Potential geological risks from mud diatremes in the orogen regime of Southwestern Taiwan
Abstract In orogenic regions, faults from plate collisions are the main cause of earthquakes. Recent studies have found that underground mudstone structures and intrusions can accompany fault development, causing surface deformation and geological hazards. In southwestern Taiwan, geodetic evidence h...
Saved in:
| Main Authors: | Hung-Yu Wu, Hou-Chun Liu, Li-Cheng Kao, Kuo-En Ching, Chien-Chih Chen, Chen-Feng You, Te-Cheng Yi, Yan-Hong Chen, Bo-Lin Wu, Chun-Jung Chen |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Nature Portfolio
2025-03-01
|
| Series: | Scientific Reports |
| Online Access: | https://doi.org/10.1038/s41598-025-91915-y |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Pyrrhotite as a tracer for denudation of the Taiwan orogen
by: Chorng‐Shern Horng, et al.
Published: (2012-08-01) -
Bayesian inversion for the crustal anisotropy of the Taiwan foreland basin: syn- and pre-orogenic deformation
by: Cheng-Chien Peng, et al.
Published: (2025-07-01) -
Systematic correlations of the earthquake frequency‐magnitude distribution with the deformation and mechanical regimes in the Taiwan orogen
by: Yen‐Ling Chen, et al.
Published: (2016-05-01) -
Fast report: Coseismic source model of the January 2025 Mw 6.1 Dapu earthquake from geodetic data and its implications for seismogenic structures in Southwestern Taiwan
by: Yogendra Sharma, et al.
Published: (2025-04-01) -
Unraveling the role played by a buried mud diapir: alternative model for 2016 Mw 6.4 MeiNong earthquake in southwestern Taiwan
by: Geng-Pei Lin, et al.
Published: (2024-04-01)