Shallow moonquake mechanisms illuminated by rheologic characteristics of basaltic gouges
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The projected evolutionary history of the Moon and observed occurrence of moonquakes suggest that brittle faulting is present in the shallow lunar crust. Chang'e 5 samples of lunar regolith show a mineral composition almost identical to basaltic bedrock. We measure the friction-stability characteristics of dry synthetic gouges representative of basaltic faults assumed to be present in the lunar crust. Frictional strengths are ~0.7 and exhibit overall velocity-strengthening response but transition to velocity-weakening at intermediate temperatures (100-300â) and stresses (10-100 MPa). Bounding temperature profiles representative of the lunar crust suggest that moonquakes are feasible throughout the shallowest ~40-60 km of the crust. However, observations of unusually high stress drops (up to 210 MPa) are inconsistent with the measured frictional strengths â suggesting that high degrees of healing on preexisting faults or intact crust are present â to augment stress accumulation mechanism..., , , # Data from: Shallow moonquake mechanisms illuminated by rheologic characteristics of basaltic gouges
[https://doi.org/10.5061/dryad.18931zd3b](https://doi.org/10.5061/dryad.18931zd3b)
**Fengshou Zhang, Wenzhi Zhao, Mengke An, Xianda Shen, Jizhou Tang, Luanxiao Zhao, Hai Liu, Derek Elsworth, Hehua Zhu, Manchao He. Shallow moonquake mechanisms illuminated by rheologic characteristics of basaltic gouges. *Journal of Geophysical Research: Planets*.**
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**Experimental data:**
**The friction-displacement data for all shear experiments on simulated mare basaltic gouges.**
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**Authors:**
Fengshou Zhang
Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai 200092, China
Key Laboratory of Geotechnical & Underground Engineering of Ministry of Education, Tongji University, Shanghai 200092, China
fengshou.zhang...
创建时间:
2025-07-12



