Earth Science (Chikyu Kagaku)
Online ISSN : 2189-7212
Print ISSN : 0366-6611
Volume 1958, Issue 38
Displaying 1-5 of 5 articles from this issue
  • Masao MINATO, Susumu HONJO
    Article type: Article
    1958 Volume 1958 Issue 38 Pages i-ii
    Published: June 28, 1958
    Released on J-STAGE: July 24, 2017
    JOURNAL OPEN ACCESS
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  • Tadashi YOSHIDA, Keiji SUZUKI
    Article type: Article
    1958 Volume 1958 Issue 38 Pages 1-12
    Published: June 28, 1958
    Released on J-STAGE: July 24, 2017
    JOURNAL OPEN ACCESS
    The intimate stratigraphical relationship, conformable in the central area but uncofnormable in the northeastern and southwestern borders, has been recognized by the writers, between the Yamato and the Yamasato groups. The Ikenahara coarse sandstone member (upper Miocene) is the lowest one of the Yamato group, and the Shiotsubo sandstone member (upper Miocene) is the uppermost one of the Yamasato group. To clarify the mechanism which caused the relationship between the both groups and the sedimentary conditions of both sandstone members, the writers carried out the grain size and mineral analyses. The results are as follows; 1) The Ikenohara sandstone member contains bipyramidal quartz in remarkably large quantities, and various igneous mafic minerals-hypersthene, augite and hornblende-in small quantities, and is characterized by coarse Ac and Bb grain sizes. The Shiotsubo sandstone member contains large quantities of biotite and glassy volcanic fragments, and is characterized by medium to fine Cd-e grain sizes. 2) The grain size pattern of the Ikenohara sandstone member affords several varieties. It is characterized by an uniform constitution in the northern area, by deltaic environmental patterns in the northeastern area, and by lagoonal environmental patterns in the southern and central areas. On the other hand, variation of grain size pattern is scarcely recognized in the Shiotsubo sandstone member. The Ikenohara coarse sandstone member has several different environmental patterns; i.e. deltaic in the northeastern area, inletic in the northern area, tidal inletic in the central area and lagoonal in the southern area. The Shiotsubo sandstone member has an uniform environmental pattern which shows a neritic, shallow marine condition. 3) The remarkable differences in grain size pattern and mineral composition between both sandstone members suggest a sudden change of palaeogeographical conditions of the sedimentary basin and the hinterland during the sedimentation. This change may be closely related to the acidic volcanisms (Iitani liparitic volcanics etc.), and to the tilting movements which trended from NE to SW in the northwestern area and from SW to NE in the southeastern area of the Aizu Basin, This change might have caused the differentiation of the sedimentary basin.
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  • Saburo AKAGI
    Article type: Article
    1958 Volume 1958 Issue 38 Pages 13-27
    Published: June 28, 1958
    Released on J-STAGE: July 24, 2017
    JOURNAL OPEN ACCESS

    In this paper, the writer discussed the significance of the growth and form of fusulinids, especially of the relations between such shell forms as cylindrical or fusiform and the spiral growth of the shell. Most of the materials, used in this study, are chosen from the specimens of Pseudoschwagerina miharanoensis AKAGI (MS), collected from the limestone of Miharano, Tojo-machi, Hiba-gun, Hiroshima Prefecture. It is the most abundant fusulinids in the Miharano Limestone (Sakmarian). The fossils occur as free specimens detouched from matrix, so that the external characteristics are well observed. First, the meanings of the shell form were discussed. Geometrically, the mode of growth is regular and rather simple, in spite of the apparent complexity of the internal structures exhibited in thin sections. An increase of protplasm results the growth of body and the coiling chambers. Additions of chambers along the preceding ones make up the volutions, which are performed regularly, because their floors and backside walls are substituted by the corresponding roofs and frontal walls of the preceding ones. Organization has not been studied in fusulinids. They have been included in the "Anaxonia" together with such higher invertebrates as gastropods and others, as was the case of the other members of Amoebae. But, it should be better to remove them from the Anaxonia, because they have a distinct axis in their bodies, around which the shell is formed in a certain regular and definite way of coiling, whereas the members of true Anaxonia do not show any regularity in their organization. So, the writer proposes a new group "Spiralia" for those animals characterised by the spiral organization of body. Second, the spiral curves of coiling were studied in some detail, and were compared with curves drawn geometrically. In this case, the writer found that the spiral curves of fusulinids were nearly identical with logarithmic spiral, which was characterized by a constant angle of tangent against the corresponding radius at their contact. Such spirals as those are called equiangular spirals. The angles of contact in Pseudoschwagerina miharanoensis are about 86 degrees throughout the most stages of growth, except the earliest and the gerontic stages. A deployed figure is drawn in such a way as follows : First, an ideal cross section is deduced from an axial section. In this operation, the law of constant angle of contact is used. The ideal cross section is better than a real cross section for the prepareation of a deployed figure, because it represents a cross section of the same individual from which the axial section is obtained. Further, an ideal cross section confirms the specific identity of a real cross section and the axial section, from which the ideal cross section is deduced. The spiral curve of the ideal cross section, is, then, unrolled and straightened in a straight line. Then, the chambers of the axial section are figured serially and successively on the straight line, where the positions of each chamber are located so as to equal to the lengths of corresponding half a volutions. Next, both ends of each sections were connected successively by lines on both sides of the figure. The figure, thus obtained, represents an unrolled sheet of a fusulinid indvidual, and it, really, shows the mode of growth very clearly. The deployed figure of Pseudoschwagerina miharanoensis, deduced from the holotype specimen, shows that the rate of growth changes rapidly in several stages. Also, it shows the relation between growth and form, the increase of tunnel angles and the relative growth of several parts of shell. The growth of the shell in spiral direction is larger in the center, and becomes smaller toward the polar regions. From such deployed figures of fusulinids, followings are noticed. 1. In fusnlinids, four factors of growth are important in the study of shell form. These

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  • Satoru UOZUMI
    Article type: Article
    1958 Volume 1958 Issue 38 Pages 36-38
    Published: June 28, 1958
    Released on J-STAGE: July 24, 2017
    JOURNAL OPEN ACCESS
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  • Hiroyuki TAKEDA
    Article type: Article
    1958 Volume 1958 Issue 38 Pages 38-
    Published: June 28, 1958
    Released on J-STAGE: July 24, 2017
    JOURNAL OPEN ACCESS
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