Chemical Weathering Intensity as a Reliable Indicator for Southwest Summer Monsoon Reconstruction: Evidence From Clay Minerals of Qionghai Lake Sediments Since the Last Glacial Maximum.

MLA

Yu, Xiaoli, et al. “Chemical Weathering Intensity as a Reliable Indicator for Southwest Summer Monsoon Reconstruction: Evidence From Clay Minerals of Qionghai Lake Sediments Since the Last Glacial Maximum.” Geochemistry, Geophysics, Geosystems: G3, vol. 24, no. 7, July 2023, pp. 1–17. EBSCOhost, https://doi.org/10.1029/2023GC010900.

APA

Yu, X., Wang, G., Zhang, T., Ma, X., Zhang, X., Li, L., Li, Z., Guo, Z., Wei, Z., Wang, Y., & Zhou, S. (2023). Chemical Weathering Intensity as a Reliable Indicator for Southwest Summer Monsoon Reconstruction: Evidence From Clay Minerals of Qionghai Lake Sediments Since the Last Glacial Maximum. Geochemistry, Geophysics, Geosystems: G3, 24(7), 1–17. https://doi.org/10.1029/2023GC010900

Chicago

Yu, Xiaoli, Gen Wang, Ting Zhang, Xueyun Ma, Xiaomei Zhang, Lun Li, Zelong Li, et al. 2023. “Chemical Weathering Intensity as a Reliable Indicator for Southwest Summer Monsoon Reconstruction: Evidence From Clay Minerals of Qionghai Lake Sediments Since the Last Glacial Maximum.” Geochemistry, Geophysics, Geosystems: G3 24 (7): 1–17. doi:10.1029/2023GC010900.