Archean crustal evolution
著者
書誌事項
Archean crustal evolution
(Developments in Precambrian geology, 11)
Elsevier, 1994
- pbk
大学図書館所蔵 全11件
  青森
  岩手
  宮城
  秋田
  山形
  福島
  茨城
  栃木
  群馬
  埼玉
  千葉
  東京
  神奈川
  新潟
  富山
  石川
  福井
  山梨
  長野
  岐阜
  静岡
  愛知
  三重
  滋賀
  京都
  大阪
  兵庫
  奈良
  和歌山
  鳥取
  島根
  岡山
  広島
  山口
  徳島
  香川
  愛媛
  高知
  福岡
  佐賀
  長崎
  熊本
  大分
  宮崎
  鹿児島
  沖縄
  韓国
  中国
  タイ
  イギリス
  ドイツ
  スイス
  フランス
  ベルギー
  オランダ
  スウェーデン
  ノルウェー
  アメリカ
注記
Includes bibliographical references and index
内容説明・目次
内容説明
The integration of Tectonics/Geochemistry, up-to-date reviews by leading scientists as well as a broad topical coverage of the Archean, are some of the features of this particular volume. As geochronology has progressed in the last 20 years, the Archean has continued to attract interest. Advancements in the understanding of Archean crustal and mantle evolution have progressed rapidly since the first International Archean Symposium in Western Australia (1970). The landmark for the Archean was the NATO Advanced Study Institute at Leicester (1975). At this meeting the Archean truly "came of age". Investigators from many different disciplines focused their expertise on the early history of the earth. For the first time, the nature of the atmosphere, oceans, and life during the Archean was an important part of an Archean symposium. During the most recent Archean Symposium in Perth in 1990, there was a shift in interest from field and trace element data to the new rapidly evolving high-precision U/Pb geochronology of Archean rocks and to detailed structural studies of both low and high grade Archean terrains. The terrane concept so widely applied to the Phanerozoic was proposed for the Archean Yilgarn Province in Western Australia and is now widely accepted for the Archean (as evident by the articles in this book). Plate tectonics is now widely accepted as the principal process that controls the history of continents and oceans. There are, though, well substantiated differences between Archean and post-Archean rocks that indicate that Archean tectonic regimes must have differed in some respects from modern ones. The question of how and to what degree did Archean plate tectonics differ from modern plate tectonics is treated in many of the chapters of this book. Altogether, the editor has presented a selection of articles that provide a fascinating insight into the latest observations in this field.
目次
Contributing Authors. Introduction (K.C. Condie). 1. Archean komatiites (N.T. Arndt). 2. Archean volcanic patterns (P.C. Thurston). 3. Greenstones through time (K.C. Condie). 4. Archean greenstone-related sedimentary rocks (D.R. Lowe). 5. Archean synrift and stable-shelf sedimentary successions (K.A. Eriksson, C.M. Fedo). 6. Archean grey gneisses and the genesis of continental crust (H. Martin). 7. Archean granite plutons (P.J. Sylvester). 8. Archean anorthosites (L.D. Aswal, J.S. Myers). 9. Archean high-grade metamorphism (J.A. Percival). 10. Archean and early Proterozoic evolution of the Siberian craton: a preliminary assessment (O.M. Rosen et al.). 11. Archean mineralization (D.I. Groves, M.E. Barley). 12. The Archean atmosphere: its composition and fate (D.J. Des Marais). Reference Index. Subject Index
「Nielsen BookData」 より