Source data (unprocessed) for "The influence of variable host rock cohesion and magma viscosity on intrusion-fault interaction: Insights from laboratory models" (Greiner et al., 2025, JGR: Solid Earth)
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Unprocessed surface deformation data for analogue experiments related to the research article "The influence of variable host rock cohesion and magma viscosity on intrusion-fault interaction: Insights from laboratory models" (Greiner et al., 2025; JGR: Solid Earth; doi: https://doi.org/10.1029/2024JB029870 ) Contents: Unprocessed surface deformation data of the 20 experiments presented in the main text of the article (four cameras for each experiment) pressure data (necessary to determine beginning of the intrusion process) MicMac scripts used to process the data information for georeferencing (file GCP.xml for each experiment) Matlab-scripts to plot the pressure curves for experiments with syrup and oil (differ in frequency of measurements) Information on the compaction of the model crust for each experiment (information on thickness and average density of model crust) Photos of the laboratory journal Related work: Research article available at: https://doi.org/10.1029/2024JB029870 Processed data available at: https://doi.org/10.5281/zenodo.14935450 Data of repeat experiments of the same article available at: https://doi.org/10.5281/zenodo.14937427 For instructions on how to process and plot the surface data, see Galland et al (2024; doi: https://doi.org/10.31223/X5QD7Q)
本数据集为与研究论文《可变围岩黏聚力与岩浆黏度对侵入-断层相互作用的影响：来自实验室模型的启示》（Greiner等，2025；《地球物理学研究杂志：固体地球》（JGR: Solid Earth）；DOI：https://doi.org/10.1029/2024JB029870）相关的类比实验未处理地表形变数据。 数据集内容： 1. 论文正文中展示的20组实验的未处理地表形变数据（每组实验配备4台相机）； 2. 用于确定侵入过程起始时刻的压力数据； 3. 用于处理该数据集的MicMac脚本； 4. 每组实验的地理配准信息（每组实验对应GCP.xml文件）； 5. 用于绘制糖浆与石油类实验压力曲线的Matlab脚本（两类实验的测量频率存在差异）； 6. 每组实验的模型地壳压实相关信息（包含模型地壳厚度与平均密度数据）； 7. 实验日志照片。 相关成果： - 研究论文访问链接：https://doi.org/10.1029/2024JB029870 - 已处理数据集访问链接：https://doi.org/10.5281/zenodo.14935450 - 该论文重复实验数据集访问链接：https://doi.org/10.5281/zenodo.14937427 - 地表数据处理与绘图操作指南参见Galland等（2024；DOI：https://doi.org/10.31223/X5QD7Q）
