Judging from the complicated structures of the pre-Miocene rocks, they are treated as the basement rocks. The Yorii conglomerate, which has been generally considered to be an Aquitanian formation, must be correlated with the Cretaceous Atokura formation, and then, it is a member of the basement rocks. The Miocene formations of this area are time-stratigraphically divided into four stages, that is, M1, M2, M3 and M, from lower to upper. The M1a stage is subdivided into two substages, M1a (lower) and M1b (upper). The rocks of M1a substage are characterized by molluscan and foraminiferal faunas, which contain proper Miocene and survived Oligocene elements, and Aniai flora. On the other hand, the rocks of M1b substage are characterized by the first occurrence of the Lepidocyclina-Miogypsina fauna and Daijima flora, and the Oligocene elemens of Mollusca and Foraminifera are rare in these rocks. The rocks of M2 stage are characterized by the Kadonosawa and Shirikonai molluscan faunas -of proper Micene type, and some of these contain Lepidocyclina, Miogypsina, Desnzostylus and Cornwallius. The rocks of M3 stage are also characterized by the Kadonosawa molluscan fauna, but Lepidocyclina has not been found in these rocks. The lowermost horizon of this stage is marked by the Miogypsina-Operculina fauna and pyroclastic rocks. The rocks of M4 stage are characterized by the Higashi-Tanagura and Zushi molluscan faunas. These faunas contain both Miocene and Pliocene elements. Globigerina nepenthes has been found in some rocks of this stage. Judging from Kasukabe GS-1, a stratigraphic well, the Kazusa group in the middle part of the Kwanto plain area contains two sedimentary cycles corresponding to lower and middle parts of this group in the type area. In the northern part of the Kwanto plain area, the Kazusa group contains only one cycle, that is, the upper cycle in Kasukabe GS-1. In this well, the Pleistocene formation between Kazusa group and Alluvium is very thick, but this formation is considered to represent only one inter-glacial age, that is, Mindel-Riss. In the Kwanto area, six diastrophic phases since middle Tertiary have been recognized by the writers. Of these phases, the Kadono, Fuji-Yoshida, Higashi-Matsuyama and Kurotaki phases correspond respectively to Savian, old Styrian, new Styrian and Rhodanic phases in Europe. The ages of remaining two phases, that is, Minami-Tama and Kasukabe, are middle Pliocene and Mindel-Riss inter-glacial age respectively. The distribution of sea and land in this area had been largely changed by the crustal deformation of the Higashi-Matsuyama phase. In the Kwanto area, all developed gas reservoirs except those of Mobara type belong to normal dissolved-in-water type. Permeability of reservoirs is generally lower than that in the Niigata gas-field, and then, the wells of large diameter are not always favourable for the southern Kwanto gas-producing region. In the Mobara type gas deposits, gas-water ratio rapidly increases with the progress of devel-opment. Development methods suitable to natural condition are especially important in case of Mobara type gas deposits. It is also very important to clarify the extension of reservoirs of this type. On the other hand, detailed gravimetric survey and facies studies are effective for exploration of the normal dissolved-in-water type gas deposits. As to Miocene formations, we cannot expect too much of free gas pools in the region except the area of thick lower and middle Miocene deposits.
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