Age and stratigraphy of volcaniclastic rocks in northern part of southwest Hokkaido based on K-Ar ages and diatom assemblages
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- Watanabe Yasushi
- Geological Survey of Japan, Hokkaido Branch
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- Watanabe Mahito
- Geological Survey of Japan, Fuel Resources Department
Bibliographic Information
- Other Title
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- K-Ar年代および珪藻化石群集に基づく西南北海道北部の火山砕屑岩類の層序と年代
- K Ar ネンダイ オヨビ ケイソウ カセキ グンシュウ ニ モトズク セイナ
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Abstract
The K-Ar dating of volcanic rocks and study on diatom fossils from northern part of southwest Hokkaido lead to the following conclusions: The Otaru Formation, Fuso Agglomerate, Eboshidake Agglomerate, Kamui Agglomerate and Hoheikyo Agglomerate composed mainly of submarine volcaniclastic andesite and basalt, formed in Late Miocene age. These volcaniclastic rocks were erupted and deposited during the period from 10 Ma to 7.5 Ma. The volcaniclastic rocks unconformably overlay felsic volcanic rocks of Middle Miocene age. The unconformity formed probably between 11 Ma and 10 Ma. K-Ar ages of the andesite lavas, resting on these submarine volcaniclastic rocks are 7.5 Ma to 5 Ma. Therefore, the "flat lavas" were erupted during not only Pliocene or Pleistocene, but also Late Miocene age. The Late Miocene to Pliocene volcanic rocks are distributed in NW-SE trending.
Journal
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- Earth Science (Chikyu Kagaku)
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Earth Science (Chikyu Kagaku) 46 (2), 143-152, 1992
The Association for the Geological Collaboration in Japan
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Details 詳細情報について
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- CRID
- 1390001204233621248
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- NII Article ID
- 110007092723
- 10006461032
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- NII Book ID
- AN00141269
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- ISSN
- 21897212
- 03666611
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- NDL BIB ID
- 3754054
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- Text Lang
- ja
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- Data Source
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- JaLC
- NDL
- CiNii Articles
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- Abstract License Flag
- Disallowed