115 



[1915-19-] 



GOSSELET, J. Obit. — See Dollfus, G. F., 12; Hakkek, A., 4; Lackoix, 



A., 36; Leriche, M., 8; & Revil, J., 4. 

 GOSSNER, B. Neuere Ergebnisse der Anwendung physikalisch-chemiseher 



Methoden auf Probleme der Geologie. Geol. Rundsch., Leipzig, vi. pp. 



218-241. 1915. 

 GOTTSCHALK, V. H. See Cox, G. H., 2. 



GOULANDRIS, E. Sur les Tremblements de Terre de Cephalonie-Zante du 



24 Janvier 1912. Ann. Observ. nat. Athenes, vii. pp. 42-46, fig. [map]. 



1916. [See also Eginitis, D., 4.] 

 2. Sur le Tremblement de Terre de Thebes du 17 Octobre 1914. Ibid. 



pp. 47-50, fig. [map]. 1916. [See also Eginitis, D., 5.] 

 GOULD, C. Report on the Mersey Coal Fields. Tasmania, Geol. Surv. No. 



50. Pp. 1-10, 3 pis. [geol. maps & sections]. 1861. 

 GRABAU, A. W. Principles of Stratigraphy. Pp. i-xxxii, 1-1185, figs. 



[geol. maps & sections]. 8vo. New York, 1913. 

 2. North American Continent in Upper Devonic Time. [Abstract.] 



Bull. Gebl. Soc. Am. xxvi. pp. 88-89. 1915. 

 3. Comparison of American and European Lower Ordovic Formations. 



Ibid, xxvii. pp. 555-622, figs, [map & geol. sections]. 1916. 

 4. Comparison of the European and American Siluric. [Abstract.] 



Ibid, xxviii. p. 129. 1917. 

 5. Problems of the Interpretation of Sedimentary Rocks. Ibid, xxviii. 



pp. 735-744. 1917. 

 6. Stratigraphic Relationships of the Tully Limestone and the Genesee 



Shale in Eastern North America. Ibid, xxviii. pp. 945-958, figs. [geol. 



map & sections]. 1917. 

 7. Age and Stratigraphic Relations of the Olentangy Shale of Central 



Ohio, with Remarks on the Prout Limestone and so-called Olentangy 



Shales of Northern Ohio. Journ. Geol., Chicago, xxv. pp. 337-343, fig. 



[geol. section]. 1917. 

 8. Relation of the Oil-bearing to the Oil-producing Formations in the 



Palaeozoic of North America. [Abstract.] Bull. Geol. Soc. Am. xxix. 



pp. 92-93. 1918. 



9. Significance of the Sherburne Bar in the Upper Devonic Stratigraphy. 



[Abstract.] Ibid. pp. 127-128. 

 10, & Marjorie O'Connell. Were the Graptolite Shales, as a rule, 



Deep or Shallow Water Deposits ? Bull. Geol. Soc. Am. xxviii. pp. 959-964, 



fig. [diagram]. 1917. 

 GRABHAM, G. W. See Bailey, E. B., 4. 



, & S. C. Dunn. Hints on Collecting Geological Information and Speci- 

 mens. Pp. 1-24. 8vo. Khartoum, 1913. 



GRABLOVITZ, G. Sul terremoto del 13 gennaio 1915. Atti R. Acc. Lincei, 

 ser. 5, Rendic. xxiv. sem. 1, pp. 597—604, pi. [map]. 1915. 



GRAHAM, J. I. The Absorption of Oxygen by Coal. Part VII.— The 

 Influence of Moisture upon the Rate of Absorption, and the Question of 

 Bacterial Oxidation. Trans. Inst. M. E. xlix. pp. 35-43. 1915; & Coll. 

 Guard, cxii. pp. 498-499. 1916. 



2. . PartX. — The Formation of Water in the Oxidation of Coal. Trans. 



Inst. M. E. lii. pp. 348-353, fig. 1917. [See also Winmiix, T. F., 2 db 3.] 



3. The Permeability of Coal to Air or Gas, and the Solubilities of Different 



Gases in Coal. Ibid. lii. pp. 338-347. 1917. 



4. . Part II. Ibid, lviii. pp. 32-38. 1919; & Coll. Guard, cxviii. 



p. 1043. 1919. 



5, & J. Hile. The Oxidizable Constituents of Coal. — Part I. Trans. 



Inst. M. E. liv. pp. 197-214, figs, [diagrams]. 1917; Coll. Guard, cxiv. 



pp. 491-492, figs, [diagrams]. 1917; & Trans. N. Engl. I?ist. Min. & 



Mech. Eng. lxviii. pp. 37-54, figs, [diagrams]. 1918. 

 GRAHAM, R. P. D. Origin of Massive Serpentine and Chrysotile-Asbestos, 



Black Lake-Thetford Area, Quebec. Econ. Geol. xii. pp. 154-202. 1917. 



[See. also Taber, S., 3. | 

 2. The Determination of the Specific Gravity of Mineral Fragments by 



Heavy Liquids. Proc. & Trans. Roy. Soc. Canada, ser. 3, xi. sect. iii. 



pp. 51-53. 1917. 



3. Lattice-like Inclusions in Calcite from North Burgess, Ontario. Min. 



Mag. xviii. pp. 252-258, pis. viii-x. 1918. 

 4. On Ferrierite, a new Zeolitic Mineral, from British Columbia ; with 



Notes on some other Canadian Minerals. Proc. & Trans. Roy. Soc. 



Canada, ser. 3, xii. sect. iv. pp. 185-201, figs. & 1 pi. 1919. 



