The recent convergence on the NW Borneo Wedge-a crustal-scale gravity gliding evidenced from GPS
The existence of an active compression on the frontal fold-and-thrust belt (FTB) of the NW Borneo Wedge is a long debate. Because of the absence of seismicity, the frontal FTB is traditionally considered as inactive and generally attributed to the thin-skin gravity-driven Baram Basin. However, there...
Saved in:
| Main Authors: | , , , , |
|---|---|
| 其他作者: | |
| 格式: | Article |
| 語言: | English |
| 出版: |
2020
|
| 主題: | |
| 在線閱讀: | https://hdl.handle.net/10356/144213 |
| 標簽: |
添加標簽
沒有標簽, 成為第一個標記此記錄!
|