Oil & Gas Training
and Competency Development

Location Bandung, Indonesia
Start07 May 2018
End11 May 2018
Discipline Geophysics ,
Petrophysics ,
Unconventional Resources ,
Duration5 Days
CostUSD 4,500.00
Delivery Mechanism Classroom

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Rock Physics - Integrating Petrophysical, Geomechanical, and Seismic Measurements

4.5 Average client rating (based on 117 attendee reviews)

Rock Physics is a key component in oil and gas exploration, development, and production. It combines concepts and principles from geology, geophysics, petrophysics, applied mathematics, and other disciplines.  Rock physics provides the empirical relationships, understanding and theory to connect petrophysical, geomechanical and seismic data to the intrinsic properties of rocks, such as mineralogy, porosity, pore shapes, pore fluids, pore pressures, stresses and overall architecture, such as laminations and fractures. Rock physics is needed to optimize all imaging and reservoir characterization solutions based on geophysical data, and to such data to build mechanical earth models for solving geomechanical problems. Attendees will obtain an understanding of the sensitivity of elastic waves in the earth to mineralogy, porosity, pore shapes, pore fluids, pore pressures, stresses, and the anisotropy of the rock fabric resulting from the depositional and stress history of the rock, and how to use this understanding in quantitative interpretation of seismic data and in the construction of mechanical earth models. A variety of applications and real data examples is presented.

  • Agenda
  • Audience
  • Prerequisites
  • Location
  • Agenda

    Day 1

    • Introduction
      • What is Rock Physics?
      • Rock Physics and Petrophysics. What’s the difference?
    • Hooke’s law, anisotropy and elastic wave velocities
    • Sedimentary rocks as heterogeneous media
    • The concept of the Representative Elementary Volume (REV) and effective elastic properties
    • Voigt/Reuss and Hashin-Shtrikman bounds
    • Modulus-porosity relations for clean sands
    • Critical porosity and mechanical percolation
    • Gassmann’s equations and fluid substitution
    • Fluid properties and mixtures 

    Day 2

    • Diagenetic and sorting trends in velocity-porosity data
    • Velocity-porosity models for shaly sands
    • Empirical relations between velocity and porosity, clay content, etc.
    • Properties of sand-clay mixtures
    • Velocity-porosity relations for shales
    • Relations between VP and VS
    • Rock compressibilities and relation of 4D seismic to well testing
    • Reflection coefficients and AVO
    • Elastic impedance
    • Rock physics templates
    • Effective medium and effective field theories
    • Velocity-porosity relations for carbonates


    Day 3

    • Biot theory
    • Patchy saturation
    • Squirt flow
    • Sediment compaction and the state of stress in the Earth
    • Pore pressure and the concept of effective stress
    • Poroelasticity
    • Application to pore pressure prediction 


    Day 4

    • Fracture gradient and 3D stress modeling
    • Effect of stress on seismic body waves
    • Third-order elasticity
    • Granular media and discrete element methods
    • Displacement discontinuity methods
    • Stress sensitivity of sandstones
    • Stress sensitivity of shales
    • Stress perturbations around a borehole
    • Determination of velocity variations around a borehole from advanced sonic logging
    • Application to wellbore stability
    • Reservoir geomechanics and stress effects in 4D seismic monitoring 

    Day 5

    • Fractured reservoirs
    • Hydraulic fracture propagation in presence of natural fractures
    • Seismic characterization of fractured reservoirs
    • Modeling the response of a fractured reservoir
    • Rock physics models for fractures
    • Shales and unconventional reservoirs
    • Anisotropy of shales
    • Rock physics modeling of kerogen in organic-rich shales
    • Effect of anisotropy on AVO
    • Microseismic and effect of azimuthal anisotropy on propagation of hydraulic fractures
  • Audience

    Geoscientists, petrophysicists, and engineers wishing to understand rock physics and learn how to work together in integrated teams to build geomechanical models.

  • Prerequisites

    A basic knowledge of Geology, Geophysics, and Petrophysics.

  • Prerequisites

  • Location


    Bandung is the capital of West Java province in Indonesia. Located 768 m (2,520 ft) above sea level, Bandung has relatively year-around cooler temperature than most other Indonesian cities

    Bandung Sky Line

    Bandung is renowned for its large stock of Dutch colonial architecture; most notably the tropical Art Deco architectural style. The modern and native architectural blending was followed by several Dutch architects that have shaped the city landmarks. In the 1930s, Bandung was known also as the city of architecture laboratory because of many Dutch architects made some experiments with new architectural designs.

    Bandung has served for popular weekend-break destination for people living in Jakarta for many reasons. The cooler climate of highland plantation area, the varieties of food, the cheaper fashion shops located in factory outlets and distros, golf courses, and the friendliness of local people have become the main attraction of the city.

    Bandung Husein Sastranegara International Airport serves direct flights to Batam, Surabaya, Yogyakarta, Denpasar, Palembang and Padang and also international services from Kuala Lumpur and Singapore Changi Airport. The airport is located nearby the Dirgantara aerospace complex and Dirgantara Fairground.

    From Wikitravel licensed under Creative Commons Attribution-ShareAlike 3.0

    • Timezone : GMT+07:00, Bangkok (Bangkok)
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