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zadetkov: 957
491.
  • Worldwide morphological var... Worldwide morphological variability in Mid-Pliocene menardellid globorotalids
    Mary, Yannick; Knappertsbusch, Michael Marine micropaleontology, December 2015, 2015-12-00, 20151201, Letnik: 121
    Journal Article
    Recenzirano

    Proper species concepts of planktonic foraminifera are essential for paleo-environmental studies. Although subtle but key differences indicate the existence of sibling species, the quantitative ...
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492.
  • New constraints on Holocene... New constraints on Holocene uplift rates for the Baudo Mountain Range, northwestern Colombia
    González, Juan L.; Shen, Zhixiong; Mauz, Barbara Journal of South American earth sciences, 07/2014, Letnik: 52
    Journal Article
    Recenzirano

    A beach deposit on the southern end of the Baudo Mountain Range, at an elevation of ∼2.0 m above the backshore of the modern beach, was dated at ∼2870 years using optically stimulated luminescence ...
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493.
  • Development of the Gulf of ... Development of the Gulf of Guayaquil (Ecuador) during the Quaternary as an effect of the North Andean block tectonic escape
    Witt, César; Bourgois, Jacques; Michaud, François ... Tectonics, June 2006, Letnik: 25, Številka: 3
    Journal Article
    Recenzirano
    Odprti dostop

    Interpretation of industrial multichannel seismic profiles and well data are used to identify the main tectonic features of the Gulf of Guayaquil (GG) area. These include two E‐W trending major ...
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494.
  • Neotectonics in the foothil... Neotectonics in the foothills of the southernmost central Andes (37°–38°S): Evidence of strike-slip displacement along the Antiñir-Copahue fault zone
    Folguera, Andrés; Ramos, Víctor A.; Hermanns, Reginald L. ... Tectonics, October 2004, Letnik: 23, Številka: 5
    Journal Article
    Recenzirano
    Odprti dostop

    The Antiñir‐Copahue fault zone (ACFZ) is the eastern orogenic front of the Andes between 38° and 37°S. It is formed by an east vergent fan of high‐angle dextral transpressive and transtensive faults, ...
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495.
  • Joint inversion of broadban... Joint inversion of broadband teleseismic and interferometric synthetic aperture radar (InSAR) data for the slip history of the Mw = 7.7, Nazca ridge (Peru) earthquake of 12 November 1996
    Salichon, J.; Delouis, B.; Lundgren, P. ... Journal of Geophysical Research, February 2003, Letnik: 108, Številka: B2
    Journal Article
    Recenzirano
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    The slip distribution of the 12 November 1996, Mw = 7.7, Peru earthquake is determined using broadband teleseismic waveforms, a differential SAR interferogram (interferometric synthetic aperture ...
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496.
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498.
  • Nazca Trophy Head Vessel
    How They Lived : An Annotated Tour of Daily Life through History in Primary Sources: Ancient and Medieval World, 2016
    Reference
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499.
  • Varying mechanical coupling... Varying mechanical coupling along the Andean margin: Implications for trench curvature, shortening and topography
    Iaffaldano, G.; Di Giuseppe, E.; Corbi, F. ... Tectonophysics, 03/2012, Letnik: 526-529
    Journal Article
    Recenzirano

    Convergent margins often exhibit spatial and temporal correlations between trench curvature, overriding plate shortening and topography uplift that provide insights into the dynamics of subduction. ...
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500.
  • A narrowly spaced double-se... A narrowly spaced double-seismic zone in the subducting Nazca plate
    Rietbrock, A.; Waldhauser, F. Geophysical research letters, 20/May , Letnik: 31, Številka: 10
    Journal Article
    Recenzirano
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    High‐precision relocations of intermediate‐depth earthquakes (80–130 km) below the Central Andes reveal a fine‐scale double‐layered Wadati‐Benioff zone (WBZ). Upper and lower band of seismicity are ...
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