[R7-06]Melt incusions containing platinum group minerals in Tahitian mantle xenolith[Presentation award entry]
*Itaru Mitsukawa1, Tetsu Kogiso1, Norikatsu Akizawa2, Tomoki Taguchi3, Kentaro Uesugi4, Akihisa Takeuchi4, Masanori Yasutake4, Akira Tsuchiyama5,6, Megumi Matsumoto7, Junya Matsuno6, Shota Okumura1, Yohei Igami1, Akira Miyake1(1. Kyoto Univ., 2. Univ. of Tokyo, 3. Waseda Univ., 4. SPring-8/JASRI, 5. Guangzhou Inst. of Geochem., CAS, 6. Ritsumeikan Univ., 7. Tohoku Univ.)
Keywords:
Platinum Group Minerals,Bitumen,Melt inclusions,Raman spectroscopy,Tahiti Island
Platinum Group Elements (PGE) are important geochemical tracers to constrain Earth's early history. Recently, melt inclusions containing much platinum group minerals are found in a Tahitian harzburgite xenolith. They coexist with Fe-Ni-Cu sulfides, silicate glass and "vapor-like phase". We applied Raman spectroscopy to "vapor-like phase" and obtained spectra resembling to bitumen. However, we couldn't obtain significant signal of carbon with STEM-EDS analysis and "vapor-like phase" should be analyzed more in detail.
