Fluid flow and transport in rocks : mechanisms and effects
著者
書誌事項
Fluid flow and transport in rocks : mechanisms and effects
Chapman & Hall, c1997
- タイトル別名
-
Fluid flow and transport in rocks
大学図書館所蔵 全12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
This book represents the proceedings of the 9th written by a very active group of physicists at Kongsberg seminar, held at the Norwegian Mining the University of Oslo - physicists interested in Museum located in the city of Kongsberg about complex systems in general and geo-like systems 70 km Southwest of Oslo. The Kongsberg district in particular. is known for numerous Permian vein deposits of The content of the book is organized into three native silver, and mining activity in the area lasted major parts following the introductory chapter. for more than 300 years, finally ceasing in 1957. Chapters 2 to 7 primarily treat the role of fluids The previous eight Kongsberg seminars were in specific geological environments, ranging from focused on ore-forming processes and all of these sedimentary basins (Chapters 2-3) to contact were organized by Professor Arne Bj0rlykke, now metamorphic/hydrothermal scenarios (Chapters director of the Norwegian Geological Survey. 4-5) and regional metamorphic settings (Chapters Since process-orientated research tends to break 6-7). The following four chapters (8-11) focus down the traditional barriers between the different on various properties of fluid-rock systems that geological disciplines, this seminar has always are critical in controlling flow and transport been a meeting point for people with a variety through rocks. These include: mineral solubility of geological backgrounds.
目次
Fluid flow and transport in rocks: an overview. Lithological control on fluid flow in sedimentary basins.Polygonal extensional fault systems: a new class of structure formed during the early compaction of shales. Flow and transport during contact metamorphism and hydrothermal activity: examples from the Oslo rift. Porosity and permeability of carbonate rocks during contact metamorphism. The evolution of fluids through the metamorphic cycle. Fluid transport, deformation and metamorphism at depth in a collision zone. Coupled reaction and flow in subduction zones: silica metasomatism in the mantle wedge. Sufrace chemical controls on pore-fluid connectivity in texturally equilibrated materials. Quantification of microscopic porous networks by image analysis and measurements of permeability in the Soultz-sous-Forets granite (Alsace, France). Network topology and homogenization of fractrued rocks. Fractal structures in secondary migration. Flow along fractures in sedimentary basins. Mid-crustal focused fluid movement: thermal consequences and silica transport. Simulations of one-and two-phase flow in fractures. Transient versus continuous fluid flow in seismically active faults: an investigation by electric analogue and numerical modelling. Flow and focusing of metamorphic fluids.
「Nielsen BookData」 より