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(1933) ボーキサイトの成因 (2) The Journal of the Geological Society of Japan, 40 (479) 495-516 doi:10.5575/geosoc.40.495

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Reference TypeJournal (article/letter/editorial)
Titleボーキサイトの成因 (2)
JournalThe Journal of the Geological Society of Japan
Year1933Volume40
Issue479
PublisherThe Geological Society of Japan
DOIdoi:10.5575/geosoc.40.495
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Mindat Ref. ID920511Long-form Identifiermindat:1:5:920511:0
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Full Reference(1933) ボーキサイトの成因 (2) The Journal of the Geological Society of Japan, 40 (479) 495-516 doi:10.5575/geosoc.40.495
Plain Text(1933) ボーキサイトの成因 (2) The Journal of the Geological Society of Japan, 40 (479) 495-516 doi:10.5575/geosoc.40.495
In(1933) The Journal of the Geological Society of Japan Vol. 40 (479) The Geological Society of Japan

See Also

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

(1933) ボーキサイトの成因 (1) The Journal of the Geological Society of Japan, 40 (478) 431-442 doi:10.5575/geosoc.40.431
(1926) 伊豫別子鑛山附近の角閃石の成因. The Journal of the Geological Society of Japan, 33 (399) 483-516 doi:10.5575/geosoc.33.399_483
(1918) アルカリ岩の成因. The Journal of the Geological Society of Japan, 25 (294) 142-144 doi:10.5575/geosoc.25.142
(1894) 石油の成因. The Journal of the Geological Society of Japan, 1 (9) 475-480 doi:10.5575/geosoc.1.475
(1920) タングステン鑛の成因(二) The Journal of the Geological Society of Japan, 27 (318) 114-121 doi:10.5575/geosoc.27.114
(1920) タングステン鑛の成因(三) The Journal of the Geological Society of Japan, 27 (320) 223-229 doi:10.5575/geosoc.27.223
(1920) タングステン鑛の成因(四) The Journal of the Geological Society of Japan, 27 (322) 309-313 doi:10.5575/geosoc.27.322_309
(1920) タングステン鑛の成因(四) The Journal of the Geological Society of Japan, 27 (323) 338-343 doi:10.5575/geosoc.27.323_338
(1893) 陸前松島群島の成因. The Journal of the Geological Society of Japan, 1 (2) 72-75 doi:10.5575/geosoc.1.72
(1922) 石油頁岩の成因と成分. The Journal of the Geological Society of Japan, 29 (342) 114-120 doi:10.5575/geosoc.29.114
(1917) 硫黄鑛床の成因. The Journal of the Geological Society of Japan, 24 (291) 591-596 doi:10.5575/geosoc.24.291_591
 
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