TY - JOUR
T1 - Inferring the Shallow Layered Structure at the Chang’E-4 Landing Site
T2 - A Novel Interpretation Approach Using Lunar Penetrating Radar
AU - Giannakis, Iraklis
AU - Zhou, Feng
AU - Warren, Craig
AU - Giannopoulos, Antonios
PY - 2021/8/28
Y1 - 2021/8/28
N2 - The current paper investigates the shallow layers of the lunar regolith at the Chang’E-4 landing site. Four layers between 0 and 10 m were identified using lunar penetrating radar. Based on these outputs, a revised stratigraphic model is suggested for the post-Imbrian ejecta at the Von Kármán crater. The layers were previously unseen due to the smooth boundaries between them. The revised model was inferred using an advanced hyperbola-fitting scheme. Applying conventional hyperbola-fitting to non-homogeneous media results in errors and inaccuracies that are often wrongly assumed to be negligible. We propose a novel hyperbola-fitting scheme that is, not constrained to homogeneous media and can be applied subject to any arbitrary one-dimensional permittivity distribution. Via this approach, we can estimate the permittivity profile of an investigated area and detect layered structures that were previously transparent to electromagnetic waves due to the gradational dielectric properties at their interfaces.
AB - The current paper investigates the shallow layers of the lunar regolith at the Chang’E-4 landing site. Four layers between 0 and 10 m were identified using lunar penetrating radar. Based on these outputs, a revised stratigraphic model is suggested for the post-Imbrian ejecta at the Von Kármán crater. The layers were previously unseen due to the smooth boundaries between them. The revised model was inferred using an advanced hyperbola-fitting scheme. Applying conventional hyperbola-fitting to non-homogeneous media results in errors and inaccuracies that are often wrongly assumed to be negligible. We propose a novel hyperbola-fitting scheme that is, not constrained to homogeneous media and can be applied subject to any arbitrary one-dimensional permittivity distribution. Via this approach, we can estimate the permittivity profile of an investigated area and detect layered structures that were previously transparent to electromagnetic waves due to the gradational dielectric properties at their interfaces.
KW - Chang’E-4
KW - South-Pole Aitken (SPA)
KW - ground penetrating radar (GPR)
KW - hyperbola-fitting
KW - lunar penetrating radar (LPR)
UR - http://www.scopus.com/inward/record.url?scp=85113467473&partnerID=8YFLogxK
U2 - 10.1029/2021gl092866
DO - 10.1029/2021gl092866
M3 - Letter
VL - 48
SP - 1
EP - 14
JO - Geophysical Research Letters
JF - Geophysical Research Letters
SN - 0094-8276
IS - 16
M1 - e2021GL092866
ER -