Lunar impact craters identification and age estimation with Chang'E data by deep and transfer learning

Impact craters, as "lunar fossils", are the most dominant lunar surface features and occupy most of the Moon's surface. Their formation and evolution record the history of the Solar System. Sixty years of triumphs in the lunar exploration projects accumulated a large amount of lunar data. Currently, there are 9137 existing recognized craters. However, only 1675 of them have been determined age, which is obviously not satisfactory to reveal the evolution of the Moon. Identifying craters is a challenging task due to their enormous difference in size, large variations in shape and vast presence. Furthermore, estimating the age of craters is extraordinarily difficult due to their complex and different morphologies. Here, in order to effectively identify craters and estimate their age, we convert the crater identification problem into a target detection task and crater age estimation into a taxonomy structure. From an initial small number of available craters, we progressively identify craters and estimate their age from Chang'E data by transfer learning (TL) using deep neural networks. For comprehensive identification of multi-scale craters, a two-stage craters detection approach is developed. Thus 117240 unrecognized lunar craters that range in diameter from 532 km to 1 km are identified. Then, a two-stage classification approach is developed to estimate the age of craters by simultaneously extracting their morphological features and stratigraphic information. The age of 79243 craters larger than 3 km in diameter is estimated. These identified and aged craters throughout the mid and low-latitude regions of the Moon are crucial for reconstructing the dynamic evolution process of the Solar System.

[1]  Ling Shao,et al.  Transfer Learning for Visual Categorization: A Survey , 2015, IEEE Transactions on Neural Networks and Learning Systems.

[2]  H. Hiesinger,et al.  Crater density differences: Exploring regional resurfacing, secondary crater populations, and crater saturation equilibrium on the moon , 2017, Planetary and Space Science.

[3]  A. F. Adams,et al.  The Survey , 2021, Dyslexia in Higher Education.

[4]  Yu Lu,et al.  Geology, tectonism and composition of the northwest Imbrium region , 2018 .

[5]  Graham Ryder,et al.  Mass flux in the ancient Earth‐Moon system and benign implications for the origin of life on Earth , 2002 .

[6]  Qiang Yang,et al.  A Survey on Transfer Learning , 2010, IEEE Transactions on Knowledge and Data Engineering.

[7]  J. Boyce,et al.  Absolute model ages from lunar crater morphology , 2015 .

[8]  J. McCauley,et al.  Geologic Map of the Near Side of the Moon , 1971 .

[9]  Erwan Mazarico,et al.  Lunar impact basins: Stratigraphy, sequence and ages from superposed impact crater populations measured from Lunar Orbiter Laser Altimeter (LOLA) data , 2012 .

[10]  J. Head,et al.  Geophysical Characteristics of Von Kármán Crater: Chang'E 4 Landing Site Region , 2019 .

[11]  Chunlai Li,et al.  Global estimates of lunar iron and titanium contents from the Chang' E‐1 IIM data , 2012 .

[12]  K. Tsiganis,et al.  Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets , 2005, Nature.

[13]  Long Xiao China's touch on the Moon , 2014 .

[14]  Jun Li,et al.  Lunar Crater Detection Based on Terrain Analysis and Mathematical Morphology Methods Using Digital Elevation Models , 2018, IEEE Transactions on Geoscience and Remote Sensing.

[15]  Erwan Mazarico,et al.  Global Distribution of Large Lunar Craters: Implications for Resurfacing and Impactor Populations , 2010, Science.

[16]  C. Chapman,et al.  What are the real constraints on the existence and magnitude of the late heavy bombardment , 2007 .

[17]  Wei Zuo,et al.  The Chang’e 3 Mission Overview , 2015 .

[18]  Farouk El-Baz,et al.  Geologic map of the east side of the Moon , 1977 .

[19]  Christian Koeberl,et al.  The Late Heavy Bombardment in the Inner Solar System: Is there any Connection to Kuiper Belt Objects? , 2003 .

[20]  Yang Zi-yuan,et al.  The Primary Science Results from the Chang’e-1 Probe , 2010 .

[21]  Long Xiao,et al.  Geological Characteristics of Von Kármán Crater, Northwestern South Pole‐Aitken Basin: Chang'E‐4 Landing Site Region , 2018, Journal of Geophysical Research: Planets.

[22]  Bo Li,et al.  Lunar iron and optical maturity mapping: Results from partial least squares modeling of Chang'E-1 IIM data , 2016 .

[23]  Newell J. Trask,et al.  The Geologic History of the Moon , 2020 .

[24]  Mohamad Ali-Dib,et al.  Lunar crater identification via deep learning , 2018, Icarus.

[25]  W. Bottke,et al.  Earth and Moon impact flux increased at the end of the Paleozoic , 2019, Science.

[26]  Wei Zuo,et al.  Chang’E-4 initial spectroscopic identification of lunar far-side mantle-derived materials , 2019, Nature.

[27]  M. Norman,et al.  The Late Heavy Bombardment , 2017 .

[28]  Sebastian Thrun,et al.  Dermatologist-level classification of skin cancer with deep neural networks , 2017, Nature.

[29]  Arjan Durresi,et al.  A survey: Control plane scalability issues and approaches in Software-Defined Networking (SDN) , 2017, Comput. Networks.

[30]  S. Sanjeevi,et al.  Crater detection, classification and contextual information extraction in lunar images using a novel algorithm , 2013 .

[31]  William K. Hartmann,et al.  Lunar cratering chronology , 1970 .

[32]  Guigang Zhang,et al.  Deep Learning , 2016, Int. J. Semantic Comput..

[33]  Paolo Gamba,et al.  Automatic Extraction and Identification of Lunar Impact Craters Based on Optical Data and DEMs Acquired by the Chang’E Satellites , 2015, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.