Skip to main navigation
Skip to search
Skip to main content
National Central University Home
Help & FAQ
Link opens in a new tab
English
中文
Search content at National Central University
Home
Scholar Profiles
Research units
Projects
Research output
Datasets
Prizes
Activities
Press/Media
Impacts
Is Taiwan the result of arc-continent or arc-arc collision?
Shu Kun Hsu
, Jean Claude Sibuet
Department of Earth Sciences
Research output
:
Contribution to journal
›
Article
›
peer-review
99
Scopus citations
Overview
Fingerprint
Fingerprint
Dive into the research topics of 'Is Taiwan the result of arc-continent or arc-arc collision?'. Together they form a unique fingerprint.
Sort by
Weight
Alphabetically
Keyphrases
Taiwan
100%
Arc-arc Collision
100%
Luzon Arc
87%
Back-arc Basin
62%
Ryukyu Arc
50%
Okinawa Trough
25%
Ryukyu
12%
Ryukyu Subduction Zone
12%
Subduction
12%
Manila Trench
12%
Tainan
12%
Back-arc
12%
Coastal Range
12%
Suture Zone
12%
Eurasian Continental Margin
12%
Oblique Collision
12%
Late Miocene
12%
Truncation
12%
Geodetic Observations
12%
Longitudinal Valley
12%
Structural Features
12%
Earthquake Focal Mechanism
12%
Counterclockwise Rotation
12%
Collision Model
12%
Clockwise Rotation
12%
Mountain Building
12%
Paleo
12%
Indentation
12%
Early-Middle Miocene
12%
Southern Japan
12%
Eocene-Oligocene
12%
Earth and Planetary Sciences
Taiwan
100%
Arc-Arc Collision
100%
Continent
100%
Backarc Basin
62%
Trough
25%
Miocene
25%
Japan
12%
Focal Mechanism
12%
Subduction Zone
12%
Trench
12%
Continental Shelf
12%
Mountain Building
12%
Eocene
12%
Oligocene
12%