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...
| Hoofdauteurs: | , , , , |
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| Andere auteurs: | |
| Formaat: | Journal Article |
| Taal: | English |
| Gepubliceerd in: |
2020
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| Onderwerpen: | |
| Online toegang: | https://hdl.handle.net/10356/144213 |