Geomathematical and Petrophysical Studies in Sedimentology. by Dan Gill

By Dan Gill

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The hydrau­ lic conductivity values in central and southern Scott County are un­ derestimated by 100 to 200 percent. This area lies on the northsouth bedrock channel in central Scott County. The deposits consist of medium to very coarse sand and gravel interbedded with layers of silt and clay (Gutentag and Stullken, 1974) and are thicker in the southern than in the northern part of the bedrock channel. Large ΔΚ values show that the hydraulic conductivity is high in this area. ft. WICHITA Figure 6.

Nat. , v. 1, p. 9-18 (in Japanese with English abstract). , Jour. , Ser. Nat. , v. 2, p. 7-16. (in Japanese with English abstract). , 1965, Izumi Group in the central tain Range, southwest Japan, with special mentary facies and cyclic sedimentation: no. 212, 33 p. (in Japanese with English part of the Izumi Moun­ reference to the sedi­ Geol. Surv. Japan, Rept. abstract). , 1968, On the checking of the theoretical backgrounds of the stochastical models in concrete geological investigations: Proc.

These characteristics indicate that a Poisson process, with some modifications, serve as an adequate model for the sedimentation of the Izumi Group. EXPLANATION OF MODELS It is accepted generally that the Izumi Group was deposited by turbidity currents (Tanaka, 1965; Suyari, 1966; Suyari and others, 20 NISHIWAKI Table 1. Number of measure­ ments of Izumi Group along west coast of Awaji Island. Data used in Fiaure 2. Litholoqy Number of beds shale sandstone conglomerate graded unit reversed unit 8358 8683 127 8305 8205 1968; Nishiwaki, 1975).

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