The deep boring at Spur . Plate 8. A. Vertical section of oolitic dolomite from between 2609and 2624 feet below the Anhydrite has replaced the materialinside many of the spherules and the matrix is dolomitic. X 40. B. Vertical section through another phase of the oolitic dolomiteshown in A, plate 8. Anhydrite has in this instance replaced mostof the material in the matrix and the spherules remain as 40, Missing Page ^^^KifiMFfflP? 1^^^%^^ l||nH|^, M •sgjs^ pH^^^H BpM ^HKpf^^p P^ ^^^^^^B^^WBB HteB ^^HH^Bw9^^H^Ci->«. -j^g^*^ j^SK hH [^^^^P 1 ?m ^^^R^H HH^^^^^HH^ka ^ji Pla
The deep boring at Spur . Plate 8. A. Vertical section of oolitic dolomite from between 2609and 2624 feet below the Anhydrite has replaced the materialinside many of the spherules and the matrix is dolomitic. X 40. B. Vertical section through another phase of the oolitic dolomiteshown in A, plate 8. Anhydrite has in this instance replaced mostof the material in the matrix and the spherules remain as 40, Missing Page ^^^KifiMFfflP? 1^^^%^^ l||nH|^, M •sgjs^ pH^^^H BpM ^HKpf^^p P^ ^^^^^^B^^WBB HteB ^^HH^Bw9^^H^Ci->«. -j^g^*^ j^SK hH [^^^^P 1 ?m ^^^R^H HH^^^^^HH^ka ^ji Plate 10. A. Horizontal section of dolomite from near the depthof 3245 feet. The rock has an obscure oolitic structure. X n+oi BoMinn r\f oi-wo+nllino rtrAomite from near the depth
Size: 1586px × 1575px
Photo credit: © The Reading Room / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookauth, bookcentury1900, bookdecade1910, bookidcu31924004622084
