A5071733459- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies
- Geology and Paleoclimatology Research
- Geological Studies and Exploration
- Geochemistry and Geochronology of Asian Mineral Deposits
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Elemental Analysis
- Mineralogy and Gemology Studies
- Hydrocarbon exploration and reservoir analysis
- Geological formations and processes
- Methane Hydrates and Related Phenomena
- Seismic Imaging and Inversion Techniques
- Archaeology and ancient environmental studies
- Radioactive element chemistry and processing
- Geomagnetism and Paleomagnetism Studies
- Geological Formations and Processes Exploration
- Marine and environmental studies
- Geoscience and Mining Technology
- Seismic Waves and Analysis
- Earthquake Detection and Analysis
- Geophysical and Geoelectrical Methods
- Geotechnical and Geomechanical Engineering
Institute of Earth Sciences, Academia Sinica
2015-2024
National Taiwan University
2015-2024
Chinese University of Hong Kong
2023
Academia Sinica
2015-2023
National Taiwan Normal University
2003-2020
ORCID
2020
Earth Science Institute of the Slovak Academy of Sciences
2017
Guangzhou Institute of Geochemistry
2003-2008
Chinese Academy of Sciences
2002-2008
Chinese Academy of Geological Sciences
2008
Plate tectonic processes introduce basaltic crust (as eclogite) into the peridotitic mantle. The proportions of these two sources in mantle melts are poorly understood. Silica-rich formed from eclogite react with peridotite, converting it to olivine-free pyroxenite. Partial this hybrid pyroxenite higher nickel and silicon but poorer manganese, calcium, magnesium than peridotite. Olivine phenocrysts' compositions record differences were used quantify contributions pyroxenite-derived mid-ocean...
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| October 01, 1995 Plume-lithosphere interaction in generation of the Emeishan flood basalts at Permian-Triassic boundary Sun-Lin Chung; Chung 1Department Geology, National Taiwan University, Taipei, Taiwan, Republic China Search for other works by this author on: GSW Google Scholar Bor-ming Jahn 2Géosciences Rennes, Université de Rennes 1, F-35042 Cedex, France Author and Article Information Publisher: Geological Society America First Online: 02 Jun 2017 Online ISSN:...
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...
Research Article| October 01, 2004 Geologic, geochemical, and geophysical consequences of plume involvement in the Emeishan flood-basalt province Yi-Gang Xu; Xu 1Guangzhou Institute Geochemistry, Chinese Academy Sciences, 510640 Guangzhou, China Search for other works by this author on: GSW Google Scholar Bin He; He Sun-Lin Chung; Chung 2Department Geosciences, National Taiwan University, Taipei 10699, Martin A. Menzies; Menzies 3Department Geology, Royal Holloway University London, Egham,...
New geochronological and geochemical data on magmatic activity from the India-Asia collision zone enables recognition of a distinct flare-up event that we ascribe to slab breakoff. This tie-point in collisional record can be used back-date time initial impingement Indian continent with Asian margin. Continental arc magmatism southern Tibet during 80-40 Ma migrated south north then back significant mantle input at 70-43 Ma. A pronounced flare up intensity (including ignimbrite mafic rock) ca....
The Okinawa Trough is an incipient intracontinental back arc basin that has developed behind the Ryukyu arc‐trench system. To explore its magmatic evolution and nature of mantle source, we present major trace element Sr‐Nd isotopic data for mafic volcanic rocks from Middle Southern Central Arc. Two episodes activity formed latter: older (∼21–13 Ma) younger (∼6–4 Ma). Although Quaternary basalts (MOT) have compositions comparable to intra‐oceanic basins, they are characterized by relative...
Research Article| April 01, 1997 Intraplate extension prior to continental extrusion along the Ailao Shan-Red River shear zone Sun-Lin Chung; Chung 1Department of Geology, National Taiwan University, Taipei 106-17, Search for other works by this author on: GSW Google Scholar Tung-Yi Lee; Lee 2Department Earth Sciences, Normal Taipei, Ching-Hua Lo; Lo Pei-Ling Wang; Wang Chin-Yu Chen; Chen Nguyen Trong Yem; Yem 3Institute Geological Center Natural Sciences and Technology, Hanoi, Vietnam Tran...
We present SHRIMP zircon dating, bulk-rock geochemical, and Sr-Nd-Pb isotopic results for Yeba volcanic rocks a mafic dike from Southern Gangdese (SG), southern Tibet, in order to constrain their tectonic setting origin. span continuous compositional range basalt dacite, although andesites are minor, felsic volumetrically predominant. New dating dacite coupled with previous fossil constraints the sedimentary sequence indicate that were emplaced Early Jurassic (174-190 Ma). tholeiitic possess...