| Title Transcription | シンジコ コテイ タイセキブツ ノ ネンド コウブツ
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| Title Alternative (English) | Clay minerals in the sediments from Lake Shinji
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| File | |
| language |
jpn
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| Author |
Hirasaka, Ken
Suzuki, Noriyuki
Tokuoka, Takao
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| Description | Clay minerals in the core sediments from Lake Shinji were analyzed．Vertical and lateral distributions of clay minerals in Lake Shinji were clearified，and can be summarized as follows；
1）Smectite，kaolinite，vermiculite，chlorite，illite and halloysite，were major clay minerals． 2）In the eastem area，relative abundance of smectite changes drastically at the depth of 40cm to be more abundant in the deeper zone．The depth，where the relative abundance of smectite starts to increase，tends to be deeper from the east to the west．This drastic change of clay mineral abundance is possibly corresponding to the invasion of Hii river into Lake Shinji in 1635's． 3）Kaolinite decreases with depth and its tendency is reversal to that of smectite． |
| Journal Title |
Geological reports of Shimane University
|
| Volume | 10
|
| Start Page | 81
|
| End Page | 88
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| ISSN | 0287816X
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| Published Date | 1991-07-30
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| NCID | AN00054980
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| DOI（SelfDOI） | |
| Publisher | 島根大学理学部地質学教室
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| Publisher Aalternative | Department of Geology, Faculty of Science, Shimane University
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| NII Type |
Departmental Bulletin Paper
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| Format |
PDF
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| Text Version |
出版社版
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| OAI-PMH Set |
Faculty of Science and Engineering
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| Remark | 1-11 / 1982-1992
島田昱郎教授退官記念論誌集
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| 他の一覧 |
