10.4231/FR4M-PF07
04/30/2024
This dataset comprises XRF, XRD, and Microprobe data collected as part of the SAND-E 2019 field campaign to Þórisjökull, Iceland in addition to the locations of candidate glaciovolcanic edifices on Mars.
geochemistry glacier Iceland Igneous petrology Mars Planetary Science volcano
10.4231/FAVY-1K42
ANGSA Science Team , Charles Shearer , James Mcfadden , Lindsay Keller , Michelle Thompson , Richard Morris , Roy Christoffersen
09/12/2024
Relevant transmission electron microscopy images and energy dispersive x-ray spectroscopic chemical data used to evaluate space weathering and mineralogy of regolith found in Apollo core sample 73002.
Moon Planetary Science Space Transmission Electron Microscopy
10.4231/RMZX-4G15
07/14/2023
The dataset contains the data products developed in the mapping of Mars' northern polar spiral troughs. This included 3D depth maps of trough migration paths from radar data, and slope, azimuth, and wavelength measurements for surface troughs.
10.4231/18M6-GC48
11/30/2023
The dataset contains the data products developed in the mapping of Mars' northern polar spiral troughs. This included 3D depth maps of trough migration paths from radar data, and slope, azimuth, and wavelength measurements for surface troughs.
10.4231/0VSJ-A287
Austin M. Blevins , Caleb I. Fassett , David A. Minton , Jun Du , Ya-Huei Huang
10/04/2024
This repository includes the shape files and power spectral densities of all the crater outlines as well as python scripts to generate the synthetic crater outlines.
10.4231/R7DR2SP6
Andrew Hesselbrock , David Minton
05/01/2018
Coupled ring-satellite systems fall into three distinct dynamical regimes, “Boomerang,” “Non-Boomerang,” and “Torque-Dependent.” This publication includes data to reproduce figures as well as the version of RING-MOONS used to produce all data.
10.4231/R79C6VMX
Bryan Howl , Caleb Fassett , David Minton , James Richardson , Masatoshi Hirabayashi
12/22/2017
Data to reproduce figures and movies for the paper "Topographic degradation by impact cratering on airless bodies is dominated by diffusive erosion from distal ejecta."
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