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Finite Homogeneous Strain, Flow And Rupture Of Rocks

Om Finite Homogeneous Strain, Flow And Rupture Of Rocks

A specialized textbook on the mechanical properties of geological materials, with a focus on practical applications for mining and engineering. This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work is in the "public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.

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  • Språk:
  • Engelska
  • ISBN:
  • 9781022387263
  • Format:
  • Häftad
  • Utgiven:
  • 18. juli 2023
  • Mått:
  • 156x234x5 mm.
  • Vikt:
  • 136 g.
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Leveranstid: 2-4 veckor
Förväntad leverans: 9. december 2024

Beskrivning av Finite Homogeneous Strain, Flow And Rupture Of Rocks

A specialized textbook on the mechanical properties of geological materials, with a focus on practical applications for mining and engineering.
This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it.
This work is in the "public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work.
Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.

Användarnas betyg av Finite Homogeneous Strain, Flow And Rupture Of Rocks



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