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  1. B100 理学部/理学研究科
  2. B100d 学位論文
  3. 博士論文(理博・論理博)

The Mesozoic Evolution of the Mino Terrane, Central Japan : A Geologic and Paleomagnetic Synthesis

http://hdl.handle.net/2237/12612
http://hdl.handle.net/2237/12612
841fb0ea-8bb3-457b-a0a6-a4585339c097
名前 / ファイル ライセンス アクション
ot2140_abstr.pdf ot2140_abstr.pdf (199.3 kB)
ot2140.pdf ot2140.pdf (2.6 MB)
Item type 学位論文 / Thesis or Dissertation(1)
公開日 2010-01-18
タイトル
タイトル The Mesozoic Evolution of the Mino Terrane, Central Japan : A Geologic and Paleomagnetic Synthesis
言語 en
その他のタイトル
その他のタイトル 美濃地域の中生代地史 : 地質学的および古地磁気学的考察
言語 ja
著者 服部, 勇

× 服部, 勇

WEKO 32351

ja 服部, 勇

Search repository
Hattori, Isamu

× Hattori, Isamu

WEKO 32352

en Hattori, Isamu

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
抄録
内容記述 The Mino tectono-stratigraphic terrane, central Japan, underlain bv Permian to Jurassic sedimentary and volcanic rocks of various origins, was formed through accretion processes associated with the Mesozoic sea-floor spreading. This conclusion has been reached mainly- from the following reasoning; 1. the entire boundary of this terrane is defined by tectonic belts with high-pressure metamorphic rocks and serpentinzed ultramafic rocks, 2. the chemistry and petrology of the Permian greenstones demonstrate their affinity with abyssal tholeiitic and alkalic basalts, 3・the widespread, but chaotic, occurrence of Permian greenstones, Triassic cherts, and Jurassic siliceous shales in the younger Jurassic clastic rocks of this terrane suggests extensive post -depositional mixing of strata, 4. the sedimentology of the Jurassic sandstones strongly suggests that they are turbidity-current deposits supplied from cratonic lands, 5. the South-Pacific type fossil assemblage in the Mino terrane shows strong contrast with the North-Pacific type fossil assemblage of the adjacent terranes, 6. the paleomagnetism of the Permian and Jurassic greenstones, the Triassic cherts, and the Jurassic siliceous shales implies long-distance northward drift in the Cretaceous- time of these rocks from their original low latitudinal regions. Along with this northward migration, the Mino terrane was accreted with extensive internal deformation to northeast Asia including the present Hida terrane. Recent accumulation of paleomagnetic and paleontologic data in the Pacific peripheral regions appears to support the existence of many allochthonoum,s terranes which migrated from the equatorial regions. The Mino terrane may be regarded as one example of these Circum-pacific allochthons.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 名古屋大学博士学位論文 学位の種類 : 理学博士(論文) 学位授与年月日 : 昭和57年3月23日
言語 ja
内容記述タイプ Other
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_db06
タイプ doctoral thesis
書誌情報
発行日 1982-03-23
学位名
言語 ja
学位名 理学博士
学位授与機関
学位授与機関識別子Scheme kakenhi
学位授与機関識別子 13901
言語 ja
学位授与機関名 名古屋大学
言語 en
学位授与機関名 Nagoya University
学位授与年度
学位授与年度 1981
学位授与年月日
学位授与年月日 1982-03-23
学位授与番号
学位授与番号 乙第2140号
フォーマット
application/pdf
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/12612
識別子タイプ HDL
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