Thickness of Lava Flows Within the Northern Smooth Plains on Mercury as Estimated by Partially Buried Craters-Reference-Cited by-同舟云学术

Thickness of Lava Flows Within the Northern Smooth Plains on Mercury as Estimated by Partially Buried Craters

Published:2020-10-19 Issue:20 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Du Jun¹²^ORCID,Wieczorek Mark A.²^ORCID,Fa Wenzhe¹³⁴^ORCID

Affiliation:

1. Institute of Remote Sensing and Geographical Information System, School of Earth and Space Sciences Peking University Beijing China

2. Laboratoire Lagrange Université Côte d'Azur, Observatoire de la Côte d'Azur, CNRS Nice France

3. State Key Laboratory of Lunar and Planetary Sciences Macau University of Science and Technology Macau China

4. CAS Center for Excellence in Comparative Planetology Hefei China

Funder

China Scholarship Council

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL090578

Reference48 articles.

1. The morphology of craters on Mercury: Results from MESSENGER flybys

2. Becker K. Robinson M. Becker T. Weller L. Edmundson K. Neumann G. &Solomon S.(2016).First global digital elevation model of Mercury. In47th Lunar and Planetary Science Conference #2959.

3. A comparison of inner Solar System volcanism

4. Widespread effusive volcanism on Mercury likely ended by about 3.5 Ga

5. Analytical Theory of Erosion

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