By the end of 2018, 42 years after the landing of the two Viking seismometers on Mars,
InSight will deploy onto Mars' surface the SEIS (S eismic E xperiment for I nternal S tructure) …

The current state of understanding of the lunar interior is the sum of nearly four decades of
work and a range of exploration programs spanning that same time period. Missions of the …

High-resolution gravity data obtained from the dual Gravity Recovery and Interior Laboratory
(GRAIL) spacecraft show that the bulk density of the Moon's highlands crust is 2550 …

Despite recent insight regarding the history and current state of the Moon from satellite
sensing and analyses of limited Apollo-era seismic data, deficiencies remain in our …

Monitoring of vibrational eigenmodes of an elastic body excited by gravitational waves was
one of the first concepts proposed for the detection of gravitational waves. At laboratory …

Several seismic experiments were deployed on the Moon by the astronauts during the
Apollo missions. The experiments began in 1969 with Apollo 11, and continued with Apollo …

The deep structure of the Moon is a missing piece to understand the formation and evolution
of the Earth–Moon system. Despite the great amount of information brought by the Apollo …

We present crystallization experiments on silicate melt compositions related to the lunar
magma ocean (LMO) and its evolution with cooling. Our approach aims at constraining the …

An international team of researchers gathered, with the support of the International Space
Science Institute (ISSI),(1) to review seismological investigations of the lunar interior from the …

Seismic traveltime tomography is commonly discretized by a truncated expansion of the
pursued model in terms of chosen basis functions. Whether parametrization affects the …