In this review article, we discuss the evidence for populations of impactors delivered to the Moon at different times in the past. We also propose approaches to the identification and characterisation of meteoritic material on the Moon in the context of future lunar exploration efforts.Katherine H. Joy, Ian A. Crawford, Natalie M. Curran, Michael Zolensky, Amy F. Fagan & David A. Krin
We all know that the pock marked face of the Moon looks the way it does because it was hit by meteor...
planetary accumulation process, the Protoearth collided with a planetary body having a substantial f...
We use ordinary Newtonian orbital mechanics to explore the possibility that near side lunar maria ar...
The Moon is an archive of impact cratering in the Solar System throughout the past 4.5 billion years...
The Moon is an archive of impact cratering in the Solar System throughout the past 4.5 billion years...
The Moon continues to provide scientific answers – and pose new questions – over 40 years after the ...
During the last half decade, hundreds of scientists from many countries have been studying the sampl...
Lunar meteorites constitute direct, varied samples of the materials forming the lunar surface, allow...
The Moon acts as a time capsule for events in our region of the Solar System. The combination of ret...
The leading hypothesis for the origin of the Moon is the giant impact model, which grew out of the p...
The Moon is the only planetary body other than the Earth for which samples have been collected in si...
Impact events have played an important role in the evolution of planets and small bodies in the Sola...
A general review of lunar science is presented, utilizing two themes: a summary of fundamental probl...
The discrepancy between the impact records on the Earth and Moon in the time period, 4.0–3.5 Ga call...
Micrometeorites, ancient planetesimal debris from the early intense bombardment, and debris of recen...
We all know that the pock marked face of the Moon looks the way it does because it was hit by meteor...
planetary accumulation process, the Protoearth collided with a planetary body having a substantial f...
We use ordinary Newtonian orbital mechanics to explore the possibility that near side lunar maria ar...
The Moon is an archive of impact cratering in the Solar System throughout the past 4.5 billion years...
The Moon is an archive of impact cratering in the Solar System throughout the past 4.5 billion years...
The Moon continues to provide scientific answers – and pose new questions – over 40 years after the ...
During the last half decade, hundreds of scientists from many countries have been studying the sampl...
Lunar meteorites constitute direct, varied samples of the materials forming the lunar surface, allow...
The Moon acts as a time capsule for events in our region of the Solar System. The combination of ret...
The leading hypothesis for the origin of the Moon is the giant impact model, which grew out of the p...
The Moon is the only planetary body other than the Earth for which samples have been collected in si...
Impact events have played an important role in the evolution of planets and small bodies in the Sola...
A general review of lunar science is presented, utilizing two themes: a summary of fundamental probl...
The discrepancy between the impact records on the Earth and Moon in the time period, 4.0–3.5 Ga call...
Micrometeorites, ancient planetesimal debris from the early intense bombardment, and debris of recen...
We all know that the pock marked face of the Moon looks the way it does because it was hit by meteor...
planetary accumulation process, the Protoearth collided with a planetary body having a substantial f...
We use ordinary Newtonian orbital mechanics to explore the possibility that near side lunar maria ar...