A5075809078- Geological and Geochemical Analysis
- Geochemistry and Elemental Analysis
- Paleontology and Stratigraphy of Fossils
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- High-pressure geophysics and materials
- Isotope Analysis in Ecology
- Radioactive element chemistry and processing
- Plasmonic and Surface Plasmon Research
- Vanadium and Halogenation Chemistry
- Hydrocarbon exploration and reservoir analysis
- Gold and Silver Nanoparticles Synthesis and Applications
- Groundwater and Isotope Geochemistry
- Fuzzy Logic and Control Systems
- Astro and Planetary Science
- Mercury impact and mitigation studies
- Gas Sensing Nanomaterials and Sensors
- Geological and Geophysical Studies
- Analytical chemistry methods development
- Nanocomposite Films for Food Packaging
- Advanced oxidation water treatment
- Analytical Chemistry and Chromatography
- Metamaterials and Metasurfaces Applications
- Wireless Power Transfer Systems
- Metal Extraction and Bioleaching
China University of Geosciences
2017-2024
Mindray (China)
2024
Memorial University of Newfoundland
2023
Macquarie University
2019-2022
National High Magnetic Field Laboratory
2018-2022
Florida State University
2018-2022
Hefei University of Technology
2021
University of Science and Technology of China
2010-2019
North University of China
2010-2019
Hefei University
2018
This article presents a high precision method for Ba isotope measurements using multiple-collector inductively coupled plasma-mass spectrometry (MC-ICP-MS).
The transition from mafic to felsic upper continental crust (UCC) is crucial habitability of Earth, and may be related the onset plate tectonics. Thus, defining when this crustal occurred has great significance for evolution Earth its inhabitants. We demonstrate that V isotope ratios (reported as δ51V) provide insights into because they correlate positively with SiO2 negatively MgO contents during igneous differentiation in both subduction zones intraplate settings. Because δ51V not affected...
Abstract In the past few years, so-called mélange model has been offered as an alternative to long-standing of enrichment subarc mantle by separate additions fluid and sediment components from subducting plate. model, plate become physically mixed at slab-mantle interface. Partial melting peridotite subsequently occurs after being hybridized material that diapirically rises into hotter portions wedge. Here, we present first Ba isotope study lavas Tonga-Kermadec arc (southwest Pacific Ocean)...
Deep neural networks have become foundational to advancements in multiple domains, including recommendation systems, natural language processing, and so on. Despite their successes, these models often contain incompatible parameters that can be underutilized or detrimental model performance, particularly when faced with specific, varying data distributions. Existing research excels removing such merging the outputs of different pretrained models. However, former focuses on efficiency rather...
Deep neural networks have become foundational to advancements in multiple domains, including recommendation systems, natural language processing, and so on. Despite their successes, these models often contain incompatible parameters that can be underutilized or detrimental model performance, particularly when faced with specific, varying data distributions. Existing research excels removing such merging the outputs of different pretrained models. However, former focuses on efficiency rather...
Abstract Cyclostratigraphy and astrochronology are now at the forefront of geologic timekeeping. While this technique heavily relies on accuracy astronomical calculations, solar system chaos limits how far back calculations can be performed with confidence. High‐resolution paleoclimate records Milankovitch imprints allow reversing traditional cyclostratigraphic approach: Middle Eocene drift sediments from Newfoundland Ridge well‐suited for purpose, due to high sedimentation rates distinct...