To achieve an improved over all under standing of the tectonics of Tai wan, an is land-wide magnetic survey, especially in the mostly inaccessible mountain ranges, was carried out from July 2003 to February 2004. In total, 6063 magnetic points were surveyed at an average spacing of 2 km. After data reductions, a new magnetic anomaly map of Taiwan was constructed. The map shows the range of magnetic anomalies mostly distributing between -400 to 400 nT. Anomalies in the southern part of Taiwan are much higher than those in the north whilst anomalies in the western plains area are higher than those of the mountain ranges
Not until magnetotellurics (MT) were conducted, was very much known about the deep electrical struct...
Succeeding to the previous geomagnetic surveys in 2000, the supplemental one was made at 45 stations...
[1] The Taiwan orogen has formed since the late Miocene by oblique collision between the Luzon Volca...
International audienceWe have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps,...
International audienceWe have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps,...
International audienceWe have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps,...
We have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps, shedding light on the...
Magnetic data provides basic information for geological and geophysical interpretation. In this stud...
AbstractThis study constructs an integrated magnetic anomaly map of Taiwan and its vicinity that com...
This special issue documents the status of various aspects on the geomagnetic research in Taiwan wit...
AbstractThis study constructs an integrated magnetic anomaly map of Taiwan and its vicinity that com...
In this paper, 3-component geomagnetic fields recorded by a fluxgate magnetometer are employed in ex...
The active Taiwan orogen is located between the Ryukyu subduction zone in the northeast and the Mani...
The active Taiwan orogen is located between the Ryukyu subduction zone in the northeast and the Mani...
An island-wide gravity in Taiwan was conducted by the Institute of Earth Sciences, Academia Sinica, ...
Not until magnetotellurics (MT) were conducted, was very much known about the deep electrical struct...
Succeeding to the previous geomagnetic surveys in 2000, the supplemental one was made at 45 stations...
[1] The Taiwan orogen has formed since the late Miocene by oblique collision between the Luzon Volca...
International audienceWe have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps,...
International audienceWe have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps,...
International audienceWe have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps,...
We have compiled new free-air gravity anomaly (FAA) and magnetic anomaly maps, shedding light on the...
Magnetic data provides basic information for geological and geophysical interpretation. In this stud...
AbstractThis study constructs an integrated magnetic anomaly map of Taiwan and its vicinity that com...
This special issue documents the status of various aspects on the geomagnetic research in Taiwan wit...
AbstractThis study constructs an integrated magnetic anomaly map of Taiwan and its vicinity that com...
In this paper, 3-component geomagnetic fields recorded by a fluxgate magnetometer are employed in ex...
The active Taiwan orogen is located between the Ryukyu subduction zone in the northeast and the Mani...
The active Taiwan orogen is located between the Ryukyu subduction zone in the northeast and the Mani...
An island-wide gravity in Taiwan was conducted by the Institute of Earth Sciences, Academia Sinica, ...
Not until magnetotellurics (MT) were conducted, was very much known about the deep electrical struct...
Succeeding to the previous geomagnetic surveys in 2000, the supplemental one was made at 45 stations...
[1] The Taiwan orogen has formed since the late Miocene by oblique collision between the Luzon Volca...