ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

Your search history is empty.
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Language
  • 1
    Call number: 9783319578224 (e-book)
    Description / Table of Contents: This volume presents a collection of contributions that were published in "Pure and Applied Geophysics - pageoph" and which deals with the major earthquake that hit Illapel, Chile on September 16, 2015 with magnitude 8.3, and associated trans-oceanic tsunami. The subducting Nazca plate beneath the Andes caused this major earthquake, generating strong shaking, permanent deformation, free oscillations of the Earth, and tsunamis. This event occurred in the flat-angle subducting segment of the plate.The generated tsunami spread throughout the entire Pacific Ocean and was recorded by numerous coastal tide gauges and open-ocean DART stations. All articles give an up-to-date account of research in one of the most active seismic zones worldwide. An introductory article by Kenji Satake rounds this collection off.
    Type of Medium: 12
    Pages: 1 Online-Ressource (XI, 335 Seiten) , Illustrationen
    Edition: previously published in Pure and Applied Geophysics (PAGEOPH)
    ISBN: 9783319578224 , 978-3-319-57822-4
    ISSN: 2504-3625 , 2504-3633
    Series Statement: Pageoph topical volumes
    Language: English
    Note: Contents Preface A Review of Source Models of the 2015 Illapel, Chile Earthquake and Insights from Tsunami Data / Kenji Satake and Mohammad Heidarzadeh, DOI: 10.1007/s00024-016-1450-5 Rapidly Estimated Seismic Source Parameters for the 16 September 2015 Illapel, Chile Mw 8 3 Earthquake / Lingling Ye, Thorne Lay, Hiroo Kanamori and Keith D. Koper, DOI: 10.1007/s00024-015-1202-y Rupture Process During the 2015 Illapel, Chile Earthquake: Zigzag-Along-Dip Rupture Episodes / Ryo Okuwaki, Yuji Yagi, Rafael Aránguiz, Juan González and Gabriel González, DOI: 10.1007/s00024-016-1271-6 Imaging Rupture Process of the 2015 Mw 8 3 Illapel Earthquake Using the US Seismic Array / Bo Li and Abhijit Ghosh, DOI: 10.1007/s00024-016-1323-y Interseismic Coupling, Megathrust Earthquakes and Seismic Swarms Along the Chilean Subduction Zone (38°–18°S) / M. Métois, C. Vigny and A. Socquet, DOI: 10.1007/s00024-016-1280-5 Low-Frequency Centroid Moment Tensor Inversion of the 2015 Illapel Earthquake from Superconducting-Gravimeter Data / Eliška Zábranová and Ctirad Matyska, DOI: 10.1007/s00024-016-1252-9 Coseismic Fault Slip of the September 16, 2015 Mw 8 3 Illapel, Chile Earthquake Estimated from InSAR Data / Yingfeng Zhang, Guohong Zhang, Eric A. Hetland, Xinjian Shan, Shaoyan Wen and Ronghu Zuo, DOI: 10.1007/s00024-016-1266-3 Analysis of the Illapel Mw = 8 3 Thrust Earthquake Rupture Zone Using GOCE-Derived Gradients / Orlando Álvarez, Agustina Pesce, Mario Gimenez, Andres Folguera, Santiago Soler and Wenjin Chen, DOI: 10.1007/s00024-016-1376-y Chile2015: Lévy Flight and Long-Range Correlation Analysis of Earthquake Magnitudes in Chile / Maria P. Beccar-Varela, Hector Gonzalez-Huizar, Maria C. Mariani, Laura F. Serpa and Osei K. Tweneboah, DOI: 10.1007/s00024-016-1334-8 Time-Based Network Analysis Before and After the Mw 8 3 Illapel Earthquake 2015 Chile / Denisse Pastén, Felipe Torres, Benjamín Toledo, Víctor Muñoz, José Rogan and Juan Alejandro Valdivia, DOI: 10.1007/s00024-016-1335-7 Chilean Earthquakes: Aquifer Responses at the Russian Platform / Alina Besedina, Evgeny Vinogradov, Ella Gorbunova and Igor Svintsov, DOI: 10.1007/s00024-016-1256-5 Ionospheric Plasma Response to Mw 8 3 Chile Illapel Earthquake on September 16, 2015 / C. D. Reddy, Mahesh N. Shrivastava, Gopi K. Seemala, Gabriel González and Juan Carlos Baez, DOI: 10.1007/s00024-016-1282-3 Remote Sensing of Atmospheric and Ionospheric Signals Prior to the Mw 8 3 Illapel Earthquake, Chile 2015 / Mohammad Reza Mansouri Daneshvar and Friedemann T. Freund, DOI: 10.1007/s00024-016-1366-0 Chile2015: Induced Magnetic Fields on the Z Component by Tsunami Wave Propagation / V. Klausner, T. Almeida, F. C. De Meneses, E. A. Kherani, V. G. Pillat and M. T. A. H. Muella, DOI: 10.1007/s00024-016-1279-y First Report on Seismogenic Magnetic Disturbances over Brazilian Sector / V. Klausner, T. Almeida, F. C. De Meneses, E. A. Kherani, V. G. Pillat, M. T. A. H. Muella and P. R. Fagundes, DOI: 10.1007/s00024-016-1455-0 The 16 September 2015 Chile Tsunami from the Post-Tsunami Survey and Numerical