Earth-Moon deep quakes triggered by orbital variability: The dataset

This dataset is linked to the paper "Earth-Moon deep quakes triggered by orbital variability".

There was present a correlation between deep moonquakes, deep earthquakes, and the main orbital parameters of the Sun-Earth-Moon system. The study showed that deep seismicity arises from the orbital movements of specific orbital parameters. The results also suggest that the layers where the deep quakes occur on the Earth and the Moon have similar seismological behavior, under the same stress field. The main reason for the evolution of the stress field is related to orbital variability. The periodic shear heating, dependent on strain rate and stress field, which changes with orbital variability, may trigger the deep quakes.

Steps:
1. Understanding the occurrence of moonquakes. Data in 'Data_moonquakes.xlsx';
2. Production of time series of deep moonquakes, deep earthquakes, and orbital parameters. Daily Values. All series are arranged in 'Parameters_Timeseries.xlsx';
3. Analysis of time series by wavelet transform. Python script in 'wavelet_Transform.ipynb';
4. Analysis of time series by wavelet coherence. R script in 'wavelet_r_coehency.txt'. Data in 'deep_moon.csv' and 'deep_earth.csv';
5. Statistical analysis. Python script in 'statistical analysis.ipynb';

6. Removal of the time series trend for clustering performance in machine learning. Python script in 'trend_timeseries.ipynb';
7. Plot of deep quakes as a function of depth. Data in 'Depth_count.xlsx';
8. Lunar mantle strain rate model. Data in 'density_moon.txt'. Python script in 'moon_density.ipynb'.