Global models of the Earth's crust magnetic anomalies
Guofa Kang
Abstract
Guofa Kang
Abstract
The crust magnetic field,or lithospheric magnetic field,can be deduced by subtracting the main field,variation field and its induced counterpart from the total field.This field is essential to navigation,communication,geophysical exploration and many others.In this paper,the developments on data acquistion are briefly reviewed,including ground,marine,airborne,and satellite magnetic surveys,focusing on magnetic satellites,such as Oersted,CHAMP,etc.Global crust magnetic models are introduced.Finally,a brief prospect is given on future studies and applications of the crust magnetic models.
OpenAlex reports 7 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
The crust magnetic field,or lithospheric magnetic field,can be deduced by subtracting the main field,variation field and its induced counterpart from the total field.This field is essential to navigation,communication,geophysical exploration and many others.In this paper,the developments on data acquistion are briefly reviewed,including ground,marine,airborne,and satellite magnetic surveys,focusing on magnetic satellites,such as Oersted,CHAMP,etc.Global crust magnetic models are introduced.Finally,a brief prospect is given on future studies and applications of the crust magnetic models.
Key concepts: Crust, Geophysics, Geology, Lithosphere, Magnetic anomaly, Earth's magnetic field, Field (mathematics), L-shell