岩浆海的演化对宜居星球的形成有何意义？

孙卫东; 商修齐

doi:10.3799/dqkx.2022.825

Volume 47 Issue 10

Oct. 2022

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2022 > 47(10): 3823-3824

Sun Weidong, Shang Xiuqi, 2022. How did the Magma Ocean Contribute to the Formation of the Habitable Earth?. Earth Science, 47(10): 3823-3824. doi: 10.3799/dqkx.2022.825

Citation:

Sun Weidong, Shang Xiuqi, 2022. How did the Magma Ocean Contribute to the Formation of the Habitable Earth?. Earth Science, 47(10): 3823-3824. doi: 10.3799/dqkx.2022.825

Sun Weidong, Shang Xiuqi, 2022. How did the Magma Ocean Contribute to the Formation of the Habitable Earth?. Earth Science, 47(10): 3823-3824. doi: 10.3799/dqkx.2022.825

Citation:

Sun Weidong, Shang Xiuqi, 2022. How did the Magma Ocean Contribute to the Formation of the Habitable Earth?. Earth Science, 47(10): 3823-3824. doi: 10.3799/dqkx.2022.825

PDF( 276 KB)

How did the Magma Ocean Contribute to the Formation of the Habitable Earth?

doi: 10.3799/dqkx.2022.825

Sun Weidong^{1, 2
,},
Shang Xiuqi^{1, 2}

Publish Date: 2022-10-25

Abstract

FullText(HTML)

References(1)

References

Sun, W. D., Hawkesworth, C. J., Yao, C., et al., 2018. Carbonated Mantle Domains at the Base of the Earth's Transition Zone. Chemical Geology, 478: 69-75. https://doi.org/10.1016/j.chemgeo.2017.08.001

Relative Articles

Supplements(0)

Cited By

Proportional views