ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
黑濑川地体源于亚洲大陆东缘何处?
  
关键词:Kurosegawa Terrane  Fusulinacean  South China Block  Paleomagnetic
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作者单位E-mail
Shigeki HADA Faculty of Literature, Kobe Women’s University hada@mailgate.kobe-u.ac.jp 
Koji UNO Graduate School of Education, Okayama University  
Kuniyuki FURUKAWA Faculty of Business Administration, Aichi University  
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摘要:
Which Continental Block in the East Asian Continental Margin is the Source of the Kurosegawa Terrane?
      The point at issue: The Kurosegawa Terrane is composed of continental fragments transecting Mesozoic terranes of accretionary complex in Southwest Japan (Fig. 1). It is an attenuated tectonic sliver and considered to be allochthonous with respect to the main part of Southwest Japan. The problem of which continental block in the East Asian continental margin is the source of the Kurosegawa Terrane has puzzled Japanese geologists for many years. Firstly, we try to approach this issue based on the analysis of fusulinacean assemblage in accreted terranes composed of subduction complex in the Pacific Rim. Secondly, by applying the result of this analysis we try to locate the source of the continental fragments of the Kurosegawa Terrane. Thirdly, we try to prove its validity with a new paleomagnetic study.
Shigeki HADA,Koji UNO,Kuniyuki FURUKAWA.2012.Which Continental Block in the East Asian Continental Margin is the Source of the Kurosegawa Terrane?[J].Acta Geoscientica Sinica,33(s1):12-14.
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