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(1914) 朝鮮の鑛物産出状態. The Journal of the Geological Society of Japan, 21 (254) 463-474 doi:10.5575/geosoc.21.463

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Reference TypeJournal (article/letter/editorial)
Title朝鮮の鑛物産出状態
JournalThe Journal of the Geological Society of Japan
Year1914Volume21
Issue254
PublisherThe Geological Society of Japan
DOIdoi:10.5575/geosoc.21.463
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Mindat Ref. ID917423Long-form Identifiermindat:1:5:917423:2
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Full Reference(1914) 朝鮮の鑛物産出状態. The Journal of the Geological Society of Japan, 21 (254) 463-474 doi:10.5575/geosoc.21.463
Plain Text(1914) 朝鮮の鑛物産出状態. The Journal of the Geological Society of Japan, 21 (254) 463-474 doi:10.5575/geosoc.21.463
In(1914) The Journal of the Geological Society of Japan Vol. 21 (254) The Geological Society of Japan

See Also

These are possibly similar items as determined by title/reference text matching only.

(1912) 朝鮮に於ける石墨の産出の状態. The Journal of the Geological Society of Japan, 19 (220) 15-24 doi:10.5575/geosoc.19.15
(1914) 朝鮮鑛物報告. The Journal of the Geological Society of Japan, 21 (249) 254-258 doi:10.5575/geosoc.21.254
(1914) 朝鮮鑛物報告(第三回) The Journal of the Geological Society of Japan, 21 (254) 499-502 doi:10.5575/geosoc.21.499
(1901) 鹿谷(ロクヤ)鑛山の鑛物及其現出の状態. The Journal of the Geological Society of Japan, 8 (88) 61-63 doi:10.5575/geosoc.8.61
(1914) 朝鮮鑛物報告(第二回) The Journal of the Geological Society of Japan, 21 (252) 384-391 doi:10.5575/geosoc.21.384
(1918) 朝鮮産鑛物標本雜記 第一. The Journal of the Geological Society of Japan, 25 (294) 97-102 doi:10.5575/geosoc.25.97
(1915) 福地氏の朝鮮鑛物誌の補遺. The Journal of the Geological Society of Japan, 22 (266) 403-412 doi:10.5575/geosoc.22.403
Ni, K. (1900) 石墨産出の状態. The Journal of the Geological Society of Japan, 7 (78) 100-102 doi:10.5575/geosoc.7.78_100
(1922) 柘榴石の産出状態に就て(一) The Journal of the Geological Society of Japan, 29 (341) 62-71 doi:10.5575/geosoc.29.62
(1922) 柘榴石の産出状態に就て(二) The Journal of the Geological Society of Japan, 29 (342) 100-114 doi:10.5575/geosoc.29.100
(1929) 朝鮮産含チタン磁鐵鑛の加熱實驗報告. The Journal of the Geological Society of Japan, 36 (424) 12-29 doi:10.5575/geosoc.36.12
 
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