Warning!
All log images are copyrighted and have been reproduced on this site with permission. The original copyright holder is not, Sanuja Senanayake.Petrophysical (Well) Log Interpretation or Petrophysics Log Interpretation is a specialized area of science that deals with borehole data. In Canada, it is typically taught with physical core log interpretation and other geological and engineering fundamental concepts in most universities. Technical educational institutions and professional organizations offer courses in well log interpretation as a stand along subject. You can learn in depth at CRAIN’S PETROPHYSICAL HANDBOOK (www.spec2000.net). This page is best viewed on desktop computers due to small font size in well logs.
Disclaimer: While every reasonable effort is made to ensure that the information provided is accurate, no guarantees for the currency or accuracy of information are made. It takes several proof readings and rewrites to bring the quiz to an exceptional level. If you find an error, please contact me as soon as possible. Please indicate the question ID-Number or description because server may randomize the questions and answers.
Petrophysical Log Interpretation
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Question 1 |

A | Heavy metals |
B | Organic rich black shale |
C | Shaly sandstone |
D | Coal |
E | Low density shale |
Question 2 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Slope channel deposit |
B | Channel point bar deposit |
C | Interbeds of coal and sand |
D | Prograding marine shelf |
E | Transgressive marine shelf |
Question 3 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Coal seam regions |
B | Gas saturated zone |
C | Water invaded zone |
D | Water saturated zone |
E | Oil saturated zone |
Question 4 |

Original at: image log; Borehole image log analysis for sedimentary environment and clay volume interpretation by A. Shahinpour (NTUN) 2013
A | Fracture 3, 8 and 9 |
B | Fracture 4 and 5 |
C | It is impossible to determine. |
D | Fracture 4, 6 and 7 |
E | Fracture 5 and 6 |
Question 5 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Calcite |
B | Dolomite |
C | Shale |
D | Anhydrite |
E | Limestone |
F | Argillaceous limestone |
Question 6 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-whatisalog.htm
A | High porosity formation |
B | High concentration of gas ("gas effect") |
C | Coal bearing formation |
D | Sandstone formation |
E | Presence of hydrocarbons |
Question 7 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1070 m and ~1078 m |
B | Between ~1066 m and ~1071 m |
C | Between ~1066 m and ~1078 m |
D | Between ~1025 m and ~1028 m |
E | Between ~1042 m and ~1043 m |
Question 8 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | ~ 0.48 |
B | ~ 0.27 |
C | ~ 0.24 |
D | ~ 0.18 |
E | ~ 0.36 |

Question 9 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Feldspatic (K-spar rich) arenite |
B | Gas-bearing calcite |
C | Shaly sandstone |
D | Gas-bearing dolomite |
E | Gas-bearing sandstone |
F | Shale interbeded sandstone |
Question 10 |

A | Prograding delta |
B | Braided channel |
C | Channel-point bar |
D | Super-fan depositional lobes |
E | Slope channel |
F | Trangessive marine shelf |
Question 11 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | At 3075 m |
B | Between 2890 m and 2895 m |
C | Between 2945 m and 2970 m |
D | Between 2970 m and 3075 m |
E | Between 3075 m and 3085 m |
Question 12 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | 9540 ft |
B | 9500 ft |
C | 9640 ft |
D | 9600 ft |
E | 958 0ft |
Question 13 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | At around 412 m , 414 m , 422 m , 470 m and 475 m |
B | At around 416 m , 451 m , 464 m , 470 m and 475 m |
C | At around 414 m , 422 m , 464 m , 470 m and 477 m |
D | At around 414 m , 451 m , 457 m , 464 m and 475 m |
E | At around 416 m , 451 m , 457 m , 470 m and 475 m |
Question 14 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Inaccuracies in measurements due to mud infiltration |
B | Signal interference or poor tool calibration |
C | Tight oil |
D | Borehole collapse |
E | Poor tool pads in the well |
Question 15 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Dolomite with clay interbeds |
B | Dolomite |
C | Clean sand |
D | Carbonaceous sandstone |
E | Limestone with sand interbeds |
Question 16 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | At 1046.5 m |
B | At 1023 m |
C | At 1027 m |
D | At 1067 m |
E | At 1079 m |
Question 17 |

A | Gas bearing sandstone |
B | Heavy metals |
C | Interbeds of clean sand with shale |
D | Glauconitic sandstone |
E | Organic rich black shale |
Question 18 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Anhydrite |
B | Shale |
C | Dolomite |
D | Limestone |
E | Sandstone |
Question 19 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | 50 degrees Southeast |
B | 150 degrees Northwest |
C | 40 degrees Southeast |
D | 30 degrees Northwest |
E | 60 degrees Southeast |
Question 20 |

