Add to ORKGSummary. An elongated zone of positive magnetic anomalies extends from Northern Ireland to the Shetland Islands. From the total magnetization of the body causing the anomaly and published palaeomagnetic directions corresponding to a range of different possible ages for the remanent magnetiz-ation of this body, associated ranges of susceptibility are calculated. These ranges favour a Siluro-Devonian age as most plausible for the remanent magnetization. Such an age is compatible with the known geology of the area. Key words: magnetic anomalies, palaeomagnetic correlations
Red sedimentary rocks of the Stoer Group (991 My BP) were resampled through their stratigraphic rang...
Early attempts to utilize magnetic data to understand the volcanic and subvolcanic succession on the...
A series of discontinuous sediment sequences, of Plio/Pleistocene age, occur onshore around the sout...
both mineral isochron ages) comprise two of four major post-tectonic granitic complexes emplaced int...
Summary. Consideration of previous work and new data show a systematic distribution of the direction...
A total of 89 sites have been sampled for palaeomagnetic studies from the Caledonian ophiolite compl...
Palaeomagnetic data are presented from early Silurian (Upper Llandovery) lavas from the Tortworth Si...
A palaeomagnetic study of mid-Silurian (Wenlock) sediments of the Salrock Formation in NW Galway yie...
The Caerfai Series carries stable NRM which is probably of Lower Cambrian (otherwise pre-mid-Devonia...
Summary. Palaeomagnetic results are reported from 47 sites within the Borrowdale Volcanic Group of l...
Presented in this thesis are three studies which document the palaeomagnetic record of rocks forming...
Palaeomagnetic analysis of 222 specimens from a high-resolution Late Devensian Lateglacial sedimenta...
Single-station transfer functions linking the time variations of the vertical and horizontal compone...
Results of palaeomagnetic and rock magnetic studies are reported mainly for quartz porphyry collecte...
Palaeomagnetic work has been undertaken on four different rock types from the Cheviot Hills, Norther...
Red sedimentary rocks of the Stoer Group (991 My BP) were resampled through their stratigraphic rang...
Early attempts to utilize magnetic data to understand the volcanic and subvolcanic succession on the...
A series of discontinuous sediment sequences, of Plio/Pleistocene age, occur onshore around the sout...
both mineral isochron ages) comprise two of four major post-tectonic granitic complexes emplaced int...
Summary. Consideration of previous work and new data show a systematic distribution of the direction...
A total of 89 sites have been sampled for palaeomagnetic studies from the Caledonian ophiolite compl...
Palaeomagnetic data are presented from early Silurian (Upper Llandovery) lavas from the Tortworth Si...
A palaeomagnetic study of mid-Silurian (Wenlock) sediments of the Salrock Formation in NW Galway yie...
The Caerfai Series carries stable NRM which is probably of Lower Cambrian (otherwise pre-mid-Devonia...
Summary. Palaeomagnetic results are reported from 47 sites within the Borrowdale Volcanic Group of l...
Presented in this thesis are three studies which document the palaeomagnetic record of rocks forming...
Palaeomagnetic analysis of 222 specimens from a high-resolution Late Devensian Lateglacial sedimenta...
Single-station transfer functions linking the time variations of the vertical and horizontal compone...
Results of palaeomagnetic and rock magnetic studies are reported mainly for quartz porphyry collecte...
Palaeomagnetic work has been undertaken on four different rock types from the Cheviot Hills, Norther...
Red sedimentary rocks of the Stoer Group (991 My BP) were resampled through their stratigraphic rang...
Early attempts to utilize magnetic data to understand the volcanic and subvolcanic succession on the...
A series of discontinuous sediment sequences, of Plio/Pleistocene age, occur onshore around the sout...