INTRODUCTION
| Bibliography (251-285) | ||
| 251. | Palache, Charles, and Berman, Harry, Crystallographic notes1, 2, Hematite; 3, willemite; 4, hedyphane: American Mineralogist, volume 12, pages 180187. Gives the results of crystallographic measurements of fine specimens from the Franklin district. | |
| 252. | Palache, Charles, and Bauer, L. H., Mcgovernite, a new from Sterling Hill, N.J.: American Mineralogist, volume 12, pages 373374. Describes for the first time and names the mineral; gives its occurrence, optical character, and composition; and discusses the complex formula derived. | |
| 253. | Shuster, E. D., Historical notes of the iron and zinc mining industry in Sussex County, N.J., privately printed. An elaborate compilation of the history of the discovery, development, and ownership of and the litigation regarding the iron and zinc mines of Sussex County, by a member of the surveying staff of the New Jersey Zinc Co. | |
| 254. | Spencer, L. J., South African occurrences of willemite; fluorescence of willemite and some other zinc minerals in ultraviolet rays: Mineralogical Magazine, volume 21, pages 388396. The second part of the paper described the fluorescence of willemite, including material from Franklin. See Palache (258). | |
| 254a. | Gordon, S. G., The probable identity of gageite with tephroite: Academy of Natural Sciences Philadelphia Proc., volume 79 [for 1927], pages 207208, 1928. Suggests identity on the basis of optical and chemical resemblances that are not convincing. | |
|
1928 |
||
| 255. | Van Horn, F. R., Large magnetite and franklinite crystals from Franklin Furnace, N.J.: American Mineralogist, volume 13, pages 171173. Describes some unusually large crystals. | |
| 256. | Palache, Charles, Bauer, L. H., and Berman, Harry, Larsenite and calcium larsenite, a new member of the chrysolite group from Franklin, N.J.: American Mineralogist, volume 13, pages 142144. Preliminary notice. Describes the two minerals briefly for the first time and gives their composition. (See Palache, Bauer, and Berman (259).) | |
| 257. | Palache, Charles, Mineralogical notes on Franklin and Sterling Hill, N.J.: American Mineralogist, volume 18, pages 297329. Crystallographic, physical, and chemical data regarding azurite, bornite, cahnite, clinohedrite, clinozoisite, crocidolite, gageite, glaucochroite, hetaerolite, hodgkinsonite, leucophoenicite, manganite, quartz, smithsonite, sussexite, tephroite, tennantite, and willemite. | |
| 258. | Palache, Charles, The phosphorescence and fluorescence of Franklin minerals: American Mineralogist, volume 13, pages 330333. A description of the apparatus used for observing fluorescence and of the reactions under ultraviolet light of ten of the minerals of the district and the colors they emit when fluorescing. | |
| 259. | Palache, Charles, Bauer, L. H., and Berman, Harry, Larsenite, calcium larsenite, and the associated minerals at Franklin, N.J.: American Mineralogist, volume 13, pages 334340. A fuller statement than that in Palache, Bauer, and Berman (256) of the occurrence, crystal form, physical properties, and composition of the two new minerals described. | |
| 260. | Bauer, L. H., and Berman, Harry, Friedelite, schallerite, and related minerals: American Mineralogist, volume 18, pages 341348. Discusses the general characters of the friedelite group, gives tables of the composition of friedelite and schallerite and of their physical and optical constants and those of related minerals, arid discusses a few of the related minerals. | |
| 261. | Larsen, E. S., Bauer, L. H., and Berman, Harry, Norbergite from Franklin, N.J.: American Mineralogist, volume 18, pages 349353. Much of the material from Franklin labeled chondrodite or humite proves to be norbergite. The paper describes the occurrence, optical character, crystallography, and composition of that mineral. | |