Modeling Perspectives / Rafael Aránguiz, Gabriel González, Juan González, Patricio A. Catalán, Rodrigo Cienfuegos, Yuji Yagi, Ryo Okuwaki, Luisa Urra, Karla Contreras, Ian Del Rio and Camilo Rojas, DOI: 10.1007/s00024-015-1225-4 Field Survey of the 2015 Chile Tsunami with Emphasis on Coastal Wetland and Conservation Areas / Manuel Contreras-López, Patricio Winckler, Ignacio Sepúlveda, Adolfo Andaur-Álvarez, Fernanda Cortés-Molina, Camila J. Guerrero, Cyntia E. Mizobe, Felipe Igualt, Wolfgang Breuer, José F. Beyá, Hernán Vergara and Rodrigo Figueroa-Sterquel, DOI: 10.1007/s00024-015-1235-2 A Study of the 2015 Mw 8 3 Illapel Earthquake and Tsunami: Numerical and Analytical Approaches / Mauricio Fuentes, Sebastián Riquelme, Gavin Hayes, Miguel Medina, Diego Melgar, Gabriel Vargas, José González and Angelo Villalobos, DOI: 10.1007/s00024-016-1305-0 Real-Time Assessment of the 16 September 2015 Chile Tsunami and Implications for Near-Field Forecast / Liujuan Tang, Vasily V. Titov, Christopher Moore and Yong Wei, DOI: 10.1007/s00024-015-1226-3 . Comparison Between Tsunami Signals Generated by Different Source Models and the Observed Data of the Illapel 2015 Earthquake / Ignacia Calisto, Matthew Miller and Iván Constanzo, DOI: 10.1007/s00024-016-1253-8 Tsunami Characteristics Along the Peru–Chile Trench: Analysis of the 2015 Mw8 3 Illapel, the 2014 Mw8 2 Iquique and the 2010 Mw8 8 Maule Tsunamis in the Near-field / R. Omira, M. A. Baptista and F. Lisboa, DOI: 10.1007/s00024-016-1277-0 Tsunami Penetration in Tidal Rivers, with Observations of the Chile 2015 Tsunami in Rivers in Japan / Elena Tolkova, DOI: 10.1007/s00024-015-1229-0
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2005
    Keywords: Earthquake ; Tsunami(s) ; Earthquake hazard ; Indonesia ; Banda ; Aceh ; seismic Moment ; Surface waves ; Source ; Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; slow ; red ; silent ; contribution ; Camp
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2012-06-28
    Description: SUMMARY Global gravity field models, derived from satellite measurements integrated with terrestrial observations, provide a model of the Earth's gravity field with high spatial resolution and accuracy. The Earth Gravity Model EGM08, a spherical harmonic expansion of the geopotential up to degree and order 2159, has been used to calculate two functionals of the geopotential: the gravity anomaly and the vertical gravity gradient applied to the South Central Andes area. The satellite-only field of the highest resolution has been developed with the observations of satellite GOCE, up to degree and order 250. The topographic effect, a fundamental quantity for the downward continuation and validation of satellite gravity gradiometry data, was calculated from a digital elevation model which was converted into a set of tesseroids. This data is used to calculate the anomalous potential and vertical gravity gradient. In the Southern Central Andes region the geological structures are very complex, but not well resolved. The processing and interpreting of the gravity anomaly and vertical gradients allow the comparison with geological maps and known tectonic structures. Using this as a basis, a few features can be clearly depicted as the contact between Pacific oceanic crust and the Andean fold and thrust belt, the seamount chains over the Oceanic Nazca Plate, and the Famatinian and Pampean Ranges. Moreover the contact between the Rio de la Plata craton and the Pampia Terrain is of great interest, since it represents a boundary that has not been clearly defined until now. Another great lineament, the Valle Fertil-Desaguadero mega-lineament, an expression of the contact between Cuyania and Pampia terranes, can also be clearly depicted. The authors attempt to demonstrate that the new gravity fields can be used for identifying geological features, and therefore serve as useful innovative tools in geophysical exploration.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2011-03-01
