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/07-eslog.htm
A | Around 470 m of depth |
B | Around 465 m of depth |
C | Around 451 m of depth |
D | Around 460 m of depth |
E | Around 422 m of depth |
Question 2 |

A | Prograding delta |
B | Channel-point bar |
C | Braided channel |
D | Super-fan depositional lobes |
E | Slope channel |
F | Trangessive marine shelf |
Question 3 |

A | Shaly sandstone |
B | Organic rich black shale |
C | Low density shale |
D | Heavy metals |
E | Coal |
Question 4 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Caprock |
B | Sandtone |
C | Seal |
D | Mudstone |
E | Shale |
Question 5 |


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 4 |
C | Fracture 8 and 9 |
D | Fracture 4 and 5 |
E | Fracture 1 and 2 |
Question 6 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/30-tmprlog.htm
A | 958 0ft |
B | 9540 ft |
C | 9600 ft |
D | 9640 ft |
E | 9500 ft |
Question 7 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Anhydrite |
B | Shale |
C | Limestone |
D | Dolomite |
E | 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 | At 2893 m |
B | At 2955 m |
C | At 3095 m |
D | At 2995 m |
E | At 3011 m |
Question 9 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | 30 degrees Northwest |
B | 40 degrees Southeast |
C | 150 degrees Northwest |
D | 50 degrees Southeast |
E | 60 degrees Southeast |
Question 10 |

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 | ~0.38 |
C | ~75 |
D | 0.0 |
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 11 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Tight oil |
B | Inaccuracies in measurements due to mud infiltration |
C | Signal interference or poor tool calibration |
D | Borehole collapse |
E | Poor tool pads in the well |
Question 12 |

A | At around 2180 m of depth |
B | At around 2145m of depth |
C | At around 2110 m of depth |
D | At around 2102 m of depth |
E | At around 2158 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 | Prograding marine shelf |
B | Slope channel deposit |
C | Channel point bar deposit |
D | Transgressive marine shelf |
E | Interbeds of coal and sand |
Question 14 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Dolomite |
B | Carbonaceous sandstone |
C | Dolomite with clay interbeds |
D | Limestone with sand interbeds |
E | Clean sand |
Question 15 |

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 | AT90 (dashed red line) |
C | AT10 (black line) |
D | It is difficult to determine with the given log. |
Question 16 |

A | Natural gas |
B | Low density bitumen |
C | Fresh water |
D | Oil (petroleum) |
E | Brine water |
Question 17 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2090 m (+/- 5m) |
B | 2077 m (+/- 5m) |
C | 2057 m (+/- 5m) |
D | 2047 m (+/- 5m) |
E | 2047 m (+/- 5m) |
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 1067 m |
B | At 1046.5 m |
C | At 1079 m |
D | At 1027 m |
E | At 1023 m |
Question 19 |

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 | Bedding contacts |
C | Coal seams |
D | Effective porosity |
E | Hydrocarbon saturated zones |
F | Fractures |
Question 20 |

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

A | Just above position II |
B | At position III |
C | At position I |
D | Just above position I |
E | Just below position II |
Question 23 |

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 9600 ft. |
D | From KB down to 9500 ft. |
Question 24 |

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 4 and 5 |
C | Fracture 3, 8 and 9 |
D | Fracture 5 and 6 |
E | Fracture 4, 6 and 7 |
Question 25 |

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

A | Coal |
B | Shale |
C | Clean limestone |
D | Sandstone |
E | Interbedded clean sandstone and 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 | 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 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 28 |

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

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1042 m and ~1043 m |
B | Between ~1066 m and ~1071 m |
C | Between ~1025 m and ~1028 m |
D | Between ~1066 m and ~1078 m |
E | Between ~1070 m and ~1078 m |
Question 30 |

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 31 |

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 | At 3075 m |
D | Between 2970 m and 3075 m |
E | Between 2945 m and 2970 m |
Question 32 |

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 | Water invaded zone |
C | Water saturated zone |
D | Oil saturated zone |
E | Coal seam regions |
Question 33 |

A | At around 2102 m of depth |
B | At around 2105 m of depth |
C | At around 2158 m of depth |
D | At around 2177 m of depth |
E | At around 2110 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 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/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 1078 m |
E | Between 1066 m and 1071 m |
Question 36 |

Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1066 m and ~1078 m |
B | Between ~1025 m and ~1028 m |
C | Between ~1070 m and ~1078 m |
D | Between ~1066 m and ~1071 m |
E | Between ~1042 m and ~1043 m |
Question 37 |

Image credit: United States Geological Survey, online at USGS database
A | Intentionally changed the drill bit |
B | Soft lithological facies |
C | High pressure due to increased in depth |
D | Borehole collapse |
E | Drilling mud infiltration |
Question 38 |

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 | Coal bearing formation |
C | Sandstone formation |
D | Presence of hydrocarbons |
E | High concentration of gas ("gas effect") |
Question 39 |

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 | Anhydrite |
D | Shale |
E | Limestone |
F | Argillaceous limestone |
Question 40 |

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 | Shale interbeded sandstone |
C | Gas-bearing sandstone |
D | Gas-bearing calcite |
E | Shaly sandstone |
F | Gas-bearing dolomite |
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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.