مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

716
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

ESTIMATION OF FRAGMENTATION ON GEOMETRICAL VIEWPOINT

Pages

  51-61

Abstract

 Good estimation of FRAGMENTATION potential is very important topic before selection of CAVING EXTRACTION METHODS. In-situ FRAGMENTATION is result of discontinuities with zero tension strength but primary and secondary FRAGMENTATIONs happen in rock blocks that seem intact and without any discontinuity. In reality in these blocks when induced stresses (due to under cutting) or shock and stress (due to transition of rock mass) affect the blocks, weak surfaces such as rock bridges, veinlet and schistose surfaces (surfaces with tension strength) are first candidates for breakage and slice. Thus it is necessary to quantify these discontinuities in a rock mass. The purpose is to construct a way for prediction of potential discontinuities. In the next step based on necessary energy for breakage, potential discontinuities are classified. We try to design and construct a new method for quantifying and classifying discontinuities in rock mass.  This method helps us to have an initial estimate of FRAGMENTATION when induced stress and large scale displacement affect rock blocks. Rock bridges, veinlet and weak surfaces in rock like as schistose surfaces (surfaces with tension strength) are potential discontinuity. Those joints that have potential of being counted as discontinuities but are not considered discontinuity in in-situ form are put in class No, 2 versus IN SITU FRACTUREs (surfaces without tension strength) are classified No, 1. fractures which are created after large scale displacements are known class No, 3.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    EMAMI MEYBODI, E., & JALALI, S.M.E.. (2015). ESTIMATION OF FRAGMENTATION ON GEOMETRICAL VIEWPOINT. JOURNAL OF ANALYTICAL AND NUMERICAL METHODS IN MINING ENGINEERING, 5(9 ), 51-61. SID. https://sid.ir/paper/266028/en

    Vancouver: Copy

    EMAMI MEYBODI E., JALALI S.M.E.. ESTIMATION OF FRAGMENTATION ON GEOMETRICAL VIEWPOINT. JOURNAL OF ANALYTICAL AND NUMERICAL METHODS IN MINING ENGINEERING[Internet]. 2015;5(9 ):51-61. Available from: https://sid.ir/paper/266028/en

    IEEE: Copy

    E. EMAMI MEYBODI, and S.M.E. JALALI, “ESTIMATION OF FRAGMENTATION ON GEOMETRICAL VIEWPOINT,” JOURNAL OF ANALYTICAL AND NUMERICAL METHODS IN MINING ENGINEERING, vol. 5, no. 9 , pp. 51–61, 2015, [Online]. Available: https://sid.ir/paper/266028/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top
    telegram sharing button
    whatsapp sharing button
    linkedin sharing button
    twitter sharing button
    email sharing button
    email sharing button
    email sharing button
    sharethis sharing button