Hairuo Fu

ORCID: 0000-0002-1823-2016
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About
Contact & Profiles
Research Areas
  • Astro and Planetary Science
  • Geological and Geochemical Analysis
  • Geomagnetism and Paleomagnetism Studies
  • Planetary Science and Exploration
  • High-pressure geophysics and materials
  • Geological Studies and Exploration
  • Geology and Paleoclimatology Research
  • earthquake and tectonic studies
  • Paleontology and Stratigraphy of Fossils
  • Methane Hydrates and Related Phenomena
  • Isotope Analysis in Ecology
  • Geochemistry and Geologic Mapping
  • Geophysics and Gravity Measurements
  • Geochemistry and Elemental Analysis
  • Mass Spectrometry Techniques and Applications
  • Atmospheric and Environmental Gas Dynamics
  • Hydrocarbon exploration and reservoir analysis
  • Atmospheric Ozone and Climate
  • Paleontology and Evolutionary Biology
  • Scientific Research and Discoveries
  • Geological and Geophysical Studies
  • Hydraulic Fracturing and Reservoir Analysis

Harvard University
2021-2024

China University of Geosciences
2024

Planetary Science Institute
2021-2023

Harvard University Press
2022-2023

China University of Geosciences (Beijing)
2018-2022

10.1016/j.epsl.2022.117743 article EN publisher-specific-oa Earth and Planetary Science Letters 2022-08-03

Abstract To better constrain the evolution of Mongol‐Okhotsk suture, we carried out new paleomagnetic studies on Sharilyn Formation (~155 Ma) and Tsagantsav (~130 in southern Mongolia, Amuria Block (AMU), Tuchengzi (~140 Dadianzi/Yixian Yanshan belt, North China (NCB). A total 719 collected samples (from 100 sites) were subjected to stepwise thermal demagnetization. After a low‐temperature component viscous magnetic remanence acquired recent field was removed, stable high‐temperature...

10.1029/2018jb016703 article EN Journal of Geophysical Research Solid Earth 2018-11-29

Abstract We have conducted an extensive towed-magnetic-sled survey during the period 2023 June 14–28, over seafloor about 85 km north of Manus Island, Papua New Guinea, centered around calculated path bolide CNEOS 2014 January 8 (IM1). found 850 spherules diameter 0.05–1.3 mm in our samples. They were analyzed by microXRF, Electron Probe Microanalyzer and ICP Mass spectrometry. identified 22% as product planetary igneous differentiation labeled them D-type spherules. A small portion...

10.3847/2515-5172/ad2370 article EN cc-by Research Notes of the AAS 2024-01-31

Abstract Mass-dependent stable isotopic variations recorded in lunar samples provide novel resolution to the formation and differentiation history of Moon. In this study, we report new high-precision Ca-isotope measurements for rocks minerals. data modeling magma ocean together demonstrate indistinguishable mass-dependent Ca compositions bulk silicate Earth This implied Earth-Moon isotope equilibration is consistent with Moon’s high-energy giant-impact (Synestia) origin not readily...

10.1038/s43247-023-00974-4 article EN cc-by Communications Earth & Environment 2023-09-05

Abstract The Tonian supercontinent Rodinia is hypothesized to have included almost all Proterozoic continental blocks. Competing models variably place South China at the core or periphery of separated from it entirely. paleogeographic also vary in whether they incorporate large and rapid oscillatory true polar wander associated with ca. 810–795 Ma Bitter Springs Stage. Here, we present paleomagnetic data paired U‐Pb chemical abrasion isotope dilution thermal ionization mass spectrometry...

10.1029/2020jb021541 article EN publisher-specific-oa Journal of Geophysical Research Solid Earth 2021-05-17

The rate of movement Earth's solid shell relative to its spin axis, or true polar wander, depends on variations in mantle convection and viscosity. We report paleomagnetic geochronologic data from South China that constrain the rapid wander (>5° per million years) between 832 years 821 ago. Analysis database demonstrates secular change related cooling thermal structure across supercontinent cycles. True rates are relatively muted with a partially insulated during assembly accelerate as...

10.1126/sciadv.abo2753 article EN cc-by-nc Science Advances 2022-10-14

We have conducted an extensive towed-magnetic-sled survey during the period 14-28 June, 2023, over seafloor centered around calculated path of bolide CNEOS 2014-01-08 (IM1) about 85 km north Manus Island, Papua New Guinea. found 700 spherules diameter 0.05-1.3 millimeters in our samples, which 57 were analyzed so far. The significantly concentrated along expected meteor path. Mass spectrometry 47 near high-yield regions IM1's reveals a distinct extra-solar abundance pattern for 5 them, while...

10.48550/arxiv.2308.15623 preprint EN cc-by-nc-nd arXiv (Cornell University) 2023-01-01

We have conducted an extensive towed-magnetic-sled survey during the period of June 14-28, 2023, over seafloor about 85 km north Manus Island, Papua New Guinea, centered around calculated path bolide CNEOS 2014-01-08 (IM1). found 850 spherules diameter 0.1-1.3 millimeters in our samples. The samples were analyzed by micro-XRF, Electron Probe Microanalyzer and ICP Mass spectrometry. Here we report major trace element compositions classify based on that analysis. identified 78% as primitive,...

10.48550/arxiv.2401.09882 preprint EN cc-by arXiv (Cornell University) 2024-01-01

Abstract Stable isotopic variations recorded in lunar samples provide novel and crucial resolution to the differentiation history of Moon. We report new high-precision Ca-isotope measurements for rocks minerals. data modeling magma ocean together demonstrate indistinguishable Ca compositions between bulk silicate Earth Moon, consistent with isotope equilibration Moon preceding differentiation. This is also high-energy giant impact (Synestia) origin Earth-Moon system. Moreover,...

10.21203/rs.3.rs-2548042/v1 preprint EN cc-by Research Square (Research Square) 2023-03-21

The rate of movement Earth’s solid shell relative to its spin axis, or true polar wander, depends on variations in mantle convection and viscosity. We report paleomagnetic geochronologic data from South China that constrain the rapid wander (>5° Myr-1) 832–821 million years ago. Analysis database demonstrates secular change related cooling thermal structure across supercontinent cycles. True rates are relatively muted with a partially insulated during assembly accelerate as mixing...

10.31223/x5km0w preprint EN cc-by EarthArXiv (California Digital Library) 2022-09-15
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