By Selley Richard C.
This variation keeps the case background method of emphasize the subsurface analysis of environments utilizing seismic and geophysical good logs and their program to petroleum exploration and construction. This booklet can be of curiosity to undergraduates in sedimentology and petroleum geology.
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Additional resources for Ancient Sedimentary Environments: And Their Sub-surface Diagnosis
P. curve (Fig. 6). Calibration may then be made since the sand line will correspond to the coarsest sand samples seen in the well samples. P. log as a grain-size profile is a well-established technique it has several limitations naturally. The relationship between the permeability and grain size is valid only for sediments with primary intergranular porosity. P. log may not reflect grain size in cemented sandstones or in carbonates with complex diagenetic histories. P. curve only shows good amplitude when there is a substantial difference between the salinity of the drilling mud and that of the formation waters.
Palaeoecology, Concepts and Applications. J. Wiley, London, p. 544. Doeglas, D. , 1946. Interpretation of the results of mechanical analysis. J. Sediment. Elsevier, Amsterdam, p. 280. Duff, P. McL. , and Walton, E. , 1967. Cyclic Sedimentation. Elsevier, Amsterdam, p. 280. Dunham, R. , 1962. Classification of carbonate rocks according to their depositional texture. In: Classification of carbonate rocks. (Ed. W. E. Ham) Amer. Assoc. Petrol. Geol. 1, pp. 108-21. Feldhausen, P. , and Ali, S. , 1975.
Petrol. , 52, 1689-99. Merriam, D. F. ) 1967. Computer Applications in the Earth Sciences. Colloquium on time-series analysis. Computer contribution No. 18. State Geological Survey. University of Kansas. Middleton, G. , 1973. Johannes Walther's law of correlation of facies. Bull. Geol. Soc. , 84, pp. 979-88. Mills, P. , 1983. Genesis and diagnostic value of soft sediment deformation structures-a review. Sed. , 35, 83-104. Moiola, R. J. , 1968. Textural parameters: an evaluation. J. , 38, 45-53.