Precision of source depth estimates made from ‘thin dyke’ magnetic anomalies

2002 ◽  
Author(s):  
Clive Foss
Keyword(s):  
Magnetic Anomalies ◽  
Source Depth

Modelling Source Depth and Possible Origin of Magnetic Anomalies Associated with the Yallalie Impact Structure, Perth Basin, Western Australia

2006 ◽  
Vol 37 (2) ◽  
pp. 191-196 ◽  
Author(s):  
P.J. Hawke ◽  
A.J. Buckingham ◽  
M.C. Dentith
Keyword(s):  
Western Australia ◽  
Magnetic Anomalies ◽  
Impact Structure ◽  
Source Depth

Large magnetic anomalies over Russia revealed by balloon data

2004 ◽  
Vol 6 (6) ◽  
pp. 457-460
Author(s):  
K. A. Nazarova ◽  
T. Sabaka ◽  
Yu. Tsvetkov ◽  
J. Heirtzler
Keyword(s):  
Magnetic Anomalies

Magnetic anomalies, chemical and magnetic properties at wide temperature range (15–1000 K) in LiSrxFe5-xO8 (x = 0, 0.025, 0.05)

2021 ◽  
Vol 859 ◽  
pp. 158290
Author(s):  
S. Udhayakumar ◽  
G. Jagadish Kumar ◽  
E. Senthil Kumar ◽  
M. Navaneethan ◽  
K. Kamala Bharathi
Keyword(s):  
Magnetic Properties ◽  
Wide Temperature Range ◽  
Magnetic Anomalies ◽  
Temperature Range

Metamorphism in the Troodos ophiolite: implications for marine magnetic anomalies

Nature ◽  
1980 ◽  
Vol 285 (5766) ◽  
pp. 563-564 ◽  
Author(s):  
Suzanne Beske-Diehl ◽  
Subir K. Banerjee
Keyword(s):  
Magnetic Anomalies ◽  
Troodos Ophiolite ◽  
Marine Magnetic Anomalies

Intrusives, Extrusives and Linear Magnetic Anomalies

2007 ◽  
Vol 23 (1) ◽  
pp. 1-13 ◽  
Author(s):  
N. D. Watkins ◽  
A. Richardson
Keyword(s):  
Magnetic Anomalies

Large scale magnetic anomalies over western Canada and the Arctic: a discussion

1976 ◽  
Vol 13 (6) ◽  
pp. 790-802 ◽  
Author(s):  
R. L. Coles ◽  
G. V. Haines ◽  
W. Hannaford
Keyword(s):  
Magnetic Field ◽  
Large Scale ◽  
Elevated Temperatures ◽  
Magnetic Anomalies ◽  
The Arctic ◽  
Evolutionary Development ◽  
Magnetic Feature ◽  
Western Canada ◽  
Arctic Regions ◽  
The Magnetic Field

A contoured map of vertical magnetic field residuals (relative to the IGRF) over western Canada and adjacent Arctic regions has been produced by amalgamating new data with those from previous surveys. The measurements were made at altitudes between 3.5 and 5.5 km above sea level. The map shows the form of the magnetic field within the waveband 30 to 5000 km. A magnetic feature of several thousand kilometres wavelength dominates the map, and is probably due in major part to sources in the earth's core. Superimposed on this are several groups of anomalies which contain wavelengths of the order of a thousand kilometres. The patterns of the short wavelength anomalies provide a broad view of major structures and indicate several regimes of distinctive evolutionary development. Enhancement of viscous magnetization at elevated temperatures may account for the concentration of intense anomalies observed near the western edge of the craton.

scholarly journals Correction to ‘Theory of electrokinetic-magnetic anomalies in a faulted half-space’

1981 ◽  
Vol 86 (B10) ◽  
pp. 9585-9588 ◽  
Author(s):  
D. V. Fitterman
Keyword(s):  
Half Space ◽  
Magnetic Anomalies

Phase separation as origin of the magnetic anomalies in La0.85Sr0.15CoO3

2001 ◽  
Vol 89 (10) ◽  
pp. 5606-5609 ◽  
Author(s):  
J. Mira ◽  
J. Rivas ◽  
G. Baio ◽  
G. Barucca ◽  
R. Caciuffo ◽  
...  
Keyword(s):  
Phase Separation ◽  
Magnetic Anomalies

Magnetic anomalies and basalt composition in the Juan de Fuca-Gorda Ridge area

1976 ◽  
Vol 33 (2) ◽  
pp. 185-207 ◽  
Author(s):  
P.R. Vogt ◽  
G.R. Byerly
Keyword(s):  
Magnetic Anomalies ◽  
Juan De Fuca ◽  
Ridge Area ◽  
Gorda Ridge ◽  
Basalt Composition
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