Difference between revisions of "Magnetotellurics case history: Precambrian overthrust (Northwestern Colorado)"
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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- | + | | frompg = 16-10 |
− | | topg = 16- | + | | 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. |
− | 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> |
==Survey results== | ==Survey results== | ||
− | [[file:applying-magnetotellurics_fig16-7.png|thumb| | + | [[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 />]] |
− | 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. | + | 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. |
[[:file:applying-magnetotellurics_fig16-7.png|Figure 1]] 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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* 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]] |
− | A very detailed subsurface structural map could be obtained in this area using a 3-D grid, controlled-source MT survey depicting the Precambrian | + | 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. |
==See also== | ==See also== | ||
+ | * [[Magnetotellurics]] | ||
* [[Magnetotellurics survey measurements]] | * [[Magnetotellurics survey measurements]] | ||
− | * [[ | + | * [[Magnetotelluric data acquisition]] |
− | * [[ | + | * [[Magnetotellurics case history: frontier basin analysis (Amazon Basin, Colombia)]] |
− | * [[ | + | * [[Magnetotellurics case history: rugged carbonate terrain (Highlands of Papua New Guinea)]] |
− | * [[ | + | * [[Magnetotellurics case history: volcanic terrain (Columbia River Plateau)]] |
==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]] |
Latest revision as of 15:13, 31 January 2022
Exploring for Oil and Gas Traps | |
Series | Treatise in Petroleum Geology |
---|---|
Part | Predicting the occurrence of oil and gas traps |
Chapter | Applying magnetotellurics |
Author | Arnie Ostrander |
Link | Web page |
Store | AAPG Store |
Magnetotellurics (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, low-conductivity) rocks overlie low-velocity (low-resistivity, high-conductivity) sediments.
The Precambrian overthrust in the Bear Springs area of northwestern Colorado is an example.[1]
Survey results[edit]
The MT station near the drill hole (see diagram 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.
Figure 1 is an 11-station MT profile across the thrust.
Structural details[edit]
These data provide the following structural details:
- Thickness of Quaternary and Tertiary cover
- Thickness of Precambrian thrust sheet
- Thinning of Cretaceous sediments to the south
- Depth to top of Paleozoic sediments
- No differentiation between Paleozoic and basement
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.
See also[edit]
- Magnetotellurics
- Magnetotellurics survey measurements
- Magnetotelluric data acquisition
- Magnetotellurics case history: frontier basin analysis (Amazon Basin, Colombia)
- Magnetotellurics case history: rugged carbonate terrain (Highlands of Papua New Guinea)
- Magnetotellurics case history: volcanic terrain (Columbia River Plateau)