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| | part = Predicting the occurrence of oil and gas traps | | | part = Predicting the occurrence of oil and gas traps |
| | chapter = Applying magnetotellurics | | | chapter = Applying magnetotellurics |
− | | frompg = 16-1 | + | | frompg = 16-10 |
− | | topg = 16-12 | + | | topg = 16-10 |
| | author = Arnie Ostrander | | | author = Arnie Ostrander |
| | link = http://archives.datapages.com/data/specpubs/beaumont/ch16/ch16.htm | | | link = http://archives.datapages.com/data/specpubs/beaumont/ch16/ch16.htm |
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| | isbn = 0-89181-602-X | | | isbn = 0-89181-602-X |
| }} | | }} |
− | MT can be used in an overthrust environment to delineate conductive sediments beneath a resistive thrust plate. It is often difficult to acquire good-quality seismic data in an overthrust area where high-velocity (high-resistivity) rocks overlie low-velocity (low-resistivity) sediments. | + | Magnetotellurics (MT) can be used in an [[overthrust]] environment to delineate [[Wikipedia:Electrical resistivity and conductivity|conductive]] sediments beneath a [[Wikipedia:Electrical resistivity and conductivity|resistive]] thrust plate. It is often difficult to acquire good-quality [[seismic data]] in an overthrust area where high-velocity (high-resistivity, low-conductivity) rocks overlie low-velocity (low-resistivity, high-conductivity) sediments. |
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− | The Precambrian overthrust in the Bear Springs area of northwestern Colorado is an example.<ref name=ch16r5>Mills, A., 1994, Zephyr Geophysical Services, personal communication.</ref> | + | The [[Precambrian]] overthrust in the Bear Springs area of northwestern Colorado is an example.<ref name=ch16r5>Mills, A., 1994, Zephyr Geophysical Services, personal communication.</ref> |
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| ==Survey results== | | ==Survey results== |
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− | [[file:applying-magnetotellurics_fig16-7.png|thumb|{{figure number|1}}An 11-station MT profile across the thrust. Drafted from data from Mills.<ref name=ch16r5 />]] | + | [[file:applying-magnetotellurics_fig16-7.png|thumb|500px|{{figure number|1}}An 11-station MT profile across the thrust. Drafted from data from Mills.<ref name=ch16r5 />]] |
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− | The MT station near the drill hole (see diagram below) shows a thin, near-surface conductor on top of the resistive Precambrian thrust sheet. This is a wedge of Quaternary and [[Tertiary]] sediments. Beneath the thrust, a thick conductive section of Cretaceous sediments is observed. | + | The MT station near the drill hole (see diagram [[:file:applying-magnetotellurics_fig16-7.png|Figure 1]]) shows a thin, near-surface conductor on top of the resistive Precambrian thrust sheet. This is a wedge of [[Quaternary]] and [[Tertiary]] sediments. Beneath the thrust, a thick conductive section of [[Cretaceous]] sediments is observed. |
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− | [[:file:applying-magnetotellurics_fig16-7.png|Figure 1]] below is an 11-station MT profile across the thrust. | + | [[:file:applying-magnetotellurics_fig16-7.png|Figure 1]] is an 11-station MT profile across the thrust. |
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| ==Structural details== | | ==Structural details== |
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| * Thickness of Precambrian thrust sheet | | * Thickness of Precambrian thrust sheet |
| * Thinning of Cretaceous sediments to the south | | * Thinning of Cretaceous sediments to the south |
− | * Depth to top of Paleozoic sediments | + | * Depth to top of [[Paleozoic]] sediments |
− | * No differentiation between Paleozoic and basement | + | * No differentiation between Paleozoic and [[basement]] |
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− | A very detailed subsurface structural map could be obtained in this area using a 3-D grid, controlled-source MT survey depicting the Precambrian/Cretaceous thrust contact and the top of the Paleozoic section. | + | A very detailed subsurface structural map could be obtained in this area using a 3-D grid, controlled-source MT survey depicting the Precambrian-Cretaceous thrust contact and the top of the Paleozoic section. |
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| ==See also== | | ==See also== |
− | * [[What is magnetotellurics?]] | + | * [[Magnetotellurics]] |
− | * [[What does an MT survey measure?]] | + | * [[Magnetotellurics survey measurements]] |
− | * [[How are MT data acquired?]] | + | * [[Magnetotelluric data acquisition]] |
− | * [[Case history: frontier basin analysis (Amazon Basin, Colombia)]] | + | * [[Magnetotellurics case history: frontier basin analysis (Amazon Basin, Colombia)]] |
− | * [[Case history: rugged carbonate terrain (Highlands of Papua New Guinea)]] | + | * [[Magnetotellurics case history: rugged carbonate terrain (Highlands of Papua New Guinea)]] |
− | * [[Case history: volcanic terrain (Columbia River Plateau)]] | + | * [[Magnetotellurics case history: volcanic terrain (Columbia River Plateau)]] |
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| ==References== | | ==References== |
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| [[Category:Predicting the occurrence of oil and gas traps]] | | [[Category:Predicting the occurrence of oil and gas traps]] |
| [[Category:Applying magnetotellurics]] | | [[Category:Applying magnetotellurics]] |
| + | [[Category:Treatise Handbook 3]] |