A | Clean limestone |
B | Coal |
C | Sandstone |
D | Shale |
E | Interbedded clean sandstone and shale |
Question 21 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Shaly sandstone |
B | Dolomitic pelmicrite |
C | Limy dolomite |
D | Shale |
E | Quartz arenite |
Question 22 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | At 3095 m |
B | At 3011 m |
C | At 2955 m |
D | At 2893 m |
E | At 2995 m |
Question 23 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | From KB down to 9500 ft. |
B | Between 9550 ft to 9650 ft. |
C | From KB down to 9600 ft. |
D | Between 9500 ft and 9600 ft. |
Question 24 |

A | Brine water |
B | Oil (petroleum) |
C | Natural gas |
D | Low density bitumen |
E | Fresh water |
Question 25 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Between 1066 m and 1071 m |
B | Between 1071 m and 1078 m |
C | Between 1049 m and 1055 m |
D | Between 1047 m and 1060 m |
E | Between 1066 m and 1078 m |
Question 26 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1066 m and ~1071 m |
B | Between ~1070 m and ~1078 m |
C | Between ~1066 m and ~1078 m |
D | Between ~1042 m and ~1043 m |
E | Between ~1025 m and ~1028 m |
Question 27 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2057 m (+/- 5m) |
B | 2047 m (+/- 5m) |
C | 2047 m (+/- 5m) |
D | 2090 m (+/- 5m) |
E | 2077 m (+/- 5m) |
Question 28 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Glauconitic Sandstone |
B | Limestone |
C | Dolomite |
D | Anhydrite |
E | Sandstone |
Question 29 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Seal |
B | Sandtone |
C | Mudstone |
D | Shale |
E | Caprock |
Question 30 |

Image credit: United States Geological Survey, online at USGS database
A | Borehole collapse |
B | High pressure due to increased in depth |
C | Soft lithological facies |
D | Drilling mud infiltration |
E | Intentionally changed the drill bit |
Question 31 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | AT90 (dashed red line) |
B | AT10 (black line) |
C | It is difficult to determine with the given log. |
D | AT30 (dashed blue line) |
Question 32 |

A | At position I |
B | Just below position II |
C | At position III |
D | Just above position I |
E | Just above position II |
Question 33 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | ~0.013 |
B | 0.0 |
C | ~1.0 |
D | ~0.38 |
E | ~75 |
Net sand interval = 3075 m - 3000 m = 75 m (read off the GR curve)
Hence, net:gross = 75 m/75 m = 1.0
Question 34 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Between 1209.5 m to 1211.5 m |
B | Between 1203 m to 1239.5 m |
C | Between 1211.5 m to 1239.5 m |
D | Between 1212.5 m to 1223.5 m |
Question 35 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Argillaceous limestone |
B | Anhydrite |
C | Shale |
D | Calcite |
E | Dolomite |
F | Argillaceous dolomite |
Question 36 |


Original at: schematic diagram; http://www.google.com/patents/US20110064277
image log; Borehole image log analysis for sedimentary environment and clay volume interpretation by A. Shahinpour (NTUN) 2013
A | Fracture 1 and 2 |
B | Fracture 4 |
C | Fracture 8 and 9 |
D | Fracture 7 |
E | Fracture 4 and 5 |
Question 37 |

A | At around 2177 m of depth |
B | At around 2110 m of depth |
C | At around 2105 m of depth |
D | At around 2102 m of depth |
E | At around 2158 m of depth |
Question 38 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | Lithological contacts |
B | Coal seams |
C | Fractures |
D | Hydrocarbon saturated zones |
E | Bedding contacts |
F | Effective porosity |
Question 39 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | Around 470 m of depth |
B | Around 460 m of depth |
C | Around 451 m of depth |
D | Around 422 m of depth |
E | Around 465 m of depth |
Question 40 |

A | At around 2110 m of depth |
B | At around 2145m of depth |
C | At around 2180 m of depth |
D | At around 2158 m of depth |
E | At around 2102 m of depth |
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Credits: Based on the excellent class notes provided by, Dr. Rudi Meyer during Fall 2014 and the generous support from CRAIN’S PETROPHYSICAL HANDBOOK (spec2000.net) by supplying the petrophysical well log images. Some of the welllogs are produced by E.R. Crain, P.Eng. Those logs obtianed from E.R. Crain is the copyrighted intellectual property of the author.
FAQ | Report an Error
Supplementary Materials
Petrophysical Techniques; Geology/Geophysics (449)
Introduction to Petroleum Geology (577)
CRAIN’S PETROPHYSICAL HANDBOOK (www.spec2000.net)
If you are a company or an organization willing to donate copies of well logs, please contact me. I really appreciate your contributions and proper credits will be provided.