DOI: 10.57760/sciencedb.14234
title: Isolation of primary remanent magnetization from Himalayan rocks: Insights from partially remagnetized Upper Cretaceous oceanic red beds in southern Tibet, China
title: Isolation of primary remanent magnetization from Himalayan rocks: Insights from partially remagnetized Upper Cretaceous oceanic red beds in southern Tibet, China

description: The file contains Figures S1 to S9 and Tables S1 to S11 to support the research presented in "Isolation of primary remanent magnetization from Himalayan rocks: Insights from partially remagnetized Upper Cretaceous oceanic red beds in southern Tibet, China".Figure S1. Normalized thermal decay curves.Figure S2. EDS analysis results of dots presented in Figure 4.Figure S3. First derivative of hysteresis loop measurements of (a) CM118 and (b) CM124.Figure S4. Isothermal remanent magnetization (IRM) acquisition and back-field demagnetization curves.Figure S5. Component analysis of the IRM acquisition curves by a single skewed component.Figure S6. Derivatives of the RTSIRM cooling curves for representative samples.Figure S7. Field-cooled and zero-field-cooled curves.Figure S8. The TRM is cooled to 10 K (blue squares) and warmed to 400 K (orange squares), providing a partial thermal demagnetization before cooling back to 10 K (blue triangles) and warming to 300 K (orange triangles).Figure S9. Equal-area projections of in-situ (a-c) and tilt-corrected (d-f) paleomagnetic directions of all specimens in the Cailangba section, after Yuan et al. (2021).Table S1. Thermal demagnetization data.Table S2. X-Ray diffractogram data.Table S3. Volume percent of minerals calculated from semi-quantitative analyses of XRD results.Table S4. Diffuse reflectance spectroscopy data.Table S5. Hysteresis loop data.Table S6. IRM acquisition curves and backfield demagnetization data.Table S7. Thermal demagnetization data of the three-component IRM and 150 mT IRM.Table S8. Low‐temperature RT-SIRM cycling data (Rewarming to 300 K).Table S9. Field-cooled and zero-field-cooled data.Table S10. RT-SIRM cycling, TRM cycling, ZFC-LTSIRM warming, and FC-SIRM warming data.Table S11. The TRM is cooled to 10 K and warmed to 400 K, providing a partial thermal demagnetization before cooling back to 10 K and warming to 300 K.
description: The file contains Figures S1 to S9 and Tables S1 to S11 to support the research presented in "Isolation of primary remanent magnetization from Himalayan rocks: Insights from partially remagnetized Upper Cretaceous oceanic red beds in southern Tibet, China".Figure S1. Normalized thermal decay curves.Figure S2. EDS analysis results of dots presented in Figure 4.Figure S3. First derivative of hysteresis loop measurements of (a) CM118 and (b) CM124.Figure S4. Isothermal remanent magnetization (IRM) acquisition and back-field demagnetization curves.Figure S5. Component analysis of the IRM acquisition curves by a single skewed component.Figure S6. Derivatives of the RTSIRM cooling curves for representative samples.Figure S7. Field-cooled and zero-field-cooled curves.Figure S8. The TRM is cooled to 10 K (blue squares) and warmed to 400 K (orange squares), providing a partial thermal demagnetization before cooling back to 10 K (blue triangles) and warming to 300 K (orange triangles).Figure S9. Equal-area projections of in-situ (a-c) and tilt-corrected (d-f) paleomagnetic directions of all specimens in the Cailangba section, after Yuan et al. (2021).Table S1. Thermal demagnetization data.Table S2. X-Ray diffractogram data.Table S3. Volume percent of minerals calculated from semi-quantitative analyses of XRD results.Table S4. Diffuse reflectance spectroscopy data.Table S5. Hysteresis loop data.Table S6. IRM acquisition curves and backfield demagnetization data.Table S7. Thermal demagnetization data of the three-component IRM and 150 mT IRM.Table S8. Low‐temperature RT-SIRM cycling data (Rewarming to 300 K).Table S9. Field-cooled and zero-field-cooled data.Table S10. RT-SIRM cycling, TRM cycling, ZFC-LTSIRM warming, and FC-SIRM warming data.Table S11. The TRM is cooled to 10 K and warmed to 400 K, providing a partial thermal demagnetization before cooling back to 10 K and warming to 300 K.