| 262. | Larsen, E. S., The optical properties of the humite group: American Mineralogist, volume 13, pages 354359. Discusses the optical properties of the minerals of the group, from many localities, including material from the Franklin district. | |
| 262a. | Fitch, A. A., The origin of the zinc deposits of Franklin Furnace, N.J.: Mining Magazine, volume 39, pages 8284. Gives a theory of magmatic origin of the deposits by the contact action of the gneiss on the limestone similar to the theory of Ries and Bowen (223). | |
|
1929 |
||
| 263. | Palache, Charles, Paragenetic classification of the minerals of Franklin, N.J.: American Mineralogist, volume 14, pages 118. An elaborate discussion of the occurrence and association of the minerals, classified under five paragenetic groups, according to geologic occurrence. Special attention is given to the minerals of the zinc ores, arranged under four subgroups according to stage of development and time of formation. The several previous theories of the origin of the zinc ores are discussed and rejected, and the author gives a full statement of and supports the theory of metasomatic emplacement of the ores in the Franklin limestone and their subsequent metamorphism. (See Rastall (228). | |
| 264. | Spencer, L. J., Fluorescence of minerals in ultraviolet rays: American Mineralogist, volume 14, pages 3337. Appeared originally in Natural History Magazine, volume 1, pages 291298, 1928. Describes the fluorescence of willemite. | |
| 265. | Palache, Charles, A comparison of the ore deposits of Langban, Sweden, with those of Franklin, N.J.: American Mineralogist, volume 14, pages 4347. A study in which it is pointed out that, despite the occurrence in both districts of numerous minerals known nowhere else, the two deposits have very different geologic histories. | |
| 266. | Bauer, L. H., and Herman, Harry, Loseyite, a new Franklin mineral: American Mineralogist, volume 14, pages 150153. The first description of a new basic hydrous carbonate of manganese, zinc, and magnesium. | |
| 267. | Bauer, L. H., and Berman, Harry, Mooreite, a new mineral, and fluoborite from Sterling Hill, N.J.: American Mineralogist, volume 14, pages 165172. The first description of a new basic hydrous sulphate of magnesium, manganese, and zinc, and the first description of fluoborite from the locality. | |
| 268. | Tarr, W. A., The origin of the zinc deposits at Franklin and Sterling Hill, N.J.: American Mineralogist, volume 14, pages 207221. In this paper the author adopts the theory that the deposits are metamorphosed metasomatic emplacements in limestone and attempts to deduce the nature of the original metasomatic minerals from the present mineralogical constitution of the deposits. | |
| 269. | Hey, M. H., The variation of optical properties with chemical composition in the rhodonite-bustamite series: Mineralogical Magazine, volume 22, pages 193205. A detailed statement of a rather elaborate study of the minerals of the series, including material from Franklin. | |
| 270. | Taylor, W. H., and West, J., The structure of norbergite: Zeitschr. Krist., Band 70, pages 461474, 1029. Confirms the place of norbergite in the humite group and shows that structurally olivine fits into the series. | |
|
1930 |
||
| 271. | Barth, Tom, and Berman, Harry, Neue optische Daten wenig bekannter Minerale: Chemie der Erde, Band 5, pages 2242. Contains an account of the determination of the optical constants of apatite and svabite, as an illustration of the application of their method. | |
| 272. | Palache, Charles, and Bauer, L. H., On the occurrence of beryllium in the zinc deposits of Franklin, N.J.: American Mineralogist, volume 15, pages 3038. A description of beryllium-rich vesuvianite and of barylite at Franklin. Beryllium had not previously been found in vesuvianite. | |
