Wen-Han LoNational Dong Hwa University · Department of Natural Resources and Environmental Studies
Wen-Han Lo
Master of Science
About
6
Publications
480
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Introduction
Wen-Han currently works at the National Dong Hwa University, Taiwan. Wen-Han does research in petrology, geochemistry, and geochronology on metamorphic rocks. Ph.D. project: P-T-t paths and geochemical characteristics of garnet-
bearing metamorphic rocks in the eastern Central Range, Taiwan.
Additional affiliations
July 2015 - August 2018
National Dong Hwa University
Position
- Master's Student
Publications
Publications (6)
Glaucophane-bearing metaplagiogranite occurs among the high-pressure (HP) metamorphic rock types poorly exposed in the Yuli belt. This lithologic association has been interpreted as scattered fragments of a metamorphosed ophiolite. Through field and petrographic investigations, we have identified several types of metaplagiogranite in the Chinshuich...
The Yuli belt is a high-pressure (HP) metamorphic terrane located at the convergent boundary between the Eurasia plate and the Philippine Sea plate. It is mainly composed of metapelites with minor serpentinites and metaigneous rocks. In the northern part of the belt, HP metamorphism is by far only reported on the omphacite-bearing metagabbro in ser...
Ultramafic rocks are important for deciphering geodynamic evolution of orogenic belts. The Yuli metamorphic belt has been the most crucial topic in regional tectonics of eastern Taiwan in recent years (Tsai et al., 2013; Brown et al., 2015; Keyser et al., 2016; Chen et al., 2017). Four major serpentinite-bearing tectonic blocks crop out in Fengtien...
Serpentinization of ultramafic rock is a key process that controls the geodynamic evolution of orogenic belts. The Yuli metamorphic belt has been the focus of regional tectonic studies in recent years (Tsai et al., 2013; Brown et al., 2015; Keyser et al., 2016; Chen et al., 2017). Four major serpentinite bodies crop out in Fengtien, Wanjung, Juisui...
Serpentinization of ultramafic rock is a key process that controls the geodynamic evolution of orogenic belts. The Yuli metamorphic belt has been the focus of regional tectonic studies in recent years (Tsai et al., 2013; Brown et al., 2015; Keyser et al., 2016; Chen et al., 2017). Four major serpentinite bodies crop out in Fengtien, Wanjung, Juisui...
