The purposes of this study are to find out relationship between geology and reservoir conditions, and crude oil properties, if any, and to reveal the direction of secondary migration of the crude oil by grasping the crude oil characteristics. Thus, our study is concerned with reservoir geology as well as petroleum geochemistry.
Minami-Aga oil field is situated in the Niigata plain, to the 250km north of Tokyo (Figure 1). The field was discovered in 1964 and is one of the largest oil fields in Japan at present. The geology and case history of the field in detail were described and presented by the Japanese Delegation to the 4th ECAFE Petroleum Symposium, held at Canberra, Austraria, in 1969. The only oil reservoir is in the upper part of the Shiiya Formation. The Shiiya Formation is composed of dark grey mudstone intercalating tuffaceous sandstone and regarded as uppermost Miocene marine sediments. The reservoir rock is poorly sorted fine to coarse tuffaceous or muddy sandstone, partly conglomeratic. The average porosity is reported to be 23%; average permeability 52-58md; average water saturation 41%.
The geologic structure consists of two anticlines, plunging to the north and bordered by the f-f' fault of north-south direction (Figure 2). The sandstone reservoir pinches out up the dip, thereby forming a combination anticlinal-pinchout trap (Figure 3). A large gas cap is found in the upper part of the reservoir, but the cap gas is not exploited. The isopachous contours of the true thickness of the reservoir are shown in Figure 4. Figure 5 shows the distribution of water saturation of the reservoir. The change in porosity is demonstrated in Figure 6. Figure 7 shows the temperature of the reservoir. From these maps we can recognize that the field is divided into three parts, i.e. A, B and C blocks. The A block is a district on the west of the f-f' fault. The C block denotes the southern wing of the east anticline, where the dip of the reservoir is very steep. The B block is a district between the A and C blocks. In the B block the dip is most gentle, and the irregularities of the various aforementioned parameters are recognized. These facts seem to have some correlation with the various crude oil properties which we will refer to afterwards.
We collected 24 degassed oil samples separately from all the producing wells. At first specific gravity of the crude oil was measured and the result is shown in Figures 8 and 9. The variation in the specific gravity of the crude from the B block is wide, whereas that of the crude from the A and C blocks has small variation and almost coincides with each other. The specific gravity of the B block crude is higher than that of other blocks, which is probably due to the remarkable change in lithology in the B block. Figure 10 is a specific gravity-absolute viscosity plot, in which a positive correlation and a wider variation of the B block are found. From the result of distillation of the crude by the Hempel method and the measurement of specific gravity of the particular cuts, we can conclude that the Minami-Aga crude is of intermediate-paraffinic base. There is the tendency that the crudes which have smaller amounts of the cut up to 300°C are from the wells situated in the anticlinal wings of high water-saturation.
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