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 | At around 2102 m of depth |
B | At around 2110 m of depth |
C | At around 2180 m of depth |
D | At around 2145m of depth |
E | At around 2158 m of depth |
Question 2 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Tight oil |
B | Poor tool pads in the well |
C | Inaccuracies in measurements due to mud infiltration |
D | Signal interference or poor tool calibration |
E | Borehole collapse |
Question 3 |
A | Coal |
B | Low density shale |
C | Organic rich black shale |
D | Heavy metals |
E | Shaly sandstone |
Question 4 |
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 | Fractures |
D | Effective porosity |
E | Bedding contacts |
F | Lithological contacts |
Question 5 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Carbonaceous sandstone |
B | Clean sand |
C | Limestone with sand interbeds |
D | Dolomite with clay interbeds |
E | Dolomite |
Question 6 |
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 1023 m |
C | At 1067 m |
D | At 1046.5 m |
E | At 1027 m |
Question 7 |
A | At around 2102 m of depth |
B | At around 2110 m of depth |
C | At around 2177 m of depth |
D | At around 2158 m of depth |
E | At around 2105 m of depth |
Question 8 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/18-shalegas.htm
A | Between 1212.5 m to 1223.5 m |
B | Between 1209.5 m to 1211.5 m |
C | Between 1203 m to 1239.5 m |
D | Between 1211.5 m to 1239.5 m |
Question 9 |
Image credit: United States Geological Survey, online at USGS database
A | Borehole collapse |
B | Soft lithological facies |
C | High pressure due to increased in depth |
D | Drilling mud infiltration |
E | Intentionally changed the drill bit |
Question 10 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-whatisalog.htm
A | Coal bearing formation |
B | Sandstone formation |
C | High porosity formation |
D | Presence of hydrocarbons |
E | High concentration of gas ("gas effect") |
Question 11 |
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 | 50 degrees Southeast |
D | 150 degrees Northwest |
E | 60 degrees Southeast |
Question 12 |
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 | 0.0 |
C | ~75 |
D | ~0.38 |
E | ~1.0 |
Net sand interval = 3075 m - 3000 m = 75 m (read off the GR curve)
Hence, net:gross = 75 m/75 m = 1.0
Question 13 |
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 | Shaly sandstone |
C | Limy dolomite |
D | Dolomitic pelmicrite |
E | Shale |
Question 14 |
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 | AT30 (dashed blue line) |
C | It is difficult to determine with the given log. |
D | AT90 (dashed red line) |
Question 15 |
A | Fresh water |
B | Low density bitumen |
C | Brine water |
D | Natural gas |
E | Oil (petroleum) |
Question 16 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2047 m (+/- 5m) |
B | 2057 m (+/- 5m) |
C | 2077 m (+/- 5m) |
D | 2047 m (+/- 5m) |
E | 2090 m (+/- 5m) |
Question 17 |
A | Shale |
B | Clean limestone |
C | Interbedded clean sandstone and shale |
D | Sandstone |
E | Coal |
Question 18 |
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 451 m of depth |
C | Around 465 m of depth |
D | Around 422 m of depth |
E | Around 460 m of depth |
Question 19 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1066 m and ~1078 m |
B | Between ~1066 m and ~1071 m |
C | Between ~1070 m and ~1078 m |
D | Between ~1042 m and ~1043 m |
E | Between ~1025 m and ~1028 m |
Question 20 |
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 | Gas saturated zone |
C | Water invaded zone |
D | Oil saturated zone |
E | Coal seam regions |
Question 21 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Calcite |
B | Limestone |
C | Shale |
D | Anhydrite |
E | Dolomite |
F | Argillaceous limestone |
Question 22 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1042 m and ~1043 m |
B | Between ~1066 m and ~1078 m |
C | Between ~1070 m and ~1078 m |
D | Between ~1066 m and ~1071 m |
E | Between ~1025 m and ~1028 m |
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 2995 m |
B | At 3011 m |
C | At 2893 m |
D | At 3095 m |
E | At 2955 m |
Question 24 |
A | Just above position I |
B | At position III |
C | At position I |
D | Just below position II |
E | Just above position II |
Question 25 |
A | Trangessive marine shelf |
B | Braided channel |
C | Slope channel |
D | Super-fan depositional lobes |
E | Prograding delta |
F | Channel-point bar |
Question 26 |
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 | Gas-bearing calcite |
C | Gas-bearing sandstone |
D | Gas-bearing dolomite |
E | Shaly sandstone |
F | Shale interbeded sandstone |
Question 27 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Caprock |
B | Mudstone |
C | Seal |
D | Shale |
E | Sandtone |
Question 28 |
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 | Interbeds of coal and sand |
D | Transgressive marine shelf |
E | Prograding marine shelf |
Question 29 |
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 1047 m and 1060 m |
D | Between 1071 m and 1078 m |
E | Between 1066 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 | At 3075 m |
B | Between 2970 m and 3075 m |
C | Between 3075 m and 3085 m |
D | Between 2890 m and 2895 m |
E | Between 2945 m and 2970 m |
Question 31 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Anhydrite |
B | Glauconitic Sandstone |
C | Limestone |
D | Sandstone |
E | Dolomite |
Question 32 |
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 | Between 9500 ft and 9600 ft. |
D | From KB down to 9600 ft. |
Question 33 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | ~ 0.24 |
B | ~ 0.36 |
C | ~ 0.18 |
D | ~ 0.27 |
E | ~ 0.48 |
Question 34 |
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 | Fracture 5 and 6 |
C | It is impossible to determine. |
D | Fracture 3, 8 and 9 |
E | Fracture 4 and 5 |
Question 35 |
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 , 457 m , 470 m and 475 m |
B | At around 416 m , 451 m , 464 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 414 m , 451 m , 457 m , 464 m and 475 m |
Question 36 |
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 | Calcite |
C | Anhydrite |
D | Shale |
E | Argillaceous limestone |
F | Dolomite |
Question 37 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Sandstone |
B | Dolomite |
C | Anhydrite |
D | Shale |
E | Limestone |
Question 38 |
A | Heavy metals |
B | Glauconitic sandstone |
C | Organic rich black shale |
D | Interbeds of clean sand with shale |
E | Gas bearing sandstone |
Question 39 |
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 | 9600 ft |
C | 9500 ft |
D | 958 0ft |
E | 9540 ft |
Question 40 |
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 4 and 5 |
D | Fracture 8 and 9 |
E | Fracture 4 |
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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.