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 |

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 | Quartz arenite |
C | Shale |
D | Limy dolomite |
E | Shaly sandstone |
Question 2 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Sandstone |
B | Limestone |
C | Dolomite |
D | Anhydrite |
E | Glauconitic Sandstone |
Question 3 |

A | Just above position I |
B | At position III |
C | Just below position II |
D | Just above position II |
E | At position I |
Question 4 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Interbeds of coal and sand |
B | Slope channel deposit |
C | Transgressive marine shelf |
D | Channel point bar deposit |
E | Prograding marine shelf |
Question 6 |

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

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 | Clean sand |
D | Limestone with sand interbeds |
E | Carbonaceous sandstone |
Question 8 |

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 | Calcite |
C | Dolomite |
D | Limestone |
E | Shale |
F | Anhydrite |
Question 9 |

A | Interbeds of clean sand with shale |
B | Heavy metals |
C | Glauconitic sandstone |
D | Organic rich black shale |
E | Gas bearing sandstone |
Question 10 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Sandtone |
B | Caprock |
C | Shale |
D | Mudstone |
E | Seal |
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 3011 m |
B | At 2893 m |
C | At 2955 m |
D | At 3095 m |
E | At 2995 m |
Question 12 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | 40 degrees Southeast |
B | 150 degrees Northwest |
C | 30 degrees Northwest |
D | 50 degrees Southeast |
E | 60 degrees Southeast |
Question 13 |

A | Shale |
B | Clean limestone |
C | Sandstone |
D | Interbedded clean sandstone and shale |
E | Coal |
Question 14 |

Original at: image log; Borehole image log analysis for sedimentary environment and clay volume interpretation by A. Shahinpour (NTUN) 2013
A | Fracture 4, 6 and 7 |
B | It is impossible to determine. |
C | Fracture 5 and 6 |
D | Fracture 3, 8 and 9 |
E | Fracture 4 and 5 |
Question 15 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | Between 9550 ft to 9650 ft. |
B | From KB down to 9500 ft. |
C | From KB down to 9600 ft. |
D | Between 9500 ft and 9600 ft. |
Question 16 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | It is difficult to determine with the given log. |
B | AT30 (dashed blue line) |
C | AT90 (dashed red line) |
D | AT10 (black line) |
Question 17 |

Image credit: United States Geological Survey, online at USGS database
A | Borehole collapse |
B | Intentionally changed the drill bit |
C | Drilling mud infiltration |
D | High pressure due to increased in depth |
E | Soft lithological facies |
Question 18 |

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 | Water saturated zone |
C | Gas saturated zone |
D | Oil saturated zone |
E | Water invaded zone |
Question 19 |

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 | ~ 0.48 |
E | ~ 0.27 |

Question 20 |

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 | Argillaceous limestone |
C | Calcite |
D | Dolomite |
E | Shale |
F | Anhydrite |
Question 21 |

A | At around 2110 m of depth |
B | At around 2102 m of depth |
C | At around 2158 m of depth |
D | At around 2105 m of depth |
E | At around 2177 m of depth |
Question 22 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | 9640 ft |
B | 9540 ft |
C | 9600 ft |
D | 958 0ft |
E | 9500 ft |
Question 23 |

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 sandstone |
C | Feldspatic (K-spar rich) arenite |
D | Shaly sandstone |
E | Shale interbeded sandstone |
F | Gas-bearing dolomite |
Question 24 |

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

A | At around 2102 m of depth |
B | At around 2158 m of depth |
C | At around 2110 m of depth |
D | At around 2145m of depth |
E | At around 2180 m of depth |
Question 26 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Between 1049 m and 1055 m |
B | Between 1066 m and 1071 m |
C | Between 1066 m and 1078 m |
D | Between 1047 m and 1060 m |
E | Between 1071 m and 1078 m |
Question 28 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | Effective porosity |
B | Coal seams |
C | Fractures |
D | Hydrocarbon saturated zones |
E | Lithological contacts |
F | Bedding contacts |
Question 29 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2057 m (+/- 5m) |
B | 2047 m (+/- 5m) |
C | 2077 m (+/- 5m) |
D | 2047 m (+/- 5m) |
E | 2090 m (+/- 5m) |
Question 30 |

A | Coal |
B | Low density shale |
C | Organic rich black shale |
D | Heavy metals |
E | Shaly sandstone |
Question 31 |

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 | ~0.38 |
C | ~1.0 |
D | ~75 |
E | 0.0 |
Net sand interval = 3075 m - 3000 m = 75 m (read off the GR curve)
Hence, net:gross = 75 m/75 m = 1.0
Question 32 |


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 4 |
B | Fracture 4 and 5 |
C | Fracture 8 and 9 |
D | Fracture 7 |
E | Fracture 1 and 2 |
Question 33 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/07-eslog.htm
A | At around 414 m , 451 m , 457 m , 464 m and 475 m |
B | At around 416 m , 451 m , 457 m , 470 m and 475 m |
C | At around 412 m , 414 m , 422 m , 470 m and 475 m |
D | At around 414 m , 422 m , 464 m , 470 m and 477 m |
E | At around 416 m , 451 m , 464 m , 470 m and 475 m |
Question 34 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | At 1079 m |
B | At 1067 m |
C | At 1027 m |
D | At 1046.5 m |
E | At 1023 m |
Question 35 |

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 1211.5 m to 1239.5 m |
C | Between 1212.5 m to 1223.5 m |
D | Between 1209.5 m to 1211.5 m |
Question 36 |

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 470 m of depth |
C | Around 451 m of depth |
D | Around 422 m of depth |
E | Around 460 m of depth |
Question 37 |

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 2890 m and 2895 m |
C | Between 2970 m and 3075 m |
D | Between 2945 m and 2970 m |
E | At 3075 m |
Question 38 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Limestone |
B | Sandstone |
C | Dolomite |
D | Shale |
E | Anhydrite |
Question 39 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1066 m and ~1078 m |
B | Between ~1042 m and ~1043 m |
C | Between ~1066 m and ~1071 m |
D | Between ~1070 m and ~1078 m |
E | Between ~1025 m and ~1028 m |
Question 40 |

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 | Poor tool pads in the well |
D | Tight oil |
E | Borehole collapse |
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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.