Results 121 to 130 of about 22,368 (251)

Results from the Apollo passive seismic experiment [PDF]

open access: yes
Recent results from the Apollo Seismic Network suggest that primitive differentiation occurred in the outer shell of the moon to a depth of approximately 300 km and the central region of the moon is presently molten to a radius of between 200 and 300 km.
Dorman, J.   +5 more
core   +1 more source

Home - About - Disclaimer - Privacy