Shun Li

ORCID: 0000-0002-1444-8899
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About
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Research Areas
  • Geological and Geochemical Analysis
  • Geology and Paleoclimatology Research
  • Metal-Organic Frameworks: Synthesis and Applications
  • earthquake and tectonic studies
  • Geological and Geophysical Studies
  • 3D Printing in Biomedical Research
  • Intermetallics and Advanced Alloy Properties
  • Covalent Organic Framework Applications
  • Bone Tissue Engineering Materials
  • Advanced materials and composites
  • Geological formations and processes
  • Geochemistry and Geologic Mapping
  • Nuclear Materials and Properties
  • Geophysics and Gravity Measurements
  • Climate variability and models
  • Geochemistry and Elemental Analysis
  • Supramolecular Chemistry and Complexes
  • Crystallography and molecular interactions
  • Hydrogels: synthesis, properties, applications
  • Dental Implant Techniques and Outcomes
  • Organic and Molecular Conductors Research
  • High Temperature Alloys and Creep
  • Paleontology and Stratigraphy of Fossils
  • Supramolecular Self-Assembly in Materials
  • Magnetism in coordination complexes

Shenzhen Institutes of Advanced Technology
2024

Chinese Academy of Sciences
2009-2024

Fujian Institute of Research on the Structure of Matter
2021-2024

Xiamen Institute of Rare-earth Materials
2021-2024

Shanghai Jiao Tong University
2022

Fujian Agriculture and Forestry University
2021

Center for Excellence in Tibetan Plateau Earth Sciences
2014-2019

Institute of Tibetan Plateau Research
2014-2019

Sun Yat-sen University
2017-2019

Université Laval
2017

Abstract We reconstruct the rise of a segment southern flank Himalaya-Tibet orogen, to south Lhasa terrane, using paleoaltimeter based on paleoenthalpy encoded in fossil leaves from two new assemblages Tibet (Liuqu and Qiabulin) four previously known floras Himalaya foreland basin. U-Pb dating zircons constrains Liuqu flora latest Paleocene (ca. 56 Ma) Qiabulin earliest Miocene (21–19 Ma). The proto-Himalaya grew slowly against high (∼4 km) proto–Tibetan Plateau ∼1 km late ∼2.3 at beginning...

10.1130/g38583.1 article EN cc-by Geology 2017-01-10

Abstract The scaffold that bioinspired natural bone‐periosteum is ideal for the repair of bone defects, while achievement a gradient with an integrated and stable interface remains challenging. Herein, collagen‐based developed, in which top layer electrospun collagen‐dense as periosteum (BP) to prevent invasion reticular fiber tissue bottom situ mineralized collagen (IMCS) promote osteogenic differentiation. Owing proposed continuous manufacturing successive 3D printing electrospinning,...

10.1002/adfm.202403235 article EN Advanced Functional Materials 2024-07-17

Abstract The physical microtopography, in an effective and stable manner, can powerfully confer biomaterials with enhanced osteoconduction for the repair of critical‐sized bone defects. However, realization osteoconductive microtopography within a 3D porous scaffold is still unmet. Herein, this work presents stone‐cottage‐inspired printing strategy to build microsphere patterned scaffolds tunable accelerated regeneration. customized composite inks poly (lactic‐ co ‐glycolic acid)...

10.1002/adfm.202417836 article EN Advanced Functional Materials 2024-10-30

Abstract Design of flexible porous materials where the diffusion guest molecules is regulated by dynamics contracted pore aperture challenging. Here, a self‐assembly consisting 1D channels with dynamic bottleneck gates reported. The pendant naphthimidazolylmethyl moieties at channel necks provide kinetic gate function, that enables unusual adsorption for light hydrocarbons. CO 2 mainly dominated thermodynamics uptakes decreasing increasing temperature, whereas adsorptions larger hydrocarbons...

10.1002/advs.202308028 article EN cc-by Advanced Science 2024-02-02

Abstract When the modern-like geomorphology and climate pattern of Himalaya-Tibetan Plateau were established still remains unclear. In this study, we apply paired stable isotope compositions carbonate (δ18Oc) leaf waxderived n-alkanes (δ2Halk) from upper Gazhacun Formation in Namling Basin to reconstruct middle Miocene elevation southern Tibet. Depositional age has been precisely constrained between 15.5 Ma 15.1 by zircon U-Pb ages dacite interlayers. Paired derived δ18Ow values (–17.9 ±...

10.1130/b36198.1 article EN Geological Society of America Bulletin 2022-02-14
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