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.

为深入解析造山带内流体运移过程及其伴生的化学重磁化作用，我们在中国重要造山带——侏罗纪大巴山褶皱冲断带中开展了详尽的磁学、岩石学及锶（Strontium, Sr）同位素研究。本研究成果已提交至《Journal of Geophysical Research-Solid Earth》（地球物理研究杂志-固体地球）。本次数据集包含两份数据表：87锶/86锶比值数据表（表S1）与黏土矿物数据表（表S2），二者均为图8及补充图S1的核心支撑数据。