NO. 2 BIBLIOGRAPITY OF TIN — HESS 195 



GENERAL BIBLIOGRAPHY (Continued) 



1311. Clarke, Fbank W. The data of geochemistry. 



U. S. Geol. Surv. Bull. 330, 190S, Washington, D. C, pp. 591-595. 



Treats the principal known minerals of tin; the artificial production of cassiterite; 

 the solubility of cassiterite; rocks in which tin ores occur; and the associated minerals. 

 Many bibliographic references. 



1312. CoTTA, Bernaed von. a treatise on ore deposits. 



Translated from 2d German Edition by F. Prime, 1870, New York, pp. 553. 



Treats of tin deposits; modes of occurrence; relation of the rocks to the ore 

 deposits; distribution of ores in deposits; tin of Germany, France, Cornwall and 

 Finland. 



1313. D'Ac'iiiARDi, Antonio. I metalli loro minerali e miniere. 



Vol. II, 1883, Milan, pp. 522-559. 



Gives a general treatment of tin as a metal and then of its minerals, cassiterite and 

 stannite, and accompanying minerals. Gives descriptions of deposits in Italy, Great 

 Britain, France, Spain, Portugal, Germany, Austria, Siberia, Cliina, Japan, India, 

 Siam, Malay Peninsula, East Indies, Queensland, Victoria, Tasmania, Bolivia and the 

 United States followed by generalizations upon the deposits. 



1314. Daubree, a. Memoire sur le gisement, la constitution, et I'origine des 



amas de minerai d'etain. 



Ann. Mines, 3d ser.. Vol. 20, 1841, Paris, pp. 65-112. 



Extrait par I'auteur, C. R. Acad. Sci., Vol. 12, 1841, Paris, pp. 886-890. 



Extrait: Bull. Soc. Geol. France, 1st ser., Vol. 12, 1841, Paris, pp. 393-401. 



Also, Edinburgh, New Philos. Journ., Vol. 32, 1842, Edinburgh, pp. 154-159. 



Translation, Mg. Journ. Railw. Cornm. Gaz., Vol. 12, 1842, London, pp. 9-10. 



" In the above memoir DaubrOe describes the mode of occurrence of tin ore in 

 certain stockworks in Saxony, Bohemia, Cornwall and France. He shows that, after 

 quartz, the minerals most frequently accompanying tin ore are compounds containing 

 fluorine, principally fluosilicates (lepidolite, topaz), sometimes fiuophosphates (apatite) 

 and fluorides (fluorspar). The element boron (tourmaline, axinite) is often abundant. 

 The other elements most commonly met with are tungsten, molybdenum, phosphorus, 

 arsenic and iron. Daubrfe draws the conclusion that the tin ore, fluorine com- 

 pounds, and borosilicates owe their origin to the same set of reactions. He supposes 

 that the tin, tungsten, molybdenum, boron, phosphorus, and some of the silicon came 

 up through fissures from some deep seated source as fluorides. Finally, Daubree 

 suggests that the present condition of the stockworks, which consist of quartz, tin 

 ore, silicates, fluosilicates and borosilicates, resulted from the reactions of these 

 fluorides, probably in the presence of water, on the enclosing rocks." — C. Le Neve 

 Foster. 



1315. . Ueber Zusammensetzung und Entstehung der Zinnerzlager- 



statten. 



(From Dufrenoy's report to the Paris Academy, 1841.) Institut Vol. 9, 1841, Paris, 

 pp. 36.5-366. 



Abstract: Neues .lahrb. Min., 1842, Stuttgart, p. 609-610. 



General discussion as to the manner in which tin occurs in different deposits of the 

 world. 



1316. . Etudes synthetiques de gSologie experimentale. 



1879, Paris, pp. 24, 37, 67-68, 113, 594. 



Treats of tin oxide in veins, the artificial production of tin oxide, its presence in 

 kaolin in Allier, occurrence of tin in Central France, the occurrence of tin in an 

 altered lead in Bourbonne, also the presence of tin in meteorites. 



