4.3 Article

K-Ar analyses of the post-caldera lavas of Bratan volcano in Bali Island, Indonesia - Ar isotope mass fractionation to light isotope enrichment

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出版社

ELSEVIER SCIENCE BV
DOI: 10.1016/j.jvolgeores.2013.07.002

关键词

Sunda-Banda island arc; Bali island; Bratan volcano; late Pleistocene volcanic rocks; Ar isotope mass fractionation; K-Ar age

资金

  1. JSPS [18404020]
  2. Grants-in-Aid for Scientific Research [23340160, 18404020] Funding Source: KAKEN

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The post-caldera lavas of Bratan volcano in Bali Island, Indonesia were collected for whole rock chemical analyses and K-Ar analyses. Major and trace element chemistry shows that the lavas are basalts to andesites and typical of subduction-related tectonic setting. The Ar-38/Ar-36 ratios are 0.1851 +/- 3-0.1875 +/- 2 and the Ar-40/Ar-36, 294.3 +/- 03-301.6 +/- 0.1, which strongly suggest that the mass fractionation to light isotope enrichment took place. The effect of the groundwater on magma is common on the basis of systematic mass fractionation of the atmospheric Ar enriched in lighter isotopes. This case was under the mass fractionation law analyzed numerically, giving the mass fractionation correction ages (14 +/- 15, 31 +/- 6, 55 +/- 22, 66 +/- 23, 94 +/- 32 and 125 +/- 51 ka) consistent with the volcano stratigraphy though the magma composition that changed frequently in time. (C) 2013 Elsevier B.V. All rights reserved.

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