Export Mendeley
＜departmental bulletin paper＞
The Izumi Group in the Kawauchi-Shigenobu Area to the East of Matsuyama
| Creator | |
|---|---|
| Language | |
| Publisher | |
| Date | |
| Source Title | |
| Vol | |
| Issue | |
| First Page | |
| Last Page | |
| Publication Type | |
| Access Rights | |
| JaLC DOI | |
| Abstract | The lithological aspects of the Izumi group, the notes of general geology and the structural geology are described. The elongated area of Northern Shikoku is covered by the marine elastic sediments, t...he upper Cretaceous Izumi Group, which is distributed along the Median Tectonic Line of the Southwest Japan. They consist of a large volume of elastics. The stratigraphic succession of the Izumi Group in the investigated area is summarized as follows in ascending order. Lower subgroup Formation A : conglomerates and sandstones Formation B: sandstones with thin shales Formation C : alternation of shales and sandstones Middle subgroup Formation D: alternation of sandstones and shales lower part predominated sandstones Formation E : shales alternated with sandstones Upper subgroup Formation F: chiefly-coarse grained sandstones, partly with sporadic gravels Formation G: alternation of sandstones and shales Formation H: conglomeratic sandstones One subgroup shows one sedimentary cycle, the lower part of which is dominated by coarse-grained elastic rocks. Various types of graded bedding are shown in Figs. 3 to 6 and Tables 1 to 7. The direction of the sedimentary transport is determined as being from northeast to southwest by the analysis of primary sedimentary structures. As a result of the comparison of the sedimentary environments, the main part of them are considered to be a kind of submarine fan.show more |
Hide fulltext details.
| File | FileType | Size | Views | Description |
|---|---|---|---|---|
0802_p137
|
1.17 MB | 1,103 |
Details
| PISSN | |
|---|---|
| NCID | |
| Record ID | |
| Created Date | 2021.11.26 |
| Modified Date | 2022.06.20 |