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 | Interbedded clean sandstone and shale |
B | Sandstone |
C | Clean limestone |
D | Coal |
E | Shale |
Question 2 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | 9600 ft |
B | 9640 ft |
C | 9540 ft |
D | 9500 ft |
E | 958 0ft |
Question 3 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Signal interference or poor tool calibration |
B | Borehole collapse |
C | Poor tool pads in the well |
D | Tight oil |
E | Inaccuracies in measurements due to mud infiltration |
Question 4 |

A | Slope channel |
B | Super-fan depositional lobes |
C | Channel-point bar |
D | Trangessive marine shelf |
E | Braided channel |
F | Prograding delta |
Question 5 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Dolomite |
B | Limestone |
C | Shale |
D | Anhydrite |
E | Sandstone |
Question 6 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | Hydrocarbon saturated zones |
B | Coal seams |
C | Lithological contacts |
D | Effective porosity |
E | Bedding contacts |
F | Fractures |
Question 7 |

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 | 30 degrees Northwest |
C | 40 degrees Southeast |
D | 150 degrees Northwest |
E | 60 degrees Southeast |
Question 8 |

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

Question 9 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | At around 416 m , 451 m , 464 m , 470 m and 475 m |
B | At around 416 m , 451 m , 457 m , 470 m and 475 m |
C | At around 414 m , 422 m , 464 m , 470 m and 477 m |
D | At around 412 m , 414 m , 422 m , 470 m and 475 m |
E | At around 414 m , 451 m , 457 m , 464 m and 475 m |
Question 10 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1070 m and ~1078 m |
B | Between ~1066 m and ~1078 m |
C | Between ~1042 m and ~1043 m |
D | Between ~1066 m and ~1071 m |
E | Between ~1025 m and ~1028 m |
Question 11 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Shale |
B | Argillaceous dolomite |
C | Argillaceous limestone |
D | Anhydrite |
E | Calcite |
F | Dolomite |
Question 12 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Between 1071 m and 1078 m |
B | Between 1066 m and 1071 m |
C | Between 1047 m and 1060 m |
D | Between 1066 m and 1078 m |
E | Between 1049 m and 1055 m |
Question 14 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Calcite |
B | Shale |
C | Anhydrite |
D | Limestone |
E | Dolomite |
F | Argillaceous limestone |
Question 15 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Glauconitic Sandstone |
B | Sandstone |
C | Anhydrite |
D | Limestone |
E | Dolomite |
Question 16 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1066 m and ~1071 m |
B | Between ~1025 m and ~1028 m |
C | Between ~1042 m and ~1043 m |
D | Between ~1066 m and ~1078 m |
E | Between ~1070 m and ~1078 m |
Question 17 |

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 1067 m |
C | At 1079 m |
D | At 1027 m |
E | At 1046.5 m |
Question 18 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Limestone with sand interbeds |
B | Dolomite with clay interbeds |
C | Carbonaceous sandstone |
D | Clean sand |
E | Dolomite |
Question 19 |

A | At around 2158 m of depth |
B | At around 2105 m of depth |
C | At around 2177 m of depth |
D | At around 2102 m of depth |
E | At around 2110 m of depth |
Question 20 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Dolomitic pelmicrite |
B | Shale |
C | Quartz arenite |
D | Limy dolomite |
E | Shaly sandstone |
Question 21 |

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 22 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2090 m (+/- 5m) |
B | 2057 m (+/- 5m) |
C | 2047 m (+/- 5m) |
D | 2047 m (+/- 5m) |
E | 2077 m (+/- 5m) |
Question 23 |

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 | High porosity formation |
C | Presence of hydrocarbons |
D | Coal bearing formation |
E | Sandstone formation |
Question 24 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | At 2955 m |
B | At 2893 m |
C | At 3095 m |
D | At 3011 m |
E | At 2995 m |
Question 25 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | ~1.0 |
B | ~75 |
C | 0.0 |
D | ~0.013 |
E | ~0.38 |
Net sand interval = 3075 m - 3000 m = 75 m (read off the GR curve)
Hence, net:gross = 75 m/75 m = 1.0
Question 26 |

A | Heavy metals |
B | Organic rich black shale |
C | Interbeds of clean sand with shale |
D | Glauconitic sandstone |
E | Gas bearing sandstone |
Question 27 |

A | Just above position I |
B | At position III |
C | At position I |
D | Just above position II |
E | Just below position II |
Question 28 |


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 8 and 9 |
B | Fracture 4 |
C | Fracture 7 |
D | Fracture 1 and 2 |
E | Fracture 4 and 5 |
Question 29 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Water saturated zone |
B | Oil saturated zone |
C | Coal seam regions |
D | Water invaded zone |
E | Gas saturated zone |
Question 31 |

A | Shaly sandstone |
B | Heavy metals |
C | Coal |
D | Organic rich black shale |
E | Low density shale |
Question 32 |

Original at: image log; Borehole image log analysis for sedimentary environment and clay volume interpretation by A. Shahinpour (NTUN) 2013
A | Fracture 4 and 5 |
B | It is impossible to determine. |
C | Fracture 5 and 6 |
D | Fracture 3, 8 and 9 |
E | Fracture 4, 6 and 7 |
Question 33 |

A | At around 2145m of depth |
B | At around 2110 m of depth |
C | At around 2158 m of depth |
D | At around 2180 m of depth |
E | At around 2102 m of depth |
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 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 35 |

A | Natural gas |
B | Oil (petroleum) |
C | Low density bitumen |
D | Brine water |
E | Fresh water |
Question 36 |

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 | Transgressive marine shelf |
E | Interbeds of coal and sand |
Question 37 |

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 9550 ft to 9650 ft. |
C | From KB down to 9500 ft. |
D | Between 9500 ft and 9600 ft. |
Question 38 |

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 422 m of depth |
C | Around 465 m of depth |
D | Around 451 m of depth |
E | Around 460 m of depth |
Question 39 |

Image credit: United States Geological Survey, online at USGS database
A | Borehole collapse |
B | Soft lithological facies |
C | Intentionally changed the drill bit |
D | Drilling mud infiltration |
E | High pressure due to increased in depth |
Question 40 |

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