WFRF:(Marron M.)
Sökning: WFRF:(Marron M.) > (2004) > The seismic crustal...
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03653naa a2200685 4500 | |
| 001 | oai:DiVA.org:uu-14468 | |
| 003 | SwePub | |
| 008 | 080130s2004 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-144682 URI |
| 040 | a (SwePub)uu | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a ref2 swepub-contenttype |
| 072 | 7 | a art2 swepub-publicationtype |
| 100 | 1 | a Simancas, J.F.4 aut |
| 245 | 1 0 | a The seismic crustal structure of the Ossa-Morena Zone and its geological interpretation |
| 264 | 1 | c 2004 |
| 338 | a print2 rdacarrier | |
| 520 | a The IBERSEIS deep reflection seismic experiment has provided a crustal image of the Variscan orogen of southwest Iberia. A brief presentation of the entire seismic profile is given, and then the Ossa-Morena Zone (OMZ) and its boundaries are considered. The crust of the OMZ is shown to be divided into an upper crust, characterized by dominantly NE-dipping reflectivity, and a poorly reflective lower crust. The reflectivity of the upper crust has good correlation with the geological cross-section constructed from surface mapping. In the seismic image, the upper crustal geological structures are seen to merge in the middle crust. Nevertheless, the OMZ middle crust is not a mere detachment level, as it shows very unusual features: it appears as a band of strong reflectivity and irregular thickness (the Iberian Reflective Body, IRB) that we interpret as a great sill-like intrusion of basic rocks. The boundaries of the OMZ are considered sutures of the orogen, and their geometrical features, as deduced from geological mapping and the seismic image, are in accordance with the transpressional character of the Variscan collision recorded in SW Iberia. The present Moho is flat, obliterating the root of the orogen. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geofysik0 (SwePub)105052 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geophysics0 (SwePub)105052 hsv//eng |
| 653 | a Deep seismic reflection | |
| 653 | a structure of the crust | |
| 653 | a Variscan orogen | |
| 653 | a Ossa-Morena Zone | |
| 700 | 1 | a Carbonell, R.4 aut |
| 700 | 1 | a González Lodeiro, F.4 aut |
| 700 | 1 | a Pérez Estaún, A.4 aut |
| 700 | 1 | a Juhlin, Christopheru Uppsala universitet,Geofysik4 aut0 (Swepub:uu)chrisjuh |
| 700 | 1 | a Ayarza, P.4 aut |
| 700 | 1 | a Azor, A.4 aut |
| 700 | 1 | a Martínez Poyatos, D.4 aut |
| 700 | 1 | a Almodóvar, G.R.4 aut |
| 700 | 1 | a Pascual, E.4 aut |
| 700 | 1 | a Sáez, R.4 aut |
| 700 | 1 | a Kashubin, A.u Uppsala universitet,Geofysik4 aut |
| 700 | 1 | a Alonso, F.4 aut |
| 700 | 1 | a Álvarez Marrón, J.4 aut |
| 700 | 1 | a Bohoyo, F.4 aut |
| 700 | 1 | a Castillo, S.4 aut |
| 700 | 1 | a Donaire, T.4 aut |
| 700 | 1 | a Expósito, I.4 aut |
| 700 | 1 | a Flecha, I.4 aut |
| 700 | 1 | a Galindo Zaldívar, J.4 aut |
| 700 | 1 | a González, F.4 aut |
| 700 | 1 | a González Cuadra, P.4 aut |
| 700 | 1 | a Macías, I.4 aut |
| 700 | 1 | a Martí, D.4 aut |
| 700 | 1 | a Martín, A.4 aut |
| 700 | 1 | a Martín Parra, L.M.4 aut |
| 700 | 1 | a Nieto, J.M.4 aut |
| 700 | 1 | a Palm, H.u Uppsala universitet,Geofysik4 aut |
| 700 | 1 | a Ruano, P.4 aut |
| 700 | 1 | a Ruiz, M.4 aut |
| 700 | 1 | a Toscano, M.4 aut |
| 700 | 1 | a Galadi, E.4 aut |
| 710 | 2 | a Uppsala universitetb Geofysik4 org |
| 773 | 0 | t Journal of Iberian Geologyg 30, s. 133-142q 30<133-142x 1698-6180x 1886-7995 |
| 856 | 4 | u http://digital.csic.es/bitstream/10261/5510/1/JIGE0404120133A.pdf |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-14468 |
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