A5100676789- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Methane Hydrates and Related Phenomena
- Geological and Geophysical Studies
- Geochemistry and Geologic Mapping
- Geochemistry and Elemental Analysis
- Astro and Planetary Science
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geophysics and Gravity Measurements
- Planetary Science and Exploration
- Spacecraft and Cryogenic Technologies
- Hydrocarbon exploration and reservoir analysis
- Offshore Engineering and Technologies
- Nuclear physics research studies
- Geomagnetism and Paleomagnetism Studies
- Paleontology and Stratigraphy of Fossils
- Geological Studies and Exploration
- Dyeing and Modifying Textile Fibers
- Astronomical Observations and Instrumentation
- Geological Modeling and Analysis
- Geological formations and processes
- Radioactive Decay and Measurement Techniques
- Mining and Gasification Technologies
- Nuclear Physics and Applications
East China University of Technology
2025
Guangzhou Institute of Geochemistry
2014-2024
Chinese Academy of Sciences
2015-2024
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2021-2024
Wuhan Textile University
2022-2024
Second Affiliated Hospital of Nanjing Medical University
2024
Jingdezhen Ceramic Institute
2024
University of the Arts London
2024
University of Salerno
2024
First People's Hospital of Chongqing
2024
Abstract Combined analyses of deep tow magnetic anomalies and International Ocean Discovery Program Expedition 349 cores show that initial seafloor spreading started around 33 Ma in the northeastern South China Sea (SCS), but varied slightly by 1–2 Myr along northern continent‐ocean boundary (COB). A southward ridge jump ∼20 km occurred 23.6 East Subbasin; this timing also was coeval to onset Southwest Subbasin, which propagated for about 400 southwestward from ∼23.6 ∼21.5 Ma. The terminal...
Abstract Coring/logging data and physical property measurements from International Ocean Discovery Program Expedition 349 are integrated with, correlated to, reflection seismic to map sequence boundaries facies of the central basin neighboring regions South China Sea. First‐order interpreted, which Oligocene/Miocene, middle Miocene/late Miocene, Miocene/Pliocene, Pliocene/Pleistocene boundaries. A characteristic early Pleistocene strong reflector is also identified, marks top extensive...
Paleogene mafic potassic and ultrapotassic volcanic rocks in western Yunnan, China, show a compositional spectrum from trachybasalt to latite (MgO = 6·24–21·8 wt %; SiO2 44·5–59·1 %). These have high K2O (3·07–5·28 %), relatively low Na2O (0·99–4·18 %) K2O/Na2O ratios (0·91–3·89). They share geochemical features such as depletion of Ta, Nb Ti relative other similarly incompatible elements enriched Sr–Nd isotopic compositions (initial 87Sr/86Sr 0·7056–0·7101; εNd(t) –0·97 –4·36). The contain...
The Yichun topaz–lepidolite granite is the latest and most evolved unit of granitic complex, South China, well known by virtue its unusual Ta–Nb–Li mineralization. A drill hole down to 300 m has intersected from top bottom, revealed three petrographic zones: K-feldspar-rich facies in lower part, albite-rich middle Ab- Kfs-rich upper part. Geochemically, belongs phosphorus-rich type rare-element-enriched granite. phosphorus concentrated feldspars, which contain up 0.93 wt% P2O5. It less...