FIG. 2.--Pyrite (P) replaced by sphalerite (S), in turn veined by X 54. 267. X 54. Oil immersion. X 540. Dipterocarpoxylon garense, sp. nov., G. S. I. Type No. 16502. PLATE 15.--Fig. 1.—Transverse section showing distribution of vessel, rays and vertical gum ducts. Note the arrangement of gum ducts at the right hand corner (Gd). X 10. FIG. 2.--Transverse section showing distribution of small (Sv) and large vessels in comparison with that of gum ducts (Gd). X 40. Fig. 3.-Transverse section showing parenchyma and tracheids round the vessels. Note also the distribution of metatracheal parenchyma cells. x 75. FIG. 4.--Transverse section showing a pair of gum ducts surrounded by rows of parenchyma cells. x 35. Fig. 5.--Tangential section showing distribution, width and height Note also the size and shape of the cells forming different types of rays. x 50. Fig. 6.—Tangential section showing tyloses in the vessels. X 110. of rays. Dipterocaropxylon gurænse, sp. nov., G. S. I. Type No. 16502. PLATE 16.-Fig. 1.-A vessel element showing inter-vessel pits. X 90. Fig. 2.--Radial section showing inter-vessel pits (Ivp) and fungal hyphæ (H). X 440. Fig. 3.-Radial section showing vessel-ray pits (Vrp). Note their distribution and size. X 440. Dryoxylon sp., G. S. I. No. K40/485. X 10. Note the shape of individual oells of rays. x 75. x 35. Inter-trappean Fish Remains. PLATE 11.–Fig. 1.-A Pristolepid scale (K29/629). x 20. FIG. 2.-A Nandid scale (K29/628). x 20. Fig. 3.-A fragment of a Clupeoid scale (K32/159). X 15. Fig. 4.-A Labyrinthid scale (K32/147) allied to Polyacanthus C. V. x 7. X 3. X 54. Inter-trappean Fish Remains. X 4. x 4. FIG. 5.-- An Acanthopterygian scale (K40/286), Type A. x 20. B. X 4. singha. X 15. Dhamni. x 7. X 3. Dongargaon. x 7. P. S. 217. X 54. Unreplaced ganela (white). P. S. 217. of the various minerals. Fig. 2. -The centre shows one of the felspathic patches in Fig. 1 under crossed nicols. The granulation and disconti. nuity of the twinning planes is due to crushing and move ment. Fig. 3.-Charnockite similar to that shown in Fig. 1, but more intensely crushed. Most of the hypersthene is altered to a feathery aggregate of scaly hornblende. Fig. 4.—Completely crushed charnockite, consisting of narrow bands of hornblende (dark), felspar, etc. (light) and garnet (G). A few crystals of hypersthene (H) always seem to have survived the crushing. PLATE 21.–Fig. 1.- Typical hypersthene-gneiss. FIG. 2.-Typical soda-granite. (M) cor ling the orthoclase (Or). PLATE 22.-Fig. 1.—Myrmekite corroding microcline. Fig. 2.---Dactylites of biotite and a myrmekitic intergrowth of biotite and albite. some cases altered to garnet. Seismograms of the Baluchistan (Quetta) Earthquake of May 31, 1935. E.-W. Component. MGIPC-M-VIII-1-17-15-8 39.800. 443. . . 370-372. Aceratherium tetradactylum insigne palæindicum correlation with Umia stage 1937 granted in, during 1937 Peshawar district, N.-W. F. P. Recent. series sandstone in laterite in 388. 460. . . 24. . . . |