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Volumn 101, Issue 2, 2012, Pages 587-594

Reply to the discussion by F. Gutiérrez, P. Lucha, J. Guerrero, M. Gutiérrez and D. Carbonel on the article 'Paleoseismological analysis of an intraplate extensional structure: The Concud fault (Iberian Chain, eastern Spain)'

Author keywords

Fluvial terrace; Normal fault; Paleoseismology; Slip rate

Indexed keywords

COLLUVIAL DEPOSIT; DISPLACEMENT; NORMAL FAULT; PALEOSEISMICITY; SLIP RATE; TERRACE; THEORETICAL STUDY;

EID: 85027937647     PISSN: 14373254     EISSN: 14373262     Source Type: Journal    
DOI: 10.1007/s00531-011-0661-3     Document Type: Article
Times cited : (8)

References (15)
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    • (2005) J Struct Geol , vol.27 , pp. 693-705
    • Arlegui, L.E.1    Simón, J.L.2    Lisle, R.J.3    Orife, T.4
  • 2
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    • Analysis of non-striated faults in a recent extensional setting: the Plio-Pleistocene Concud fault (Jiloca graben, eastern Spain)
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    • (2006) J Struct Geol , vol.28 , pp. 1019-1027
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  • 4
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  • 7
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    • Gutiérrez F, Gutiérrez M, Gracia FJ, McCalpin JP, Lucha P, Guerrero J (2008) Plio- Quaternary extensional seismotectonics and drainage network development in the central sector of the Iberian Chain (NE Spain). Geomorphology 102: 21-42.
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  • 12
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    • Edel J-B, Schulmann K (2007) Paleomagnetic constraints on the evolution of the Variscan belt in Carboniferous times. In: Schulmann K, Ledru P, Faure M, Lardeaux J-M (eds) Mechanics of Variscan Orogeny: a modern view on orogenic research. Orléans, Abstr Vol.
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    • (2005) Geogaceta , vol.38 , pp. 63-66
    • Simón, J.L.1    Lafuente, P.2    Arlegui, L.3    Liesa, C.L.4    Soriano, M.A.5


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.