The Tibetan Plateau, between the Kunlun Shan and the Himalayas, consists of terranes
accreted successively to Eurasia. The northernmost, the Songban Ganzi Terrane, was …

Vector magnetic field observations of the martian crust were acquired by the Mars Global
Surveyor (MGS) magnetic field experiment/electron reflectometer (MAG/ER) during the …

Many geological features of the Earth's lithosphere create variations in the Earth's magnetic
field that can be detected by satellites. The resulting magnetic anomaly maps can provide …

Observations of the Earth's magnetic field from low-Earth orbiting (LEO) satellites started
very early on, more than 50 years ago. Continuous such observations, relying on more …

Reliable global crustal field anomaly maps produced from magnetic measurements of the
CHAMP satellite mission now allow for quantitative geological studies of crustal structure …

The CHAMP magnetic field mission is providing highly reliable measurements from which
the global lithospheric magnetic field can be determined in unprecedented resolution and …

Using a simplified petrogenetic grid and a one-dimensional thermal model to compute the
evolution of the density of the crust with time, the contribution to the uplift of Tibet of …

Initial stages of compression produce periodic buckling of models analogous to a four‐layer
continental lithosphere. With further shortening, amplification of the buckles occurs by thrust …

Downward continuation is a very useful technique in the interpretation of potential field data.
It would enhance the short wavelength of the gravity anomalies or accentuate the details of …

The Tibetan plateau is associated with a pronounced satellite magnetic low. Forward
modeling of this anomaly demonstrates that the crust underlying the Tibetan plateau is …