Abu Ya’Qub Al-Sijistani and Kitab Sullam Al-Najat, A Study by Mohamed Abualy Alibhai
By Mohamed Abualy Alibhai
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2-4). Frameworks of such rocks show complete transition from those which are grain- 45 Fig. 2-4. Incompatible cement (dolomite, d ) , later than quartz overgrowths, abuts with sharp boundary against rounded, detrital grains of quartz. Dolomite partly fills pores, does not weld to quartz grains, and assumes outline of detrital grain. Attachment t o quartz grain is by surface cohesion. An early stage of a bilateral junction and welding of two quartz grains t o form a self-boundary is shown by arrow at position j .
47 Fig. 2-6. Displacive precipitation of calcite in red-bed sandstone initially cemented by hematite as a primary incompatible cement. The hematite is now dispersed throughout the calcite as inclusions (dark gray and black), primarily in right half of photo. A.
1 3 (1/2). , 1966. Towards question of determining stages and total volume of catagenetic changes in sedimentary rocks. Sou. , 3. , 1953. Use of Ca/Mg ratio in limestones as a geologic tool. Compass, 30: 29-34. , 1955. Review of Soviet literature on petroleum source rocks. Bull. A m . Assoc. Pet. , 3 9 ( 5 ) : 764-768. , 1956. Relationship between Ca/Mg ratio and geologic age. Bull. A m . Assoc. Pet. , 40: 2256-2266. , 1958. Some data o n diagenesis obtained from Soviet literature: a summary.