• Home
  • Communities & Collections
  • All of DSpace
  1. Portal IGP
  2. Home
  3. Browse by Author

Browsing by Author "Skinner, Steven"

Now showing 1 - 1 of 1
Results Per Page
Sort Options
  • Loading...
    Thumbnail Image
    ItemRestricted
    Structure of the subduction system in southern Peru from seismic array data
    (American Geophysical Union, 2012-11-28) Phillips, Kristin; Clayton, Robert W.; Davis, Paul; Tavera, Hernando; Guy, Richard; Skinner, Steven; Stubailo, Igor; Audin, Laurence; Aguilar, Victor
    The subduction zone in southern Peru is imaged using converted phases from teleseismic P, PP, and PKP waves and P wave tomography using local and teleseismic events with a linear array of 50 broadband seismic stations spanning 300 km from the coast to near Lake Titicaca. The slab dips at 30° and can be observed to a depth of over 200 km. The Moho is seen as a continuous interface along the profile, and the crustal thickness in the back-arc region (the Altiplano) is 75 km thick, which is sufficient to isostatically support the Andes, as evidenced by the gravity. The shallow crust has zones of negative impedance at a depth of 20 km, which is likely the result of volcanism. At the midcrustal level of 40 km, there is a continuous structure with a positive impedance contrast, which we interpret as the western extent of the Brazilian Craton as it underthrusts to the west. Vp/Vs ratios estimated from receiver function stacks show average values for this region with a few areas of elevated Vp/Vs near the volcanic arc and at a few points in the Altiplano. The results support a model of crustal thickening in which the margin crust is underthrust by the Brazilian Shield.
    Palabras clave:SubductionReceiver functionsLithosphere
CONTÁCTANOS
  • Lunes a Viernes de 08:30 a 16:30

  • Calle Badajoz Nº 169 Urb. Mayorazgo IV Etapa Ate, Lima 15012

  • regen@igp.gob.pe

  • +51 13172300

LINK DE INTERÉS
  • Política de Antisoborno
  • Sistema de Gestión de la Calidad

  • Sistema de Gestión de la información

  • Certificaciones ISO’s
REDES SOCIALES