HelioWebChinese Academy of Sciences, Shanghai
flowchart
I[Chinese Academy of Sciences, Shanghai]
PI["Parent Institutions (1)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (30)"]
CA["Linked Collaborating Authors (9)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
click CI "#child-institutions"
click AW "#affiliated-works"
click CA "#collaborating-authors"
Parent Institutions [?]
Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- Research on Laser Frequency Stabilization of CO2 Laser measurement system
- Chinese carbon dioxide observation satellite (TanSat) project
- Chinese Carbon Dioxide Satellite (TanSat) Status and Plans
- Temporal and Spatial Pattern of Changes of Extreme Precipitation in the Middle and Lower Yangtze River Basin (YRB) during 1960 to 2012
- Equatorial Zonal Jets and Jupiter's Gravity
- Ground Verification Test of Lunar Mineralogical Spectrometer on the Chang'e 5 Lunar Sample Return Lander
- Synthesis and equation of state of high pressure phase of chromium-bearing spinel
- Background Ozone in Southern China During 1994-2015: Role of Anthropogenic Emission and Climate Change
- Global carbon uptake by cement carbonation
- On the Elastic Shear Modulus of Jupiter's Solid Core
- Electrical and thermal conductivity of Fe-C alloy at high pressure: implications for effects of carbon on the geodynamo of the Earth's core
- Hydrogen-bond symmetrization breakdown and dehydrogenation mechanism in FeO<SUB>2</SUB>H at high pressure
- Single-crystal structure determination of hydrous minerals and insights into a wet deep lower mantle
- Electrical resistivity of Fe-C and Fe-Si alloy at high pressure and the light element effects on Earth's core
- Interaction of major volatiles with the lower mantle: implications for deep volatile cycles
- Temperature-induced amorphization in CaCO<SUB>3 at high pressure</SUB>: Implication for recycled CaCO<SUB>3</SUB> in the transition zone
- The influence of redox condition on crystal structures of bridgmanite at megabar pressure
- The stability of Fe-bearing δ-phase and pyrite-phase FeOOH<SUB>x</SUB> in the Earth's lowermost mantle: Experimental constrains from a hydrated Fe,Al-bearing MgSiO<SUB>3</SUB> composition
- Toward a new generation Mars Global Climate Model at LMD
- Transport Properties of Fe at Earth's Core Conditions: Agreement between Experiment and Theory
- Development of High-Pressure Multigrain X-Ray Diffraction forExploring the Earth's Interior
- Discovery of a hexagonal phase in (Fe,Al)OOH under the P-T conditions of the deep lower mantle
- Hydrous Phases in Earth's Lowermost Mantle
- Melting of iron up to core pressures determined by in-situ electrical resistance jump
- Kinetics study of dehydrogenation of pyrite-FeO<SUB>2</SUB>H above 1 Mbar using laser heating and time-resolved synchrotron x-ray diffraction
- Quantifying the water content in dense SiO<SUB>2</SUB>
- Concept of the solar ring mission
- Deep Subduction of H2O in SiO2 Phases
- Monitoring Water Level Variations of the Urmia Lake by Multi-Altimetry Missions
- Superionicity of iron compounds in the deep Earth's conditions