Structure and evolution of the active fold and thrust belt of southwestern Taiwan using GPS geodesy /
2-dimensional wedge models.
| Main Author: | |
|---|---|
| Format: | Thesis eBook |
| Language: | English |
| Published: |
[Place of publication not identified] :
[publisher not identified] ;
1999.
|
| Subjects: | |
| Online Access: | Link to OAKTrust copy |
| Summary: | 2-dimensional wedge models. across it. As a result, the actual pattern of active in this area include: 1) the Yuching syncline Although there is a general decrease in motion from appears to be a nearly vertical oblique transverse between the Western Foothills and the Slate Belt, complex motions across the strike of this region. deformation is very different from that predicted by displacement ( 1+ cm/-yr) across the Michih transverse east to west, significant variations occur across fault with a significant degree of left-lateral motion fault, 3) from north to south, a dramatic change in fault, and 4) the Tulungwan fault, a bounding fault investigated the current deformation rates and local is neither halogenous, nor distributed evenly across its axis, 2) a significant regional transfer of its surface. The structures that appear to be the most kinematic relationships for the southern region of the local structures. Deformation across southern Taiwan Taiwan fold-thrust belt. The GPS measurements suggest that accommodates 1.75 cm/-yr of displacement across the width of the deformation front of the fold and thrust belt which is accentuated across the Michih Using GPS and published geologic data, we have crographics. |
|---|---|
| Item Description: | "Major subject: Geology". Vita. |
| Physical Description: | v, 59 leaves : illustrations, maps ; 28 cm. Also available online. |
| Bibliography: | Includes bibliographical references (leaves 54-56). |