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Thermal conductivity of hydrogen-rich ringwoodite under high temperatures and high pressures: Implications for the Martian thermal evolution

NIAID Data Ecosystem2026-05-02 收录

行星热演化模拟

矿物高温高压物性

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Supplementary figure

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创建时间：

2025-05-06

行星热演化模拟

天体磁场发电机制

Ganymede is the only known moon with an active dynamo today. Previous studies interpret Ganymedeâs dynamo as arising from convection in a metal core that formed billions of years ago. However, Ganym

DataONE2026-04-23 更新70

Heat flux and temperature at depth beneath InSight landing site through time

行星热演化模拟

火星地壳热物理

The heat flux and thus temperature gradient of the Martian crust is critical for comparison with measurements of crustal properties. This allows for constraints upon the inferred thermal history of Ma

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Large Scale Volcanism and the heat-death of terrestrial worlds

行星火山活动

行星热演化模拟

The files herein are used to generate the main and SI figures in the GRL paper: Title: Large Scale Volcanism and the heat-death of terrestrial worlds Authors: M.J. Way, Richard E. Ernst, Jeffrey D.

NIAID Data Ecosystem30

NUCM2 Monte Carlo results - wet crust and dry mantle rheology

行星热演化模拟

火星地壳流变学

Monte Carlo results for NUCM2 simulations (Figure 9b)Rheology = dry mantle and wet crust, diffusion creep Files: Each line of the files (scores, thickness, enrichment factor and crustal radio

Figshare2018-02-21 更新70

Output data and relevant model information for Influence of Megaregolith on the thermal evolution of Mercury’s silicate shell

行星热演化模拟

水星表面组成

This data set contains the model output data used to draw the graph for the paper. All the output data are stored in a. XLS file, which is divided into sheet-1 and Sheet-2. For reasons of intellectual

科学数据银行2021-10-18 更新50

Thermal conductivity of hydrogen-rich ringwoodite under high temperatures and high pressures: Implications for the Martian thermal evolution

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