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Volumn 13, Issue 4, 2001, Pages 235-240

The 18.7 ka phreatomagmatic flank eruption on Etna (Italy): Relationship between eruptive activity and sedimentary basement setting

Author keywords

[No Author keywords available]

Indexed keywords

BASEMENT ROCK; PHREATOMAGMATISM; SEDIMENTARY STRUCTURE; VOLCANIC ERUPTION;

EID: 0035652343     PISSN: 09544879     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-3121.2001.00336.x     Document Type: Article
Times cited : (10)

References (22)
  • 1
    • 0035968485 scopus 로고    scopus 로고
    • An example of river pattern evolution produced during the lateral growth of a central polygenic volcano: The case of the Alcantara river system, Mt Etna (Italy)
    • (2001) Catena , vol.45 , pp. 85-102
    • Branca, S.1    Ferrara, V.2
  • 16
    • 0000341862 scopus 로고
    • Une éruption à caractères Katmaiens, à l'origine de coulées de ponces, responsable de la formation de la caldeira du Cratère Elliptique de L'Etna
    • (1973) C.R. Acad. Sci. Paris , vol.277 D , pp. 2321-2324
    • Kieffer, G.1
  • 20
    • 0007426058 scopus 로고
    • del Monte Etna. Scala 1: 50.000. C.N.R., P.F.G., I.I.V
    • (1982) Mem. Soc. Geol. It , vol.23


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.