Fluid migration and widespread remagnetization in the Dabashan fold and thrust belts, China

To better understand the processes of fluid migration in orogenic zones and associated chemical remagnetization, we have conducte detailed magnetic, petrographic, and Strontium (Sr) isotope studies in an important orogenic belt of China, the Jurassic Dabashan fold and thrust belts. The result of this study has been submited to the Journal of Geophysical Research-Solid Earth. These materials contain two data tables for the 87Sr/86Sr (Table S1) and clay data (Table S2), which are two important data for the Figure 8 and Figure S1.