巻号一覧
24 巻 (1985 - 1986)
- 4 号 p. 263-
- 3 号 p. 153-
- 2 号 p. 77-
- 1 号 p. 1-
24 巻, 4 号
選択された号の論文の7件中1～7を表示しています
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福間 敏夫, 藤田 和夫1986 年 24 巻 4 号 p. 263-281
発行日: 1986/01/31
公開日: 2009/08/21
ジャーナル フリーThe Fukuchiyama Basin is one of the small intermontane basins distributed in the Meso-Paleozoic terrain of the northwestern part of the Kinki District. The basin is filled with the Quaternary deposits having wide sedimentary surfaces which are regarded as the extensions of the“Higher Terrace”widely spreading in the central part of the Kinki. The followings have been clarified by the present studies.
1) The Quaternary deposits in this basin reaches more than 50m in thickness consisting of five sedimentary units succeeded conformably, which are collectively called the Fukuchiyama Formation. Each unit was formed as a small fan developed along the marginal part of the basin or as fluvial deposit along the main river course flowing into the basin.
2) Fig. 13 is the summary of the results of the studies of the Fukuchiyama Formation from viewpoints of paint fossil and paleomagnetism. No evidence of the Metasequoia flora was found, which shows that this formation is correlative to the Upper Part of the Osaka Group. The Sabia bed, intercalated in the upper horizon of the formation, contains the plant remains of warmer or subtropical types and is thought to correspond to the Ma 8 horizon of the Osaka Group.
3) The paleomagnetic polarity of the Fukuchiyama Formation is normal except one narrow horizon showing reverse event. This is the character of the Brunhes Normal Epoch.
4) The Fukuchiyama Formation closely resembles to the Meimi Formation in the Harima Basin in various points, which has a FT age of 0.49±0.09 Ma in the lowest horizon.
5) The age of the Fukuchiyama Formation is inferred to be the Middle Pleistocene, about 0.6 or 0.7 Ma to 0.2 or 0.15 Ma, considering that the Brunhes Normal is generally dated 0.7 Ma to present with brief revesals at 0.11 and 0.02 Ma and Ma 8 horizon of the Osaka Group is intercalated with a volcanic ash layer having a FT ale of 0.38±0.04Ma.抄録全体を表示PDF形式でダウンロード (2948K) -
岩内 明子, 長谷 義隆1986 年 24 巻 4 号 p. 283-293
発行日: 1986/01/31
公開日: 2009/08/21
ジャーナル フリーThe Asono Formation is a lacustrine deposit consisting of diatomaceous siltstone, tuffaceous sandstone, tuff and conglomerate. The formation abuts unconformably against volcanic basement rocks, including the Kumamureyama rhyolite that has a FT age of 0.73±0.14Ma. The upper part of the Asono Formation contains a lava flow which has a pseudo-pillow structure. This flow is called the Uchiyama hornblende andesite and its FT age is 0.34±0.17Ma. Thus the Asono Formation is inferred to deposit during the Middle Pleistocene.
The fossil diatoms from the Asono Formation are all freshwater species. Six zones have been identified, based on the predominant species.
Zone A: Cylotella zone
Zone B: Stephanodiscus zone
Zone C: Cyclotella zone
Zone D: Opephora zone
Zone E: Melosira zone
Zone F: Stephanodiscus zone
The fossil diatom assemblages show the water in Lake Asono was alkaline throughout deposition of the formation. The alkalinity was higher and the eutrophy more advanced during depostion of the Zone E and F sediments than the other sediments. Pollen analysis indicates probably cooler water temperature at the time of Zones B and F than the other zones.抄録全体を表示PDF形式でダウンロード (2836K) -
成瀬 敏郎, 酒井 均, 井上 克弘1986 年 24 巻 4 号 p. 295-300
発行日: 1986/01/31
公開日: 2009/08/21
ジャーナル フリー我が国に分布する土壌のうち, 火山灰土 (クロボク土), 古砂丘下に埋没する古土壌, 玄武岩台地や海成段丘上にのる土壌, 南西諸島の赤黄色土など, 北海道から与那国島にかけての地域で20試料を採取した.
試料土壌中に含まれる微細石英 (1～10μm) は, 10～30%と多く, この微細石英の起源を明らかにするために石英の酸素同位体比 (18O/16O) を求めた.
その結果, 完新世に生成された火山灰土や黄色土中に含まれる微細石英の18Oは15.4～15.9‰であり, これまで行われた研究の結果とほぼ一致した. 最終氷期に生成された土壌についても, ほぼ同様の値が得られ(δ18O=14.1～15.5‰), これも, 従来の研究の結果とほぼ一致した.
以上のことから, 我が国には最終氷期, 後氷期を通じて頻繁に風成塵が飛来し, また雨水や雪にともなって降下堆積し, 土壌の母材になったことが明らかとなった.抄録全体を表示PDF形式でダウンロード (772K) -
野村 亮太郎, 田中 眞吾1986 年 24 巻 4 号 p. 301-307
発行日: 1986/01/31
公開日: 2009/08/21
ジャーナル フリーPDF形式でダウンロード (1078K) -
大上 和良, 町田 瑞男, 吉田 充1986 年 24 巻 4 号 p. 309-313
発行日: 1986/01/31
公開日: 2009/08/21
ジャーナル フリーPDF形式でダウンロード (692K) -
藤 則雄1986 年 24 巻 4 号 p. 315-318
発行日: 1986/01/31
公開日: 2009/08/21
ジャーナル フリーPDF形式でダウンロード (437K) -
1986 年 24 巻 4 号 p. e1
発行日: 1986年
公開日: 2009/08/21
ジャーナル フリーPDF形式でダウンロード (72K)
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