Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol P (Space and Planetary Sciences) » P-PS Planetary Sciences

[P-PS25_2AM2] Meteorite anatomy: synthetic analyses of solar system matter

Fri. May 2, 2014 11:00 AM - 12:45 PM 213 (2F)

Convener:*Yusuke Seto(Graduate School of Science, Kobe University), Tomohiro Usui(Department of Earth and Planetary Sciences,Tokyo Institute of Technology), Shoichi Itoh(Graduate school of Science, Kyoto University), Hikaru Yabuta(Osaka University, Department of Earth and Space Science), Hitoshi Miura(Graduate School of Natural Sciences, Department of Information and Biological Sciences, Nagoya City University), Chair:Hitoshi Miura(Graduate School of Natural Sciences, Department of Information and Biological Sciences, Nagoya City University), Hikaru Yabuta(Osaka University, Department of Earth and Space Science)

12:30 PM - 12:45 PM

[PPS25-14] C-XANES analyses of carbonaceous solid inclusions from Monahans halite

*Yoko KEBUKAWA1, Michael ZOLENSKY2, David KILCOYNE3, Zia RAHMAN4, Marc FRIES2, George CODY5 (1.Department of Natural History Sciences, Hokkaido University, 2.NASA Johnson Space Center, 3.Lawrence Berkeley National Laboratory, 4.Jacobs-Sverdrup, 5.Geophysical Laboratory, Carnegie Institution of Washington)

Keywords:C-XANES, Halite, Carbon, Chondrite, Organic matter

Monahans meteorite (H5) contains fluid inclusion-bearing halite (NaCl) crystals [1]. Microthermometry and Raman spectroscopy showed that the fluid in the inclusions is an aqueous brine and they were trapped near 25oC [1]. Their continued presence in the halite grains requires that their incorporation into the H chondrite asteroid was post metamorphism [2]. Abundant solid inclusions are also present in the halites. The solid inclusions include abundant and widely variable organics [2]. Analyses by Raman microprobe, SEM/EDX, synchrotron X-ray diffraction and TEM reveal that these grains include macromolecular carbon similar in structure to CV3 chondrite matrix carbon, aliphatic carbon compounds, olivine (Fo99-59), high- and low-Ca pyroxene, feldspars, magnetite, sulfides, lepidocrocite, carbonates, diamond, apatite and possibly the zeolite phillipsite [3]. Here we report organic analyses of these carbonaceous residues in Monahans halite using C-, N-, and O- X-ray absorption near edge structure (XANES). Approximately 100 nm-thick sections were extracted with a focused ion beam (FIB) at JSC from solid inclusions from Monahans halite. The sections were analyzed using the scanning transmission X-ray microscope (STXM) on beamline 5.3.2.2 at the Advanced Light Source, Lawrence Berkeley National Laboratory for XANES spectroscopy. C-XANES spectra of the solid inclusions show micrometer-scale heterogeneity, indicating that the macromolecular carbon in the inclusions have complex chemical variations. C-XANES features include 284.7 eV assigned to aromatic C=C, 288.4-288.8 eV assigned to carboxyl, and 290.6 eV assigned to carbonate. The carbonyl features obtained by C-XANES might have been caused by the FIB used in sample preparation. No specific N-XANES features are observed. Various degrees of 1s-σ* exciton shown in the C-XANES spectra indicate that the solid inclusions contain macromolecular carbon which experienced various degree of thermal processing. The natures of the macromolecular carbon in the solid inclusions observed by C-XANES are consistent with the previous studies showing that the solid inclusions have not originated from Monahans parent body [1-3].References: [1] Zolensky et al. 1999. Science 285: 1377-1379. [2] Fries et al. 2011. 74th MetSoc #5390. [3] Zolensky et al. 2013. 76th MetSoc #5200.