| 273. | Bauer, L. H., and Berman, Harry, Notes on some Franklin minerals: American Mineralogist, volume 15, pages 340348. Analyses and new optical and crystallographic data on zinc-manganese cummingtonite, apophyllite, barysilite, celestite, datolite, ferroschallerite, manganbrucite, and svabite. The mineral previously described as probably clinozoisite is shown to be chlorophoenicite. | |
| 274. | Bragg, W. L., and Zachariasen, W. H., The crystalline structure of phenacite, BeSiO4, and willemite, ZnSiO4: Zeitschr. Krist., Band 72, pages 518528, 3 figures, 1929. Phenacite and willemite have similar unit cells and belong to the same space group. (See Zachariasen (242) .) | |
| 275. | Warren, B. E., and Trautz, O. R., The structure of hardystonite, Ca2ZnSi2O7: Zeitschr. Krist., Band 75, pages 525528. The chemical composition of hardystonite is closely analogous to that of melilite. X-ray examination shows that the unit cell, space group, and atomic arrangement are the same as in melilite, and that the structure differs only in having (Mg,Al) in place of Zn. The space group is D32d, and there are two molecules in the unit cell. | |
| 276. | Palache, Charles, Davidson, S. C., and Goranson, E. A., The hiddenite deposit in Alexander County, N.C.: American Mineralogist, volume 15, pages 280302. Describes, among others, crystals of arsenopyrite and compares them with those found at Franklin. (See page 299 and figure 11.) | |
| 277. | Unpublished analyses of minerals, made in the chemical laboratory of the Department of Mineralogy and Petrography at Harvard University by F. A. Gonyer and others. | |
| 278. | Parsons, A. L., A chemical and optical study of amphibole, in Contributions to Canadian mineralogy, 1930: Toronto Univ. Studies, Geol. series, no. 29, pages 2933. Contains an analysis of an amphibole from Franklin, by M. C. Haller. | |
| 278a. | Krieger, Philip, Notes on an X-ray diffraction study of the series calcite-rhodochrosite: American Mineralogist, volume 15, pages 2329. Manganocalcite from Franklin and other localities was studied, and the variation of X-ray diffraction patterns was correlated with chemical, physical, and optical characters. | |
|
1931 |
||
| 279. | Berman, Harry, and Larsen, E. S., Composition of the alkali amphiboles: American Mineralogist, volume 16, pages 140144. Discusses the composition, relations, and classification of the amphiboles from a new point of view of their molecular structure. | |
| 280. | Manchester, J. G., Minerals of New York City and its environs: New York Mineralogical Club Bulletin, volume 3, no. 1. Gives a brief account of the mines at Franklin and Sterling Hill, and a list of minerals found there comprising 140 species and 78 varieties (but with many synonyms). Also a bibliography including many of the papers treating of the locality. | |
| 281. | Sundius, N., On the triclinic manganiferous pyroxenes: American Mineralogist, volume 16, pages 411429, 488518. Relations of bustamite and rhodonite. | |
| 281a. | Blix, Ragnar, The chemical composition of roeblingite: American Mineralogist, volume 16, pages 455460. | |
| 281b. | Warren, B. E., and Biscoe, J., The crystal structure of the monoclinic pyroxenes: Zeitschr. Krist., Band 80, page 400, 1931. | |
| 281c. | Buerger, M. J., The crystal structure of lollingite, FeAs2 : Zeitschr. Krist., Band 82, pages 165187. | |
|
1933 |
||
| 282. | Bauer, L. H., and Berman, Harry, Barium-muscovite from Franklin, N.J.: American Mineralogist, volume 18, page 30. Description of a muscovite containing barium, with analysis. | |
| 283. | Schaller, W. T., A tephroite crystal from Franklin Furnace, N.J.: American Mineralogist, volume 18, pages 5962. | |
| 284. | Kerr, P. F., Zinc-deposits near Franklin, N.J.: XVI International Geological Congress Guidebook 8, pages 213. | |
|
1934 |
||
| 285. | Haff, J. C., Crystallized native copper from Franklin, N.J.: American Mineralogist, volume 19, page 480. |
|
|
||
|
Website
© by Herb Yeates 1997-2006.
|
||
|
This
page created: August 12, 2006 2:32 PM
|
||