2011-02-05
    Description: The Mejillones Peninsula in northern Chile has been recognized as the surface expression of a segment boundary for large subduction zone earthquakes. The sharp contact between the rupture planes of two instrumentally recorded earthquakes, the Mw = 8.0 Antofagasta (1995) and the Mw = 7.7 Tocopilla (2007) events, is located beneath the central part of Mejillones Peninsula. We present new chronostratigraphic and structural data that allow reconstructing the evolution of the Peninsula at the surface and correlation of the latter with seismic cycle deformation on the plate interface. Uplift commenced after 3.4 Myr, as recorded in the western highland. The central graben area on the Peninsula started uplifting above sea level as an anticlinal hinge zone prior to 400 kyr ago, most probably 790 kyr ago. The resulting E-W trending hinge exactly overlies the limit between the rupture planes of the Antofagasta and Tocopilla earthquakes. By correlating the uplift data with the slip distribution of the above earthquakes, we demonstrate that deformation and uplift is focused during the postseismic and interseismic periods of the megathrust seismic cycle with coseismic deformation opposed to the long-term motion. Additionally, the slip deficit beneath the Peninsula accumulating between events is probably largely recovered by creep. Hence we suggest that Mejillones Peninsula owes its existence to the lateral variation of the propensity for unstable slip at the interface. Since the latter is a material property, the long-term spatial stability of the Peninsula as a barrier to rupture propagation since at least the middle Pleistocene is a necessary consequence.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 4
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    Nature Publishing Group (NPG)
    Publication Date: 2010-11-19
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Victor, Peter -- England -- Nature. 2010 Nov 18;468(7322):370-1. doi: 10.1038/468370a.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉York University in Toronto, Ontario. pvictor@yorku.ca〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21085153" target="_blank"〉PubMed〈/a〉
    Keywords: Biodiversity ; Carbon Footprint/economics/statistics & numerical data ; Climate Change/economics/statistics & numerical data ; Conservation of Natural Resources/economics/*methods/*trends ; Cost-Benefit Analysis ; Developing Countries/economics ; Ecology/methods/trends ; Gross Domestic Product/statistics & numerical data/*trends ; Happiness ; Internationality ; *Models, Economic ; Population Growth ; Public Policy/*trends ; Recycling/methods/trends ; Technology/economics/trends
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
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    Nature Publishing Group (NPG)
    Publication Date: 2011-04-23
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Victor, Peter -- Jackson, Tim -- England -- Nature. 2011 Apr 21;472(7343):295. doi: 10.1038/472295a.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/21512560" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2014-08-15
    Description: On 1 April 2014, Northern Chile was struck by a magnitude 8.1 earthquake following a protracted series of foreshocks. The Integrated Plate Boundary Observatory Chile monitored the entire sequence of events, providing unprecedented resolution of the build-up to the main event and its rupture evolution. Here we show that the Iquique earthquake broke a central fraction of the so-called northern Chile seismic gap, the last major segment of the South American plate boundary that had not ruptured in the past century. Since July 2013 three seismic clusters, each lasting a few weeks, hit this part of the plate boundary with earthquakes of increasing peak magnitudes. Starting with the second cluster, geodetic observations show surface displacements that can be associated with slip on the plate interface. These seismic clusters and their slip transients occupied a part of the plate interface that was transitional between a fully locked and a creeping portion. Leading up to this earthquake, the b value of the foreshocks gradually decreased during the years before the earthquake, reversing its trend a few days before the Iquique earthquake. The mainshock finally nucleated at the northern end of the foreshock area, which skirted a locked patch, and ruptured mainly downdip towards higher locking. Peak slip was attained immediately downdip of the foreshock region and at the margin of the locked patch. We conclude that gradual weakening of the central part of the seismic gap accentuated by the foreshock activity in a zone of intermediate seismic coupling was instrumental in causing final failure, distinguishing the Iquique earthquake from most great earthquakes. Finally, only one-third of the gap was broken and the remaining locked segments now pose a significant, increased seismic hazard with the potential to host an earthquake with a magnitude of 〉8.5.