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  • 2005-2009  (25)
  • 1995-1999  (1)
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  • 1
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 2
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    In:  Geología y recursos naturales de la provincia de Jujuy, Relatorio del XVII Congreso Geológico Argentino, Jujuy
    Publication Date: 2020-02-12
    Description: En este capítulo presentamos un sumario de las anomalias sísmicas de gran escala determinadas a partir de datos sismológicos por proyectos llevados a cabo en las inmediaciones de la Puna de Jujuy y regiones adyacentes. Estos datos han sido utilizados para definir la geometría de la zona de subducción, determinar el espesor de la corteza y la litósfera, enmarcar zonas de baja velocidad sísmica de ondas P y S (vp y vs) y de alta atenuación sísmica (Q) asociada con la presencia de fluidos y/o material fundido en la corteza y el manto. Han servido tambien para enmarcar zona de alta velocidad de ondas vp y vs con baja atenuación sísmica que indican la presencia de material denso y sin fluidos en la corteza y el manto. La combinación de estos resultados ha proporcionado evidencia acerca de la presencia de cuerpos magmáticos intra-crustales, zonas de fusión en el manto y finalmente de remoción o delaminación cortical y litosférica.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/bookPart
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  • 3
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 4
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    In:  GSA Backbone of the Americas-Patagonia to Alaska (Mendoza, Argentina 2006)
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 5
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    In:  EOS, Transactions, American Geophysical Union, Fall Meeting Suppl. 90, 52
    Publication Date: 2020-02-12
    Description: We study the underside reflections of precursors to SS waves at the lithosphere and the upper mantle beneath eastern Asia. By analyzing the SS bounce points we have been able to investigate the upper mantle discontinuities along a corridor that extends from the Aleutians to the Tibetan plateau passing through Kamchatka, the Japanese subduction zone and the North China craton. One of our aims was to investigate the interaction between the lithosphere and the mantle transition zone beneath different geotectonic units along this corridor and the interaction of geodynamic processes at different depths. In the analysis, we have used the short period content of SS waveform data and methods like CMP stack and migration techniques to acquire high resolution lithosphere and upper mantle images and to improve the lateral and depth resolution for the upper mantle discontinuities. By using a newly developed method we have been able to detect the presence of the continental Moho at different depths along this corridor. We show that the SS precursors provide high resolution images of upper mantle discontinuities such as the 410 and 660 km and the effects of the interaction between the subducted oceanic lithosphere and the mantle transition zone beneath the NW Pacific subduction zone. Furthermore, we show for the first time, that it is possible to create new possibilities to study shallower structures such as the Moho by using the SS precursors.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 6
    Publication Date: 2020-02-12
    Description: The Alborz Mountains build the northern part of the Alpine–Himalayan orogen in western Asia. They are located south of the Caspian Sea and form an east–west range across the north of Iran. This region is one of the most active tectonic areas, as it undergoes extensive crustal deformation and shortening. In the present work, we used data from 11 permanent stations of the Tehran Telemetry Seismic Network to estimate the thickness of the crust and mantle lithosphere beneath the Central Alborz region by P- and S-receiver function methods. Results of both P and S receiver functions revealed a relatively large crustal thickness beneath this region (∼51–54 km), which can be associated with the shortening process related to the orogenic belt. No remarkable crustal thickening has been detected below the high topography of Central Alborz. A thick crust (∼67.5 km) is observed locally in the region beneath the Damavand volcano, which is possibly related to the magmatic addition at the base of the crust beneath the volcanic region. The S receiver functions exhibit the existence of a seismic discontinuity in the upper mantle at a depth of ∼90 km, which we interpreted as the base of the lithosphere. The missing crustal root and the relatively thin lithosphere beneath the Alborz may imply that sublithospheric mantle could be responsible for and support the elevation of the Alborz.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
    Format: application/pdf
    Format: application/pdf
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  • 7
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    In:  69. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (Kiel 2009)
    Publication Date: 2020-02-12
    Description: We attempt to use the large amount of seismic data recorded by the GRSN, GRF and GEOFON stations to study the topography of the mantle transition zone in the continent-ocean transition of eastern Asia and NW Pacific by SS precursors. SS bounce points sample a corridor from the Aleutians, Kamchatka and the Japan subduction zones through the North China craton to the Tibetan plateau. The corridor passes different tectonic units such as subduction zones, an old continental shield, a fold belt and a high plateau. We aim to get information about the depth and sharpness of the mantle discontinuities at 410 and 660 km and the topography of the mantle transition beneath different geologic units along the corridor and infer geodynamic processes at depth. We also aim to investigate the mantle transition zone thickness beneath continents and oceans as it was suggested that their differences might extend into the mantle transition zone. However, this correlation has not been evident in other studies. High resolution images of SS precursors may also reveal the interaction of the subducted oceanic lithosphere with the mantle transition zone and serve to answer the often debated question about the scale and extent of the slab stagnation within the mantle transition zone beneath the NW Pacific subduction zone.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 8
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    In:  AGU 2008 Joint Assembly (Fort Lauderdale, Florida 2008)
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 9
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/conferenceObject
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  • 10
    Publication Date: 2020-02-12
    Description: We make use of S receiver function to investigate the structure and thickness of the crust and mantle lithosphere in the South American continent and adjacent areas. The Moho discontinuity has been detected at all stations and goes from 18 km beneath the coast of the continent to 80 km in the Andean region. The depth of the lithosphere-asthenosphere boundary can be clearly detected below those stations that are located on stable areas from 50 km to 160 km. The identification of this phase becomes more difficult when the stations are located near subduction zones. We also observed the base of the subducted oceanic lithosphere down to depths of 220 km.
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
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