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 |

Original at: image log; Borehole image log analysis for sedimentary environment and clay volume interpretation by A. Shahinpour (NTUN) 2013
A | It is impossible to determine. |
B | Fracture 3, 8 and 9 |
C | Fracture 4, 6 and 7 |
D | Fracture 4 and 5 |
E | Fracture 5 and 6 |
Question 2 |

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 414 m , 451 m , 457 m , 464 m and 475 m |
C | At around 416 m , 451 m , 457 m , 470 m and 475 m |
D | At around 416 m , 451 m , 464 m , 470 m and 475 m |
E | At around 414 m , 422 m , 464 m , 470 m and 477 m |
Question 3 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | 9500 ft |
B | 9600 ft |
C | 9540 ft |
D | 958 0ft |
E | 9640 ft |
Question 4 |

A | Just below position II |
B | Just above position II |
C | Just above position I |
D | At position I |
E | At position III |
Question 5 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1070 m and ~1078 m |
B | Between ~1042 m and ~1043 m |
C | Between ~1066 m and ~1078 m |
D | Between ~1066 m and ~1071 m |
E | Between ~1025 m and ~1028 m |
Question 6 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | Around 465 m of depth |
B | Around 451 m of depth |
C | Around 460 m of depth |
D | Around 422 m of depth |
E | Around 470 m of depth |
Question 7 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Oil saturated zone |
B | Water invaded zone |
C | Water saturated zone |
D | Coal seam regions |
E | Gas saturated zone |
Question 8 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1025 m and ~1028 m |
B | Between ~1066 m and ~1071 m |
C | Between ~1042 m and ~1043 m |
D | Between ~1066 m and ~1078 m |
E | Between ~1070 m and ~1078 m |
Question 9 |

A | Trangessive marine shelf |
B | Prograding delta |
C | Braided channel |
D | Slope channel |
E | Super-fan depositional lobes |
F | Channel-point bar |
Question 10 |

A | Shale |
B | Sandstone |
C | Clean limestone |
D | Interbedded clean sandstone and shale |
E | Coal |
Question 11 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Sandstone |
B | Anhydrite |
C | Glauconitic Sandstone |
D | Dolomite |
E | Limestone |
Question 12 |

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


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 7 |
B | Fracture 1 and 2 |
C | Fracture 8 and 9 |
D | Fracture 4 |
E | Fracture 4 and 5 |
Question 14 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | 60 degrees Southeast |
B | 50 degrees Southeast |
C | 150 degrees Northwest |
D | 40 degrees Southeast |
E | 30 degrees Northwest |
Question 15 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Channel point bar deposit |
B | Slope channel deposit |
C | Prograding marine shelf |
D | Interbeds of coal and sand |
E | Transgressive marine shelf |
Question 16 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Seal |
B | Caprock |
C | Mudstone |
D | Shale |
E | Sandtone |
Question 17 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2047 m (+/- 5m) |
B | 2047 m (+/- 5m) |
C | 2077 m (+/- 5m) |
D | 2090 m (+/- 5m) |
E | 2057 m (+/- 5m) |
Question 18 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | ~0.38 |
B | ~75 |
C | 0.0 |
D | ~1.0 |
E | ~0.013 |
Net sand interval = 3075 m - 3000 m = 75 m (read off the GR curve)
Hence, net:gross = 75 m/75 m = 1.0
Question 19 |

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 2995 m |
E | At 2893 m |
Question 20 |

A | Shaly sandstone |
B | Heavy metals |
C | Coal |
D | Organic rich black shale |
E | Low density 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 | Between 2945 m and 2970 m |
B | At 3075 m |
C | Between 2970 m and 3075 m |
D | Between 3075 m and 3085 m |
E | Between 2890 m and 2895 m |
Question 22 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Dolomite |
B | Dolomite with clay interbeds |
C | Carbonaceous sandstone |
D | Clean sand |
E | Limestone with sand interbeds |
Question 23 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Inaccuracies in measurements due to mud infiltration |
B | Poor tool pads in the well |
C | Borehole collapse |
D | Signal interference or poor tool calibration |
E | Tight oil |
Question 24 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Between 1203 m to 1239.5 m |
B | Between 1209.5 m to 1211.5 m |
C | Between 1211.5 m to 1239.5 m |
D | Between 1212.5 m to 1223.5 m |
Question 25 |

A | Interbeds of clean sand with shale |
B | Gas bearing sandstone |
C | Glauconitic sandstone |
D | Organic rich black shale |
E | Heavy metals |
Question 26 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Limy dolomite |
B | Quartz arenite |
C | Shaly sandstone |
D | Dolomitic pelmicrite |
E | Shale |
Question 27 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | AT10 (black line) |
B | It is difficult to determine with the given log. |
C | AT90 (dashed red line) |
D | AT30 (dashed blue line) |
Question 28 |

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 9600 ft. |
B | Between 9500 ft and 9600 ft. |
C | From KB down to 9500 ft. |
D | Between 9550 ft to 9650 ft. |
Question 29 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Argillaceous dolomite |
B | Anhydrite |
C | Dolomite |
D | Calcite |
E | Shale |
F | Argillaceous limestone |
Question 30 |

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 1047 m and 1060 m |
C | Between 1071 m and 1078 m |
D | Between 1049 m and 1055 m |
E | Between 1066 m and 1078 m |
Question 31 |

Image credit: United States Geological Survey, online at USGS database
A | Intentionally changed the drill bit |
B | High pressure due to increased in depth |
C | Borehole collapse |
D | Soft lithological facies |
E | Drilling mud infiltration |
Question 32 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Gas-bearing sandstone |
B | Feldspatic (K-spar rich) arenite |
C | Gas-bearing calcite |
D | Shaly sandstone |
E | Gas-bearing dolomite |
F | Shale interbeded sandstone |
Question 33 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | Fractures |
B | Coal seams |
C | Lithological contacts |
D | Bedding contacts |
E | Hydrocarbon saturated zones |
F | Effective porosity |
Question 34 |

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 | ~ 0.18 |
C | ~ 0.36 |
D | ~ 0.24 |
E | ~ 0.27 |

Question 35 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | At 1023 m |
B | At 1046.5 m |
C | At 1079 m |
D | At 1067 m |
E | At 1027 m |
Question 36 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Sandstone |
B | Shale |
C | Anhydrite |
D | Limestone |
E | Dolomite |
Question 37 |

A | At around 2102 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 2110 m of depth |
Question 38 |

A | Brine water |
B | Low density bitumen |
C | Natural gas |
D | Oil (petroleum) |
E | Fresh water |
Question 39 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-whatisalog.htm
A | High concentration of gas ("gas effect") |
B | Presence of hydrocarbons |
C | Coal bearing formation |
D | High porosity formation |
E | Sandstone formation |
Question 40 |

A | At around 2110 m of depth |
B | At around 2158 m of depth |
C | At around 2177 m of depth |
D | At around 2105 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.