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Schurr, Bernd -- Asch, Gunter -- Hainzl, Sebastian -- Bedford, Jonathan -- Hoechner, Andreas -- Palo, Mauro -- Wang, Rongjiang -- Moreno, Marcos -- Bartsch, Mitja -- Zhang, Yong -- Oncken, Onno -- Tilmann, Frederik -- Dahm, Torsten -- Victor, Pia -- Barrientos, Sergio -- Vilotte, Jean-Pierre -- England -- Nature. 2014 Aug 21;512(7514):299-302. doi: 10.1038/nature13681. Epub 2014 Aug 13.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉GFZ Helmholtz Centre Potsdam, German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany. ; School of Earth and Space Sciences, Peking University, Beijing 100871, China. ; Centro Sismologico National, Universidad de Chile, Facultad de Ciencias Fisicas y Matematicas, Blanco Encalada 2002, Santiago, Chile. ; Institut de Physique du Globe de Paris, 1, rue Jussieu, 75238 Paris cedex 05, France.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/25119049" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 2019-10-24
    Print ISSN: 0167-6369
    Electronic ISSN: 1573-2959
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 8
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    PANGAEA
    In:  Supplement to: Filippov, A N; Nechaev, Victor P; Ekimova, N I (2006): Clastic heavy mineral assemblages in Permian-Mesozoic accretionary cherty and siliceous-clayey complexes of Sikhote Alin. Translated from Litologiya i Poleznye Iskopaemye, 2006, 3, 258-278, Lithology and Mineral Resources, 41(3), 230-249, https://doi.org/10.1134/S0024490206030047
    Publication Date: 2023-05-12
    Description: The paper reports results of a study of clastic heavy mineral assemblages and geochemical features of some assemblages in several Permian-Mesozoic cherty and siliceous-clayey sequences of the Sikhote Alin Region. They are composed of pelagic and hemipelagic sediments of the Panthalassa (Paleopacific) Ocean. Four typical mineral assemblages and their environments are established. In one of the ocean segments, where the sedimentary cover formed during Late Paleozoic - Early Cretaceous, the Permian pelagic domain was characterized by the amphibole-pyroxene assemblage with heavy minerals derived from ophiolites. The Triassic-Jurassic stage was marked by development of the clinopyroxene assemblage with heavy minerals derived from intraplate alkaline volcanic complexes. Middle-Late Jurassic hemipelagic sediments host the zircon-clinopyroxene assemblage with greater role of continental environments and presence of volcanic products of the convergence zone. Another segment of the ocean accumulated red cherts and siliceous-clayey sediments during Jurassic - Early Cretaceous under influence of island-arc volcanism.
    Keywords: Archive of Ocean Data; ARCOD
    Type: Dataset
    Format: application/zip, 9 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Markov, Yu D; Mozherovsky, A V; Pushkar', V S; Vashchenkova, N G; Nechaev, Victor P (2005): Sedimentation features and stratigraphic correlation of unconsolidated deposits from the Clarion Transform Fault Zone (Northeast Pacific). Pacific Geology, 24(4), 24-43
    Publication Date: 2023-05-12
    Description: New data on lithology and stratigraphy of Cenozoic sediments from the Clarion Transform Fault Zone (Pacific Ocean) have been obtained on the base of polygon studies. It has been established that on different blocks (uplifted and subsided) of the Clarion tectonic structure deposits of different age (Eocene to Quaternary) occur. Unconsolidated sediments have been deposited under pelagic conditions since Eocene (probably, since Early Cretaceous) until now. Their mineral composition and content of different ore components are given.
    Keywords: Akademik A. Vinogradov; Archive of Ocean Data; ARCOD; AVI13; AVI13-100; AVI13-101; AVI13-102; AVI13-103; AVI13-104; AVI13-107; AVI13-108; AVI13-17; AVI13-73; AVI13-74; AVI13-80; AVI13-81; AVI13-82; AVI13-83; AVI13-88; AVI13-89; AVI13-97; AVI13-99; GC; Gravity corer; Northeast Pacific
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 10
    Publication Date: 2023-05-12
    Keywords: Akademik A. Vinogradov; Archive of Ocean Data; ARCOD; AVI13; AVI13-100; AVI13-101; AVI13-102; AVI13-103; AVI13-104; AVI13-107; AVI13-108; AVI13-73; AVI13-74; AVI13-80; AVI13-82; AVI13-83; AVI13-88; AVI13-89; AVI13-97; AVI13-99; Barite; Biogenic; Counting, Stereo Microscope; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; GC; Gravity corer; Latitude of event; Longitude of event; Micronodules; Northeast Pacific; Quartz and Feldspar; Rock fragments; Sediment type; Smectite; Volcanic glass; Zeolite
    Type: Dataset
    Format: text/tab-separated-values, 516 data points
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