    Description: A gravimetric study was carried out in a region of the Central Andean Range between 28∘ and 32∘ south latitudes and from 72∘ and 66∘ west longitudes. The seismological and gravimetrical Moho models were compared in a sector which coincides with the seismological stations of the CHARGE project. The comparison reveals discrepancies between the gravity Moho depths and those obtained from seismological investigations (CHARGE project), the latter giving deeper values than those resulting from the gravimetric inversion. These discrepancies are attenuated when the positive gravimetric effect of the Nazca plate is considered. Nonetheless, a small residuum of about 5 km remains beneath the Cuyania terrane region, to the east of the main Andean chain. This residuum could be gravimetrically justified if the existence of a high density or eclogitized portion of the lower crust is considered. This result differed from the interpretations from Project “CHARGE” which revealed that the entire inferior crust extending from the Precordillera to the occidental “Sierras Pampeanas” could be “eclogitized”. In this same sector, we calculated the effective elastic thickness (Te) of the crust. These results indicated an anomalous value of Te = 30 km below the Cuyania terrane. This is further conclusive evidence of the fact that the Cuyania terrane is allochthonous, for which also geological evidences exist.
    Print ISSN: 1687-885X
    Electronic ISSN: 1687-8868
    Topics: Geosciences
    Published by Hindawi
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2015-06-27
    Description: The determination of the crustal structure is essential in geophysics, as it gives insight into the geohistory, tectonic environment, geohazard mitigation, etc. Here we present the latest advance on three-dimensional modeling representing the Tibetan Mohorovičić discontinuity (topography and ranges) and its deformation (fold), revealed by analyzing gravity data from GOCE mission. Our study shows noticeable advances in estimated Tibetan Moho model which is superior to the results using the earlier gravity models prior to GOCE. The higher quality gravity field of GOCE is reflected in the Moho solution: we find that the Moho is deeper than 65 km, which is twice the normal continental crust beneath most of the Qinghai-Tibetan plateau, while the deepest Moho, up to 82 km, is located in western Tibet. The amplitude of the Moho fold is estimated to be ranging from −9 km to 9 km with a standard deviation of ~2 km. The improved GOCE gravity derived Moho signals reveal a clear directionality of the Moho ranges and Moho fold structure, orthogonal to deformation rates observed by GPS. This geophysical feature, clearly more evident than the ones estimated using earlier gravity models, reveals that it is the result of the large compressional tectonic process. Scientific Reports 5 doi: 10.1038/srep11681
    Electronic ISSN: 2045-2322
    Topics: Natural Sciences in General
    Published by Springer Nature
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2011-10-13
    Description: The crustal structure of northern Africa is puzzling, large areas being of difficult access and concealed by the Sahara. The new global gravity models are of unprecedented precision and spatial resolution and offer a new possibility to reveal the structure of the lithosphere beneath the Sahara. The gravity gradients correlate better than gravity with geological features such as rifts, fold belts and magmatic deposits and intrusions. They are an ideal tool to follow geological units (e.g. basement units) below a stratigraphic layer of varying density (e.g. sediments). We focus on the Chad lineament, a 1300 km arcuate feature located between the west and central African rift system. The gravity fields show differences between the lineament and the west and central African rift system. Along the centre of the lineament high-density rocks must be present, which relate to either magmatic or metamorphic rocks. This is very different to the lineaments of the western and central-west African rift system which are filled with sediments. Considering present models of rifting and the absence of topography, the lineament cannot be coeval to the west and central African rift system and is most likely older. We suggest that the lineament is a structural element of the Saharan Metacraton.
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2017-02-01
    Print ISSN: 2038-1719
    Electronic ISSN: 2038-1727
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
  • 9
    Publication Date: 2014-12-12
    Print ISSN: 0583-6050
    Electronic ISSN: 1580-2612
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2014-09-02
    Print ISSN: 0583-6050
    Electronic ISSN: 1580-2612
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...