. Carnegie Institution of Washington publication. FIG. 7 (Blackwelder).—Ch'au-mi-tien, Shan-tung. Section of Upper Cambrian and Lower Ordovician strata in the ridge east of the village, i = dense blue-gray limestone; 2 = conglomeritic limestone; 3 = sandy yellow dolomite; 4 = white earthy limestone; s=buff crystalline dolomite; 6 = shaly gray lime- stone; 7= blue-gray limestone; 8 =slabby yellow limestone; 9= dense brown FIG. 8 (Blackwelder).—Yen-chuang, Shan-tung. Section of Kiu-lung formation in Kiu-lung-shan. i = Man-t'o shales; 2= dark limestone, partly oolitic; 3= dense gray l
. Carnegie Institution of Washington publication. FIG. 7 (Blackwelder).—Ch'au-mi-tien, Shan-tung. Section of Upper Cambrian and Lower Ordovician strata in the ridge east of the village, i = dense blue-gray limestone; 2 = conglomeritic limestone; 3 = sandy yellow dolomite; 4 = white earthy limestone; s=buff crystalline dolomite; 6 = shaly gray lime- stone; 7= blue-gray limestone; 8 =slabby yellow limestone; 9= dense brown FIG. 8 (Blackwelder).—Yen-chuang, Shan-tung. Section of Kiu-lung formation in Kiu-lung-shan. i = Man-t'o shales; 2= dark limestone, partly oolitic; 3= dense gray limestone; 4 = nodular green shale; 5=dense gray limestone; 6=gray shale and slabby limestone; 7 = thin-bedded dense gray limestone; 8=green calcareous shale; 9=conglomeritic limestone; io = nodular green shale; n=slabby blue limestone; 12 =shaly limestone and gray shale; 13 =black limestone; 14 = slaty gray limestone; 15 = conglomeritic limestone; i6=massive gray limestone; 17 = thin-bedded gray limestone; i8=red con- glomeritic limestone; 19 = dark gray limestone, locally conglomeritic; 20 = massive gray limestone. Sections measured as follows: A B. D. Jv, F. and G, in vicinity of Ch'au-mi-tien. Shan-tung. C. H I and }, in vicinity of Ch'ang-hia. Shan-tung. K. L. M. and N. in vicinity of Sin-t'ai, Shan-tung. O. at Hin L-hou. Shan-si. vertical scale 200 300 «oo ioe Feet. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Carnegie Institution of Washington. Washington, Carnegie Institution of Washington
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