福山繭子博士後研究 福山繭子 博士後研究

 TEL:+886-2-2783-9910 ext. 407
 FAX:+886-2-2783-9871
 E-mail:mayuko@earth.sinica.edu.tw

 研究領域:Mass transfer analysis of a skarn reaction zone using steady-diffusion modelling in an open system.
      Estimate of fluid velocity at a reaction zone using oxygen isotope data.
      Mass transfer of fluid during metamorphic process.

[學 歷]
  • 2005:PhD Science (Earth Science) at Kumamoto University
  • 2002:MSC at Kumamoto University
  • 2002:BSC at Kumamoto University
[Professional Experiences]
  • Since April 2008, Postdoctoral Fellow, Institute of Earth Sciences, Academia Sinica

  • April 2005-May 2008,  Researcher, Geological Survey of Japan

  • July 2000-September 2001, Teaching Assistant
  • July 2002-February 2003, Teaching Assistant
  • May 2004-March 2005 , Research Assistant
[Analytical Experience]
  • Electron microprobe analyzer (JEOL superprobe 8800, JEOL superprobe 8900)

  • Cathode luminescence imaging (originally designed CL detector for EPMA, CL detector for SEM)

  • Secondary ion mass spectrometry (Cameca ims-1270)

  • Solution and laser ablation ICP-MS (Agient7500, New Plasma, NewWave MiniLaser III laser system + VG Elemental PQ3)

  • EDS analysis (LINK ISIS system)

  • SEM (JEOL JSM-5600)

  • XRF analysis

  • XRD analysis

  • Laser Raman analysis

  • X-ray analytical microscope (HORIBA XGT-2000WS)

  • Various sample preparation methods including for EPMA, SIMS, LA-ICP-MS analysis

[學會會員]
  • Geological Society of Japan

  • The Japanese Association of Mineralogists, Petrologists, Economic Geologists.

  • American Geophysical Union

[著 作]

Journal publications
  • Ishiyama D., Miyata M., Shibata S., Satoh H., Mizuta T., Fukuyama M., and Ogasawara M. Geochemical characteristics of Miocene Fe-Cu-Pb-Zn granitoids associated mineralization in the Chichibu skarn deposit (central
    Japan): Evidence for magmatic fluids generation coexisting with granitic melt. Geological Society of London, Special Publications, v.350, p. 68-88. (2011)

  • Fukuyama M., Ogasawara M., Ishiyama D., and Sato H. REE in garnets from skarn and their potential as the resources – Based on the distribution of REE in rock forming minerals-. Chikyu, v. 32, p 476-483. (2010)

  • Fukuyama M., Ogasawara M., Sato H., and Ishiyama D. Trace element analysis of gem garnet by LA-ICP-MS: Preliminary evaluation as micro-beam standard. Bulletin of the geological survey of Japna, 58, pp93-103. (2007)

  • Fukuyama M., Nishiyama T., Urata K., and Mori Y. Steady-diffusion modeling of a reaction zone between a metamorphosed basic dyke and a marble from Hirao-dai, Fukuoka, Japan, Journal of Metamorphic Geology, 24, pp153-168. (2006)

  • Fukuyama M., Urata K., and Nishiyama T. Geology and petrology of the Hirao Limestone and the Tagawa metamorphic rocks – with special reference to the contact metamorphism by Cretaceous granodiorite, Journal of Mineralogical and Petrological Sciences, 99, pp25-41. (2004)

 Proceedings

  • Ishiyama D., Miyata M., Mizuta T., Satoh H., Ogasawara M., and Fukuyama M. Characteristics of fluid coexisting with granitoids associated with Miocene iron-copper-lead-zinc mineralization of the Chichibu skarn deposit Japan. PACRIM Congress. (2008)

Conference Abstracts

  • Fukuyama M. (2009) The age of serpentinization by the SHRIMP dating of zircon from the   rodingite vein and zoisitite in serpentinite of the Nagasaki metamorphic rocks. The Kumamoto International Syposium on Recent Advancements of Mineralogy and Petrology II.

  • Toriumi M. and Fukuyama M. (2009) Symbolic dynamics and configuration of symmetry in the texture. Geoscience Union Meeting, G123-011

  • Fukuyama M. (2009) and Lee D-C. 182Hf-182W Chronometry and the Evolution History in the Howardites. T0he 32nd Symposium on Antratic Meteorite.

  • Lee D-C. and Fukuyama M. (2009) The formation and the differentiation of the howardite based on 182Hf-182W chronometry. Goldschmidt Conference.

  • Fukuyama M., Ogasawara M., Dunkely D., Hokada T., and Lee D-C. (2009) The age of serpentinization by the SHRIMP dating of zircon from the metasomatic rocks in serpentinite. Goldschmidt Conference.

  • Fukuyama M. (2008) U-Pb dating of serpentinization – hydrothermal zircon from metasomatic rocks, rodingite and zoisite rock in Nagasaki metamorphic rocks. NIPR-SHRIMP workshop 2008.

  • Fukuyama M. (2008) Miyazaki K., Ogasawara M., Morishita Y., and Nishiyama T. Fluid flow meter using chemical and isotope mobility in a reaction zone. Geoscience Union Meeting, G210-004.

  • Fukuyama M. (2008) Ogasawara M., Sato H., Ishiyama D., Aoki M., Morishita Y., and Nishiyama T. Distribution of trace elements between garnet and vesuvianite in the skarn: significance of REE behavior. Geoscience Union Meeting, R223-006.

