| 1. |
宮本知治・中村啓太郎・星野惠美・島田允堯, 福岡城上之橋御門石垣石材の岩石記載とその産地についての考察（福岡城上之橋御門石垣石材調査報告）．, 九州大学大学院理学研究院研究報告（地球惑星科学）, 24, 1, 1-17, 24(1)，1-17．, 2021.03.  |
| 2. |
宮本 知治, 中村啓太郎, 星野惠美, 島田 允堯, 福岡城上之橋御門石垣石材から見た産地の考察, 月刊地球, 66, 8月, 21-29, 2016.08, Abstract
As for the building stones used for the stone-wall of the Kami-no-hashi Gateway of Fukuoka Castle, so many granitic rocks and subsequent dioritic to gabbroic plutonic rocks were used, with small amount of alkali basalt, serpentinite, conglomerate, sandstone, and silicified wood. Most of the granitic rocks had leucocratic surface with pale-pink colored porphyritic potassium feldspar, with minor amounts of dark brown tabular crystals and less columnar crystals with dark green color, and some of the rocks had grayish surface. The leucocratic granitic rocks were mostly common hornblende-biotite granodiorite to adamellite, on the other hand, the dioritic to gabbroic plutonic rocks were almost grouped into common hornblende quartz diorite, on the QFM diagram. Major element compositions of the plutonic rocks used for the stone-wall were coincident with those of the Shikanoshima granodiorites and Shikanoshima basic rocks occurred on the northern area of the Hakata Bay, Fukuoka City. Since the stone-wall of the Kami-no-hashi Gateway of Fukuoka Castle were also built from alkali basalt and serpentinite which were found around the Hakata Bay area as well as the plutonic rocks, the building stones of the wall were probably provided from the Miyanoura on Itoshima Peninsula and Shikanoshima Island, and supplemented by various rocks from neighbor areas at the northern Hakata Bay.. |
| 3. |
Miyamoto, T., Hamamoto, R., and Yanagi, T., Sr and Nd isotope compositions of atmospheric mineral dust at the summit of Mt. Sefuri, north Kyushu, southwest Japan: a marker of the dust provenance and seasonal variability. , Geochimica et Cosmochimica Acta, 74, 1471-1484. , 2010.03. |
| 4. |
Miyamoto, T., Satish-Kumar, M., Dunkley, D. J., Osanai, Y., Yoshimura, Y., Motoyoshi, Y., and Carson, C. J., Post-peak (Geodynamic evolution of East Antarctica: A key to the East-West Gondwana connection. Geological Society, London, Special Publications., SP308, 165-181, 2008.11. |
| 5. |
Miyamoto, T., Osanai, Y., Nguyen Thi Minh, Nakano, N., Owada, M., Tran Ngoc Nam., Isotope compositions of mineral fractions in metamorphic rocks from Po Ko and Dien Bien Phu regions: a preliminary report for geochronological research of Indochina Peninsula. , Journal of Geology in Vietnam, Ser. A, No.296, 38-45, 2006.11. |
| 6. |
Miyamoto, T., Yoshimura, Y., Dunkley, D. J., Motoyoshi, Y. and Carson, C. J., Mineral ages for multi isotope system in phlogopite-bearing pyroxene granulite and felsic gneiss, the Howard Hills, Enderby Land, East Antarctica: Possible Proterozoic tectonothermal events in the Napier Complex., Polar Geosciences, Vol.19, page, 152-172., 2006.10. |
| 7. |
Miyamoto, T., Yoshimura, Y., Sato, K., Motoyoshi, Y., Dunkley, D. J. and Carson, C. J., Occurrences of metamorphosed ultramafic rock and associating rocks in Howard Hills, Enderby Land, East Antarctica: An evidence of partial melting on their geochemical and isotopic characters., Polar Geoscience, 17, 88-111., 2004.10. |
| 8. |
Miyamoto, T., Grew, E. S., Sheraton, J. W., Yates, M. G., Dunkley, D. J., Carson, C. J., Yoshimura, Y. and Motoyoshi, Y., Lamproite dykes in the Napier Complex at Tonagh Island, Enderby Land, East Antarctica., Polar Geoscience., 13, 41-59., 13, 41-59., 2000.10. |
| 9. |
Miyamoto, T. and Yanagi, T., U-Pb dating of detrital zircons from the Sangun metamorphic rocks, Kyushu, Southwest Japan: An evidence for 1.9-2.0 Ga granite emplacement in the provenance., Geochemical Journal, 30, 5, 261-271, 30, 261-271., 1996.09. |
