Supporting Information for Multistage activation of intraplate strike-slip faults deeply buried in the Yangtze Block: implications to the tectonics of the Qinling Orogen

Published: 22 July 2025| Version 1 | DOI: 10.17632/6n9tf8cn2j.1
Contributor:
Yanxian Zhu

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The supporting information contains detailed figures and data used in this study. Figure S1. Temporal constraints on dextral transpressional fault activity within the Qinling Orogen and northern Yangtze Block during the continental collision between the North and South China blocks. Table S1. Structural characteristics of veins within the Maokou Formation from the Fangniuba and Tailai areas along the Houba-Pengan-Fengdu Fault. Table S2. REEY data of the limestone and fracture-filling carbonate cements from the outcrop and core samples within the Houba-Pengan-Fengdu Fault. Table S3. Spot analysis data for in situ U-Pb dating of fracture-filling carbonate cements from outcrop and core samples along the Houba-Pengan-Fengdu Fault.

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Rare Earth Element, Structural Analysis, Uranium-Lead Dating

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