| 1. |
TETSUYA NAKANISHI, Geochemical research of pre-modern copper smelting site ”Kamino-Tokoya”, Besshi copper mine, Japan., The 10th International Conference on the Beginnings of the Use of Metals and Alloys (BUMA-X), 2022.07. |
| 2. |
Eiji Izawa, Tetuya Nakanishi, Japanese silver mining from 674 to early seventeenth centuries and lead isotopic ratios of silver ores, 日本鉄鋼協会, 2019.03. |
| 3. |
Seang Sirisokha, TETSUYA NAKANISHI,,KOTARO YONEZU, Akira Imai, Thomas Tindell and Koichiro Watanabe, Hydrothermal alteration, mineralization and fluid inclusion microthermometry of the Halo prospect porphyry copper-molybdenum, Southeast of Cambodia, International Symposium on Earth Science and Technology 2018, 2018.11, The Halo prospect porphyry copper-molybdenum is located in Southeastern part of Cambodia. This prospect is hosted by porphyritic diorite, porphyritic granodiorite, feldspar porphyry, andesite dykes, and rhyolite dykes. The hydrothermal alteration and mineralization can be divided into four stages, stage 1; quartz+magnetite± molybdenite±chalcopyrite ±pyrite vein, stage2; quartz+molybdenite±chalcopyrite±pyrite vein, stage 3; quartz pyrite ±chalcopyrite±sphalerite vein, stage 4; anhydrite±calcite±pyrite vein. Five main alteration assemblages were identified: potassic-sericitic, phyllic, propylitic, intermediate argillic, and silicic alteration. Hydrothermal quartz mainly contains four types of fluid inclusions: type I (liquid+vapor), typeII (liquid+vapor+anhydrite), typeIII (liquid+vapor+opaque) and type IV (liquid+vapor+halite). The homogenization temperatures (Th) (from vapor+liquid to liquid) of type I, type III, and type IV fluid inclusions in quartz veins associated with the potassic-sericitic alteration range from 185 to 309oC, 329 to 400oC and 229 to 460oC with salinity ranging from 2 to 8 wt.% 14 to 17 wt.% 35 to 58 wt.% NaCl equiv., respectively. On the other hand, the Th (from vapor+liquid to liquid) of type I, type II, type III, and type IV fluid inclusions in quartz in the silicic alteration range from 201 to 290oC, 285 oC, 210 to 286oC and 290 to 381oC with salinity ranging from 0.5 to 11 wt. %, 16.wt. %, 8 to 21 wt. %, and 40 to 52 wt. % NaCl equiv., respectively.. |
| 4. |
Seang Sirisokha, Tetsuya Nakanishi, Kotaro Yonezu and Koichiro Watanabe, Initial Study on Alteration and Fluid Inclusion Microthermometry in Oyadav South, Ratanakiri, Cambodia, 10TH AUN/SEED-NET GEOLOGICAL ENGINEERING CONFERENCE, 2017.08. |
| 5. |
TETSUYA NAKANISHI, A comparison of Gold mineralization in Northern and Southern Orogenic belt in Mongolia, 6th Asia Africa Mineral Resources Conference, 2016.09. |
| 6. |
O. Sarantuya, TETSUYA NAKANISHI, Tindell Thomas, Kotaro Yonezu, Koichiro Watanabe, S. Jargalan, Mineralogical Study and Fluid Characteristics of Olon Ovoot Gold Deposit, Southern Mongolia, International Geological Congress, 2016.06. |
| 7. |
O. Sarantuya, TETSUYA NAKANISHI, Tindell Thomas, Kotaro YONEZU, Koichiro Watanabe, S. Jargalan, Ore mineralogy and ore-forming condition of the Olon Ovoot gold deposit, South Mongolia, 資源地質学会第66回年会, 2016.06. |
| 8. |
TETSUYA NAKANISHI, Progress of Mining Activity in Resent Mongolia , 8th IC-GeoE & SIMPOMIN 2015, 2015.09. |
| 9. |
前田淳郎, TETSUYA NAKANISHI, S. Oyungerel, KOTARO YONEZU, S. Jargalan, Gold Mineralization in the Goyot Ulaan Gold Deposit, Southern Mongolia, 8TH AUN/SEED-NET GEOLOGICAL ENGINEERING CONFERENCE, 2015.09. |
| 10. |
前田淳郎, TETSUYA NAKANISHI, Oyungerel, KOTARO YONEZU, S. Jargalan, Geochemistry and mineralization of Goyot Ulaan gold deposit at Gyoto Ulaan open pit in Southern Mongolia, Asia Oceania Geosciences Society (AOGS), 2015.08. |
| 11. |
前田淳郎, TETSUYA NAKANISHI, S. Oyungerel, 米津 幸太郎, TINDELL THOMAS DAVID, Koichiro Watanabe, S. Jargalan, Geochemistry and mineralization of the Goyot Ulaan gold deposit, Southern Mongolia, 資源地質学会第64回年会, 2015.06. |
| 12. |
S. Oyungerel, TETSUYA NAKANISHI, 米津 幸太郎, TINDELL THOMAS DAVID, Koichiro Watanabe, S. Jargalan, Geology and mineralization of the Olon Ovoot gold deposit, South Mongolia, 資源地質学会第64回年会, 2015.06. |
| 13. |
TETSUYA NAKANISHI, The Naganobori copper mine: Ancient copper production of Japan in 8th century, 4th Asia Africa Mineral Resources Conference 2014, 2014.10. |
| 14. |
中西 哲也, 宮本真, 高橋亮平, 田口幸洋, 渡邊 公一郎, 米津 幸太郎, S. Jargalan, Depth and temperature of orogenic gold mineralization around the Yeroogol fault trend,
northern Mongolia, 資源地質学会第64回年会, 2014.06. |
| 15. |
MAKOTO MIYAMOTO, TETSUYA NAKANISHI, RYOHEI TAKAHASHI, Sachihiro Taguchi, KOTARO YONEZU, Koichiro Watanabe, S. Jargalan, Formation of orogenic gold deposit around the Yeroogol trend, northern Mongolia , International Symposium on Earth Science and Technology 2013, 2013.12. |
| 16. |
MAKOTO MIYAMOTO, TETSUYA NAKANISHI, RYOHEI TAKAHASHI, Sachihiro Taguchi, KOTARO YONEZU, Koichiro Watanabe, S. Jargalan, Ore forming condition of orogenic gold deposit around the Yeroogol trend, northern Mongolia, 3rd Asia Africa Mineral Resources Conference, 2013.09. |
| 17. |
TETSUYA NAKANISHI, EIJI IZAWA, Evolution of silver-smelting technology of Japan in the middle of the16th century, The 8th International Conference on the Beginnings of the Use of Metals and Alloys (BUMA-VIII), 2013.09. |
| 18. |
EIJI IZAWA, TETSUYA NAKANISHI, Gold refining by cementation with salt at Sado in early seventeenth century, The 8th International Conference on the Beginnings of the Use of Metals and Alloys (BUMA-VIII), 2013.09. |
| 19. |
Silver ore smelting in pre-modern Japan.. |
| 20. |
Variations of the chemical composition of Japanese early modern silver coin "Ichibu-gin". |
| 21. |
Investigation on mining technology in Early-Modern Japan. |
| 22. |
Transfer of liquation technology (Namban-buki) -An effect of the European copper refining system-. |
| 23. |
Contribution of economic geology to the technological history of mining.. |
