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Volumn 192, Issue 4, 2001, Pages 471-483

Subduction-like fluids in the genesis of Mt. Etna magmas: Evidence from boron isotopes and fluid mobile elements

Author keywords

B 11 B 10; Boron; Fluid phase; Geodynamics; Isotope ratios; Mount etna; Subduction

Indexed keywords

BORON; ISOTOPIC COMPOSITION; NEODYMIUM; PETROGENESIS; SUBDUCTION;

EID: 0035194839     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(01)00487-3     Document Type: Article
Times cited : (123)

References (50)
  • 2
  • 41
    • 84879882742 scopus 로고
    • Boron-isotope evidence of Halmahera arc (Indonesia) lavas evidences for involvement of the subducted slab
    • (1991) Geology , vol.19 , pp. 215-217
    • Palmer, M.R.1
  • 42
    • 0028169520 scopus 로고
    • Origin of the slab component in arc lavas from across-arc variation of B and Pb isotopes
    • (1994) Nature , vol.370 , pp. 205-208
    • Ishikawa, T.1    Nakamura, E.2
  • 45
    • 84879879021 scopus 로고    scopus 로고
    • Two isotopically distinct fluid components involved in the Mariana arc evidence from Nb/B ratios and B, Sr, Nd, and Pb isotope systematics
    • (1999) Geology , vol.27 , pp. 83-86
    • Ishikawa, T.1    Tera, F.2
  • 46
    • 0000042425 scopus 로고
    • Neogene-Quaternary magmatism of the Tyrrhenian region: Characterization of the magma sources and geodynamic implications
    • (1990) Mem. Soc. Geol. It , vol.41 , pp. 219-242
    • Serri, G.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.