U-Pb Dating of Large Zircons in Low-Temperature Jadeitite from the Osayama Serpentinite Mélange, Southwest Japan: Insights into the Timing of Serpentinization

T. Tsujimori, J. G. Liou, J. Wooden, T. Miyamoto

Research output: Contribution to journalArticle

54 Citations (Scopus)

Abstract

Crystals of zircon up to 3 mm in length occur in jadeitite veins in the Osayama serpentinite mélange, Southwest Japan. The zircon porphyroblasts show pronounced zoning, and are characterized by both low Th/U ratios (0.2-0.8) and low Th and U abundances (Th = 1-81 ppm; U = 6-149 ppm). They contain inclusions of high-pressure minerals, including jadeite and rutile; such an occurrence indicates that the zircon crystallized during subduction-zone metamorphism. Phase equilibria and the existing fluid-inclusion data constrain P-T conditions to P > 1.2 GPa at T > 350°C for formation of the jadeitite. Most U/Pb ages obtained by SHRIMP-RG are concordant, with a weighted mean 206Pb/238U age of 472 ± 8.5 Ma (MSWD = 2.7, n = 25). Because zircon porphyroblasts contain inclusions of high-pressure minerals, the SHRIMP U-Pb age represents the timing of jadeitite formation, i.e., the timing of interaction between alkaline fluid and ultramafic rocks in a subduction zone. Although this dating does not provide a direct time constraint for serpentinization, U-Pb ages of zircon in jadeitite associated with serpentinite result in new insights into the timing of fluid-rock interaction of ultramafic rocks at a subduction zone and the minimum age for serpentinization.

Original languageEnglish
Pages (from-to)1048-1057
Number of pages10
JournalInternational Geology Review
Volume47
Issue number10
DOIs
Publication statusPublished - Oct 2005

All Science Journal Classification (ASJC) codes

  • Geology

Fingerprint Dive into the research topics of 'U-Pb Dating of Large Zircons in Low-Temperature Jadeitite from the Osayama Serpentinite Mélange, Southwest Japan: Insights into the Timing of Serpentinization'. Together they form a unique fingerprint.

  • Cite this