Skip to main content

Index Geophysics

An anomaly of the upper mantle below the Rhine Graben, studied by the inductive response of natural electromagnetic fields

Item

Title (Dublin Core)

en-US An anomaly of the upper mantle below the Rhine Graben, studied by the inductive response of natural electromagnetic fields

Description (Dublin Core)

en-US The methods of Magnetotellurics (MT) and Geomagnetic Deep Sounding (GOS) have been applied to study the electromagnetic response of the rift structure of the Rhine Graben. The measurements at 17 MT and 7 GOS stations were carried out along a profile running perpendicular across the Graben. Fourier analysis and numerical filters were tried for separation of the frequencies and a least squares technique was applied for data reduction. The thus gained transfer functions can be explained well by two-dimensional models under the following assumption: a well conducting layer at the depth between about 80 and 100 km exists at distances 50 km West and 100 km East of the Rhine Graben. Immediately below the Graben, however, a zone of similar good conductivity lies between about 25 and 45 km depth. The lateral extension of this zone is only some tens of km from the Graben's edges.
          ARK: https://n2t.net/ark:/88439/y032853
Permalink: https://geophysicsjournal.com/article/276
 

Creator (Dublin Core)

Reitmayr, G.

Subject (Dublin Core)

en-US Electromagnetic induction
en-US Magnetotellurics
en-US Geomagnetic deep sounding
en-US Electrical conductivity
en-US Upper mantle
en-US Rift structure
en-US Rhine graben
en-US Solid Earth

Publisher (Dublin Core)

en-US Journal of Geophysics

Date (Dublin Core)

1975-01-03

Type (Dublin Core)

info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US Peer-reviewed Article

Format (Dublin Core)

application/pdf

Identifier (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/276

Source (Dublin Core)

en-US Journal of Geophysics; Vol 41 No 1 (1975): Journal of Geophysics; 651-658
2643-2986
2643-9271

Language (Dublin Core)

eng

Relation (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/276/233