  • Torium M. and Fukuyama M. (2008) Symbolic dynamics in metamorphic rocks 3 – instability of metasomatic banding interface and fluid flux. Geoscience Union Meeting, G210-006.

  • Ishiyama D., Miyata M., Satoh H., and Fukuyama M. (2008) Cathodeluminescence and fluid inclusion studies of granitoids associated with Miocene Fe-Cu-Pb-Zn mineralization of the Chichibu skarn deposit in the active uplifting region of central Japan: Timing of generation of magmatic fluid coexisting with granitic. International Geological Congress Oslo 2008.

  • Toriumi M. and Fukuyama M. (2008) Symbolic dynamics of metamorphic banding 4. The 115th Annual Meeting of the Geological Society of Japan, pp.

  • Ishiyama D., Miyata M., Mizuta T., Satoh H., Ogasawara M., and Fukuyama M. (2008) Characteristics of fluid coexisting with granitoids associated with Miocene iron-copper-lead-zinc mineralization of the Chichibu skarn deposit Japan. PACRIM Congress 2008.

  • Fukuyama M., Ogasawara M., Dunkley D. J., Hokada T., and Lee D. C. (2008) The estimation of the age of serpentinization by the SHRIMP dating of zircon from the rodingite vein and zoisitite in serpentinite of the Nagasaki metamorphic rocks, American Geophysical Union fall meeting.

  • Fukuyama M., Ogasawara M., Sato H., Ishiyama D., Morishita Y., and Nishiyama T. (2007) Trace element behavior in hydrothermal processes: A geochemical study of skarn reaction zone from Hirao-dai, Fukuoka, Japan. Japan Geoscience Union Meeting, G122-P008.

  • Ogasawara M., Sato M., Fukuyama M., Miyagi I., Tsukamoto H., and Hokada T. (2007) Development of a cathode luminescence detector for EPMA to obtain color CL images. Japan Geoscience Union Meeting, K130-P031.

  • Fukuyama M., Ogasawara M., Sato H., Ishiyama D. (2007) Trace element composition of gem garnet: Preliminaly evaluation as micro-beam standards. Annual Meeting for The Society of Resource Geology, pp.111.

  • Ogasawara M., Sato M., Fukuyama M., Miyagi I., and Tsukamoto H. (2007) Color cathodoluminescence (CL) images of rock and ore samples: development and evaluation of a new CL detector for EPMA. Annual Meeting for The Society of Resource Geology, pp.112.

  • Miyata M., Ishiyama D., Mizuta T., Fukuyama M., and Ogasawara M. (2007) Characteristics of magma-hydrothermal system of the Chichibu skarn deposit, Saitama Prefecture, Japan. Annual Meeting for The Society of Resource Geology, pp.95.

  • Ishizeki H., Ishiyama D., Mizuta T., Iai Y., Watanabe Y., Kato A., Fukuyama M., and Ogasawara M. (2007) Formation mechanisms of pores in the altered felsic rocks in gas reservoirs and the difference of alteration style from altered rocks in kuroko area. Annual Meeting for The Society of Resource Geology, pp.41.

  • Fukuyama M., Morishita Y., and Nishiyama T. (2007) Mass transfer by fluid and duration of oxygen isotope exchange during contact metamorphism at Hirao-dai, Japan. Goldschmidt Conference, Geochimica et Cosmochimica Acta. 71, A299,

  • Fukuyama M. (2007) Metasomatic process and characteristic of related fluid for the formation of rodingite and zoicite rocks in the serpentine from Nagasaki metamorphic rock, Nagasaki, Japan. The 114th Annual Meeting of the Geological Society of Japan. The 114th Annual Meeting of the Geological Society of Japan, pp.172.

  • Fukuyama M., Ogasawara M., Morishita Y., and Nishiyama T. (2006) Trace element behavior in the fluid-rock reaction - example of the reaction zone in the Hirao limestone. The 113th Annual Meeting of the Geological Society of Japan, pp.143.

  • Fukuyama M., Urata K., and Nishiyama T. (2004) Steady diffusion model for reaction zone in open system. Annual Meeting for The Japanese Association of Mineralogists, Petrologists and Economic Geologists, pp.195. 

  • Fukuyama M., Nishiyama T., and Urata K. (2002) Reaction zones and composite veins around the metamorphosed basic dykes in the Hirao limestone, Fukuoka, Japan. Goldschmidt conference, Geochimica et Cosmochimica Acta. 66, A250.

  • Fukuyama M., Urata K., and Nishiyama T. (2002) Composite vein derived from reaction zones in metabasite dike. The 109th Annual Meeting of the Geological Society of Japan, pp.171.

  • Fukuyama M., Urata K., and Nishiyama T. (2001) Reaction zone in metabasite dike from the Hirao Limestones. The 104th Annual Meeting of Western Japan in the Geological Society of Japan, pp.21.

  • Fukuyama M., Urata K., and Nishiyama T. (2000) Geological relation between the Sangun Metamorphic Rocks and the Hirao Limsetones, and the contact metamorphism by Cretaceous granite. The 107th Annual Meeting of the Geological Society of Japan, pp.294.

 

Book Review

  • Fukuyama M. Japan’s One Hundred Best Geosites. Chishitsu News, 645, pp. 69. (2008)