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
A | Between ~1025 m and ~1028 m |
B | Between ~1070 m and ~1078 m |
C | Between ~1042 m and ~1043 m |
D | Between ~1066 m and ~1071 m |
E | Between ~1066 m and ~1078 m |
Question 2 |

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 1047 m and 1060 m |
C | Between 1049 m and 1055 m |
D | Between 1066 m and 1071 m |
E | Between 1066 m and 1078 m |
Question 3 |

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 | Fracture 4, 6 and 7 |
C | Fracture 5 and 6 |
D | It is impossible to determine. |
E | Fracture 3, 8 and 9 |
Question 4 |

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 | Clean sand |
D | Carbonaceous sandstone |
E | Dolomite |
Question 5 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2077 m (+/- 5m) |
B | 2047 m (+/- 5m) |
C | 2090 m (+/- 5m) |
D | 2047 m (+/- 5m) |
E | 2057 m (+/- 5m) |
Question 7 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Transgressive marine shelf |
B | Prograding marine shelf |
C | Channel point bar deposit |
D | Slope channel deposit |
E | Interbeds of coal and sand |
Question 8 |

Image credit: United States Geological Survey, online at USGS database
A | Soft lithological facies |
B | Drilling mud infiltration |
C | Intentionally changed the drill bit |
D | Borehole collapse |
E | High pressure due to increased in depth |
Question 9 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Gas saturated zone |
B | Coal seam regions |
C | Water saturated zone |
D | Oil saturated zone |
E | Water invaded zone |
Question 11 |

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 12 |

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 465 m of depth |
E | Around 422 m of depth |
Question 13 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Shale |
B | Dolomite |
C | Argillaceous dolomite |
D | Calcite |
E | Anhydrite |
F | Argillaceous limestone |
Question 14 |

A | At around 2158 m of depth |
B | At around 2145m of depth |
C | At around 2180 m of depth |
D | At around 2102 m of depth |
E | At around 2110 m of depth |
Question 15 |

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 | Bedding contacts |
C | Coal seams |
D | Hydrocarbon saturated zones |
E | Lithological contacts |
F | Fractures |
Question 16 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Limestone |
B | Glauconitic Sandstone |
C | Anhydrite |
D | Dolomite |
E | Sandstone |
Question 17 |


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 and 5 |
B | Fracture 7 |
C | Fracture 8 and 9 |
D | Fracture 1 and 2 |
E | Fracture 4 |
Question 18 |

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 1023 m |
D | At 1046.5 m |
E | At 1027 m |
Question 19 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Between 2890 m and 2895 m |
B | Between 2945 m and 2970 m |
C | Between 3075 m and 3085 m |
D | At 3075 m |
E | Between 2970 m and 3075 m |
Question 20 |

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 limestone |
C | Dolomite |
D | Limestone |
E | Anhydrite |
F | Calcite |
Question 21 |

A | Interbedded clean sandstone and shale |
B | Sandstone |
C | Coal |
D | Clean limestone |
E | Shale |
Question 22 |

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 | Between 9500 ft and 9600 ft. |
C | From KB down to 9500 ft. |
D | From KB down to 9600 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 | At 3011 m |
B | At 2995 m |
C | At 2893 m |
D | At 2955 m |
E | At 3095 m |
Question 24 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Shale |
B | Limestone |
C | Dolomite |
D | Sandstone |
E | Anhydrite |
Question 25 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | ~75 |
B | ~1.0 |
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 |

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

Question 27 |

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 28 |

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 | Shaly sandstone |
C | Quartz arenite |
D | Shale |
E | Limy dolomite |
Question 29 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Between 1211.5 m to 1239.5 m |
B | Between 1212.5 m to 1223.5 m |
C | Between 1209.5 m to 1211.5 m |
D | Between 1203 m to 1239.5 m |
Question 30 |

A | Just above position II |
B | Just below position II |
C | Just above position I |
D | At position I |
E | At position III |
Question 31 |

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

A | Gas bearing sandstone |
B | Interbeds of clean sand with shale |
C | Organic rich black shale |
D | Glauconitic sandstone |
E | Heavy metals |
Question 33 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Caprock |
B | Shale |
C | Sandtone |
D | Seal |
E | Mudstone |
Question 34 |

A | At around 2177 m of depth |
B | At around 2158 m of depth |
C | At around 2105 m of depth |
D | At around 2110 m of depth |
E | At around 2102 m of depth |
Question 35 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Gas-bearing dolomite |
B | Shaly sandstone |
C | Gas-bearing calcite |
D | Gas-bearing sandstone |
E | Shale interbeded sandstone |
F | Feldspatic (K-spar rich) arenite |
Question 36 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Tight oil |
B | Signal interference or poor tool calibration |
C | Poor tool pads in the well |
D | Borehole collapse |
E | Inaccuracies in measurements due to mud infiltration |
Question 37 |

A | Fresh water |
B | Natural gas |
C | Brine water |
D | Oil (petroleum) |
E | Low density bitumen |
Question 38 |

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 | 30 degrees Northwest |
C | 150 degrees Northwest |
D | 50 degrees Southeast |
E | 60 degrees Southeast |
Question 39 |

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 412 m , 414 m , 422 m , 470 m and 475 m |
C | At around 414 m , 422 m , 464 m , 470 m and 477 m |
D | At around 416 m , 451 m , 457 m , 470 m and 475 m |
E | At around 414 m , 451 m , 457 m , 464 m and 475 m |
Question 40 |

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