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Continuum Mechanics Aspects of Geodynamics and Rock Fracture Mechanics
  • Language: en
  • Pages: 282

Continuum Mechanics Aspects of Geodynamics and Rock Fracture Mechanics

During a NATO Advanced Study Institute in Izmir, Tur key, July 1973 on Modern Developments in Engineering Seis mology and Earthquake Engineering it emerged that a debate on Continuum Mechanics Aspects of Geodynamics and Rock Fracture Mechanics would be very welcome. Therefore, it was decided to seek NATO sponsorship for an Advanced Study In stitute on this subject. The purpose of the new Advanced Study Institute was to provide a link between mechanics of continuum media and geo dynamic s. By bringing together a group of leading scientists from the above two fields and participants actively engaged in research and applications in the same fields, it was believed that fruitful discussions coul...

Geophysik I / Geophysics I
  • Language: en
  • Pages: 667

Geophysik I / Geophysics I

None

Geophysical Abstracts
  • Language: en
  • Pages: 864

Geophysical Abstracts

  • Type: Book
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  • Published: 1966
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  • Publisher: Unknown

None

Bulletin
  • Language: en
  • Pages: 348

Bulletin

  • Type: Book
  • -
  • Published: 1955
  • -
  • Publisher: Unknown

None

Elasticity of Materials
  • Language: en
  • Pages: 107

Elasticity of Materials

In the science of physics, elasticity is the ability of a deformable body (e.g., steel, aluminum, rubber, wood, crystals, etc.) to resist a distorting effect and to return to its original size and shape when that influence or force is removed. Solid bodies will deform when satisfying forces are applied to them. Elasticity solution of materials will be grouped in forms of linear and nonlinear elasticity formulations. The main subject of this book is engineering elasticity and consists of five chapters in two main sections. These two main sections are "General Theorems in Elasticity" and "Engineering Applications in Theory of Elasticity." The first chapter of the first section belongs to the e...

Geophysical Abstracts ...
  • Language: en
  • Pages: 1270

Geophysical Abstracts ...

  • Type: Book
  • -
  • Published: 1966
  • -
  • Publisher: Unknown

None

Bulletin
  • Language: en
  • Pages: 934

Bulletin

  • Type: Book
  • -
  • Published: 1965
  • -
  • Publisher: Unknown

None

Translator Positioning in Characterisation
  • Language: en
  • Pages: 161

Translator Positioning in Characterisation

Applying Systemic Functional Linguistics (SFL) to Descriptive Translation Studies (DTS), to three translations of a classic Chinese text, Zhao proposes a new model for linking translator positioning with translational norms in the target culture. Zhao combines the Appraisal model from SFL with a characterisation model to describe the role of translator positioning in character construction. Looking at three different translations of the classic Chinese novel Luotuo Xiangzi, she uses corpus tools to compare the opening and ending chapters of each translation, identifying textual patterns of translator positioning. She then analyses and compares the cover designs of the translated novels and reconstructs the translational norms governing the translator’s positioning in characterisation. In doing so she contributes to DTS by developing a systematic and consistent framework to analyse verbal and visual elements in translated novels. Her multimodal analysis also provides insights into the broader patterns of translated language. An insightful read for scholars interested in both theoretical and empirical approaches to translation studies.

Geological Survey Bulletin
  • Language: en
  • Pages: 1024

Geological Survey Bulletin

  • Type: Book
  • -
  • Published: 1965
  • -
  • Publisher: Unknown

None

Principles of Geodynamics
  • Language: en
  • Pages: 413

Principles of Geodynamics

Geodynamics is commonly thought to be one of the subjects which provide the basis for understanding the origin of the visible surface features of the Earth: the latter are usually assumed as having been built up by geodynamic forces originating inside the Earth ("endogenetic" processes) and then as having been degrad ed by geomorphological agents originating in the atmosphere and ocean ("exogenetic" agents). The modem view holds that the sequence of events is not as neat as it was once thought to be, and that, in effect, both geodynamic and geomorphological processes act simultaneously ("Principle of Antagonism"); however, the division of theoretical geology into the principles of geodynamic...