A5024021692- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
- Geology and Paleoclimatology Research
- Geochemistry and Geochronology of Asian Mineral Deposits
- Hydrocarbon exploration and reservoir analysis
- Geological Studies and Exploration
- Geological formations and processes
- Radioactive element chemistry and processing
- Astro and Planetary Science
- Geomagnetism and Paleomagnetism Studies
- CO2 Sequestration and Geologic Interactions
- Geological Modeling and Analysis
- Methane Hydrates and Related Phenomena
- Paleontology and Stratigraphy of Fossils
- Mineralogy and Gemology Studies
- Archaeology and ancient environmental studies
- Landslides and related hazards
- Oceanographic and Atmospheric Processes
- Clay minerals and soil interactions
- Coal and Its By-products
- Ocean Acidification Effects and Responses
National Taiwan University
2014-2025
National Taiwan Ocean University
2018
Macquarie University
2009-2015
ARC Centre of Excellence for Core to Crust Fluid Systems
2009-2015
Australian Research Council
2011
Institute of Earth Sciences, Academia Sinica
2009
National Taiwan Normal University
2003
Louisiana State University
1994
Research Article| November 01, 2003 Adakites from continental collision zones: Melting of thickened lower crust beneath southern Tibet Sun-Lin Chung; Chung 1Department Geosciences, National Taiwan University, Taipei, Search for other works by this author on: GSW Google Scholar Dunyi Liu; Liu 2Institute Geology, Chinese Academy Geological Sciences, Beijing, China Jianqing Ji; Ji 3School Earth and Space Peking Mei-Fei Chu; Chu 4Department Hao-Yang Lee; Lee Da-Jen Wen; Wen Ching-Hua Lo; Lo...
Research Article| September 01, 2006 Zircon U-Pb and Hf isotope constraints on the Mesozoic tectonics crustal evolution of southern Tibet Mei-Fei Chu; Chu 1Department Geosciences, National Taiwan University, Taipei, Search for other works by this author on: GSW Google Scholar Sun-Lin Chung; Chung Biao Song; Song 2Institute Geology, Chinese Academy Geological Sciences, Beijing, China Dunyi Liu; Liu Suzanne Y. O'Reilly; O'Reilly 3Australian Council Key Centre Geochemical Evolution Metallogeny...
Apatites crystallized from different types of igneous rocks show significant variations in the abundances some minor and trace elements. In this study, electron probe microanalysis laser ablation inductively coupled plasma mass spectrometry were used to determine concentrations 25 elements apatite separated three principal rock Transhimalayan plutonic suite: S-type granites, I-type Gangdese batholith post-collisional adakites. F, Mn, Sr rare earth (REE) vary systematically with composition...
Abstract The origin and geodynamic evolution of peak Early Cretaceous magmatism in the southern Great Xing'an Range, North China, have long been controversial. Here we report new U‐Pb zircon ages (141–129 Ma) a suite dioritic‐granitic rocks from central Inner Mongolia, far sutures or plate boundaries Paleo‐Pacific Mongol‐Okhotsk oceans, thus delineating an intracontinental magmatic province, which had activity at 130–120 Ma. Dioritic including diorite, tonalite, granodiorite shows variable ε...
<title>Abstract</title> The Tatun Volcano Group (TVG) in northern Taiwan is part of the Northern Volcanic Zone (NTVZ), formed an extensional back-arc setting at western end Ryukyu subduction system. Recent studies have shown that TVG much younger than previously thought, though reliable eruption ages are still scarce, complicating reconstruction its eruptive history. In this study, we used high-precision <sup>40</sup>Ar/<sup>39</sup>Ar dating plagioclase and groundmass, along with U-Th...
Abstract Chemical weathering modulates carbon transfer between the crust, hydrosphere, and atmosphere. The extent to which microbial processes are involved in mineral dissolution remains elusive. Here, we performed geochemical molecular analyses of river water other materials collected from a rapidly exhuming catchment eastern Taiwan. In addition solute generation driven primarily by pyrite-induced carbonate weathering, highly skewed community compositions with abundant Sulfuricurvum...
Research Article| October 17, 2017 Water-fluxed crustal melting and petrogenesis of large-scale Early Cretaceous intracontinental granitoids in the southern Great Xing'an Range, North China Shan Li; Li † 1Institute Geology, Chinese Academy Geological Sciences, Beijing 100037, China2Department Geosciences, National Taiwan University, Taipei 10617, †lishan428@163.com Search for other works by this author on: GSW Google Scholar Sun-Lin Chung; Chung 2Department Taiwan3Institute Earth Academia...
Encircled by arcs and trenches, the western Pacific region of Philippine Sea is exposed to trans-oceanic tsunamis pumice rafts. However, shortage extended archive has limited our knowledge tsunami recurrence, sources, drifting routes. This study identifies a backshore colluvium with three new gravel layers in northern Taiwan, stratigraphically below four previously reported pumice-bearing paleotsunami deposits from last millennium. The are attributed tsunamis, based on foreshore-derived...
Abstract Cenozoic magmatism occurs throughout West Sulawesi, Indonesia, yet its detailed evolution remains enigmatic due mainly to the scarcity of precise dating. Here, we report new whole-rock geochemical and zircon U-Pb-Hf isotopic data plutonic/volcanic rocks river sediments from Sulawesi constrain petrogenesis magmatic tempo. The are intermediate felsic (SiO2 = 58.1–68.0 wt%), high-K calc-alkaline shoshonitic (K2O 2.2–6.0 metaluminous weakly peraluminous, I-type in composition. Trace...
This study focused on the chemistry of sedimentary pore fluids to clarify hydrothermal fluid migrating within sediments at Geolin Mounds (GLM) and Mienhua Volcano (MHV) fields, southernmost Okinawa Trough, where are characterized by covering thick sediment. The significant downward decrease in Mg2+ (low 23.3 mmol L−1) concurrent increase Li+ (up 2,269 μmol implied a substantial influence fluid, which might be associated with high-temperature (>350 °C) rock/sediment-fluid interaction. best...