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/18-shalegas.htm
A | Water saturated zone |
B | Gas saturated zone |
C | Coal seam regions |
D | Oil saturated zone |
E | Water invaded zone |
Question 2 |
Image credit: United States Geological Survey, online at USGS database
A | Drilling mud infiltration |
B | Soft lithological facies |
C | Intentionally changed the drill bit |
D | High pressure due to increased in depth |
E | Borehole collapse |
Question 3 |
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 | ~ 0.36 |
C | ~ 0.27 |
D | ~ 0.18 |
E | ~ 0.24 |
Question 4 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Shaly sandstone |
B | Shale |
C | Limy dolomite |
D | Quartz arenite |
E | Dolomitic pelmicrite |
Question 5 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Between 1066 m and 1071 m |
B | Between 1047 m and 1060 m |
C | Between 1066 m and 1078 m |
D | Between 1049 m and 1055 m |
E | Between 1071 m and 1078 m |
Question 6 |
A | Shale |
B | Interbedded clean sandstone and shale |
C | Coal |
D | Clean limestone |
E | Sandstone |
Question 7 |
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 | Anhydrite |
E | Argillaceous dolomite |
F | Shale |
Question 8 |
A | Just above position I |
B | At position III |
C | At position I |
D | Just below position II |
E | Just above position II |
Question 9 |
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 ~1070 m and ~1078 m |
D | Between ~1066 m and ~1078 m |
E | Between ~1025 m and ~1028 m |
Question 10 |
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 | ~0.38 |
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
Original at: https://www.spec2000.net/07-eslog.htm
A | Around 422 m of depth |
B | Around 460 m of depth |
C | Around 470 m of depth |
D | Around 451 m of depth |
E | Around 465 m of depth |
Question 12 |
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 | Between 9500 ft and 9600 ft. |
D | From KB down to 9500 ft. |
Question 13 |
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 | Presence of hydrocarbons |
C | High porosity formation |
D | High concentration of gas ("gas effect") |
E | Sandstone formation |
Question 14 |
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 4 |
C | Fracture 7 |
D | Fracture 8 and 9 |
E | Fracture 1 and 2 |
Question 15 |
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 1209.5 m to 1211.5 m |
C | Between 1203 m to 1239.5 m |
D | Between 1212.5 m to 1223.5 m |
Question 16 |
A | Heavy metals |
B | Low density shale |
C | Shaly sandstone |
D | Organic rich black shale |
E | Coal |
Question 17 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | 2057 m (+/- 5m) |
B | 2077 m (+/- 5m) |
C | 2047 m (+/- 5m) |
D | 2090 m (+/- 5m) |
E | 2047 m (+/- 5m) |
Question 18 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Mudstone |
B | Caprock |
C | Seal |
D | Shale |
E | Sandtone |
Question 19 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/01-crainsrules.htm
A | Dolomite with clay interbeds |
B | Clean sand |
C | Dolomite |
D | Carbonaceous sandstone |
E | Limestone with sand interbeds |
Question 20 |
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 1079 m |
C | At 1027 m |
D | At 1046.5 m |
E | At 1023 m |
Question 21 |
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 | AT10 (black line) |
C | It is difficult to determine with the given log. |
D | AT90 (dashed red line) |
Question 22 |
A | Trangessive marine shelf |
B | Prograding delta |
C | Slope channel |
D | Braided channel |
E | Channel-point bar |
F | Super-fan depositional lobes |
Question 23 |
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 | 9500 ft |
E | 958 0ft |
Question 24 |
A | At around 2102 m of depth |
B | At around 2105 m of depth |
C | At around 2177 m of depth |
D | At around 2158 m of depth |
E | At around 2110 m of depth |
Question 25 |
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 5 and 6 |
C | It is impossible to determine. |
D | Fracture 3, 8 and 9 |
E | Fracture 4, 6 and 7 |
Question 26 |
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 | Limestone |
C | Shale |
D | Calcite |
E | Dolomite |
F | Anhydrite |
Question 27 |
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 dolomite |
C | Gas-bearing sandstone |
D | Shale interbeded sandstone |
E | Gas-bearing calcite |
F | Shaly sandstone |
Question 28 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Limestone |
B | Sandstone |
C | Dolomite |
D | Anhydrite |
E | Glauconitic Sandstone |
Question 29 |
A | At around 2145m of depth |
B | At around 2110 m of depth |
C | At around 2158 m of depth |
D | At around 2102 m of depth |
E | At around 2180 m of depth |
Question 30 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | Between 2970 m and 3075 m |
B | Between 2945 m and 2970 m |
C | Between 3075 m and 3085 m |
D | At 3075 m |
E | Between 2890 m and 2895 m |
Question 31 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Shale |
B | Limestone |
C | Dolomite |
D | Sandstone |
E | Anhydrite |
Question 32 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | Coal seams |
B | Effective porosity |
C | Bedding contacts |
D | Fractures |
E | Lithological contacts |
F | Hydrocarbon saturated zones |
Question 33 |
A | Oil (petroleum) |
B | Low density bitumen |
C | Natural gas |
D | Brine water |
E | Fresh water |
Question 34 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/22-fracloc5.htm
A | 150 degrees Northwest |
B | 30 degrees Northwest |
C | 40 degrees Southeast |
D | 60 degrees Southeast |
E | 50 degrees Southeast |
Question 35 |
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 | Transgressive marine shelf |
C | Slope channel deposit |
D | Channel point bar deposit |
E | Interbeds of coal and sand |
Question 36 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
Original at: https://www.spec2000.net/13-lithvisual.htm
A | At 3095 m |
B | At 2893 m |
C | At 2955 m |
D | At 2995 m |
E | At 3011 m |
Question 37 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Poor tool pads in the well |
B | Inaccuracies in measurements due to mud infiltration |
C | Tight oil |
D | Borehole collapse |
E | Signal interference or poor tool calibration |
Question 38 |
Image credit: Crain's Petrophysical Handbook, online at https://www.spec2000.net
A | Between ~1066 m and ~1071 m |
B | Between ~1042 m and ~1043 m |
C | Between ~1070 m and ~1078 m |
D | Between ~1025 m and ~1028 m |
E | Between ~1066 m and ~1078 m |
Question 39 |
A | Interbeds of clean sand with shale |
B | Heavy metals |
C | Glauconitic sandstone |
D | Organic rich black shale |
E | Gas bearing sandstone |
Question 40 |
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 412 m , 414 m , 422 m , 470 m and 475 m |
C | At around 414 m , 451 m , 457 m , 464 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 |
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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.