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Proliferative and invasive characteristics of prostate and ovarian cancers
No full text日本大学博士（歯学）doctoral thesi
Middle to Late Pleistocene Geology and Paleogeography on the Basis of Drilling Data in the Musashino Upland, Tokyo, Japan
No full textMiddle to late Pleistocene topography and geology, and paleogeography were investigated in the Musashino upland
areas, Tokyo, based on a great number of drilling core data. 32 key data of drilling cores and outcrops, having age data,
tephras and numerical ages by dating methods, were used for interpretation and geological sections along 1 km x 1 km
grid system covering the Musashino Upland(Fig.2). For these geological sections, more than sixty thousand of drilling
data were used.
Middle to late Pleistocene tephra layers, TB-1(Tm-8)(MIS 7), Ata-Th(MIS 7), TCu-1(Tm-2)(MIS 7), Tky- Ng1(MIS 9),
Yb5(GoP1)(MIS 9), So-OT(MIS 9), and TE-5a(MIS 11) were correlated to known major wide-spread tephra layers using
petrographic properties and/or major element chemical analyses of glass shards and numerical ages by Luminescence
dating.
Supported by these key data, E(MIS 12-MIS 11), D(MIS 10-MIS 9), C(MIS 8-MIS 7), B(MIS 6-MIS 5.5), and A(MIS
2-MIS 1) cycles were recognized in the geological sections.
The results are as follow:
1. During the earlier stage of the D(MIS 10-MIS 9) cycle, distinct types of fluvial activities of Paleo- Tama River existed, one is extension of alluvial fan field in the center, another is deep and small valley by underground water in the areas
of the height of Kazusa Group(Tokyo half dome area).
2. Four small sedimentary basins of the D cycle, were formed during the early stage of MIS 10 to 9. During the middle to late stage, they were filled with transgressive sandy and muddy sediments under the rising of sea-level.
3. There are two buried valleys of the lower B(MIS 6). Major buried valley course crossing the higher part of the
Kazusa Group，and minor valley in the Tama Hills, eroded part.
4. Erosion of the northern half of Tama Hills occurred after MIS 5.3 by lateral erosion of Tama River under gradual
lowering of sea-level.
5. The main reason of strong lateral erosion of the northern half of Tama Hills, may be led by the peak aggradation of
Tama River, which was supported by increased sediment supply in the upper reaches of Tama River during the Musashino and Tachikawa stages(Takahashi and Sugai, 2018).
6. Formation of the deep buried valley of MIS 2 and MIS 1, was started since the MIS 5.1. The processes were traced
by the buried fluvial terraces of MIS 4, MIS 3 and basal gravel stage of MIS 2.departmental bulletin pape
Entschädigung für Wertminderung und Herausgabe von Nutzungen bei Restitution ─ Verhältnis zwischen Wiederherstellung des negativen Vertragsinteresses und Restitution durch Rücktritt ─
No full textdepartmental bulletin pape
Human epidermal growth factor 2 overexpressed alpha-fetoprotein-producing-gastric cancer
No full text日本大学博士（医学）doctoral thesi
Aktualisierungspflicht bei digitalen Produkten: Die neuen Regelungen des BGB
No full textdepartmental bulletin pape
