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Magnetotelluric survey case history: volcanic terrain (Columbia River Plateau) (view source)
Revision as of 15:54, 28 May 2014
, 15:54, 28 May 2014→Structural details
These data provided the following structural details:
These data provided the following structural details:
* Considerable variation in the thickness of the volcanics
* Considerable variation in the thickness of the [[volcanics]]
* Considerable variation in the depth to top of basement
* Considerable variation in the depth to top of [[basement]]
* Basalts thin to the east
* [[Basalt]]s thin to the east
* Sediments thin to east and eventually disappear
* Sediments thin to east and eventually disappear
* Basement resistivities are an order-of-magnitude higher on the east end of the profile
* Basement [[Resistivity|resistivities]] are an order-of-magnitude higher on the east end of the profile
[[Magnetotelluric data acquisition#Controlled-source surveys|Controlled-source]] MT data could provide 3-D imaging of individual prospects.
[[Magnetotelluric data acquisition#Controlled-source surveys|Controlled-source]] MT data could provide 3-D imaging of individual prospects.