Key Points:Variations of environmental magnetic parameters of the Miocene sediments were established in the Subei Basin q The increased bulk susceptibility, SIRM, ARM, and HIRM were related to tectonic uplift induced provenance change since 13.7 Ma q The parameters of susceptibility ratios, redness and S ratio are climate-dependent, indicating a warmest and humid climate during the middle Miocene Optimum q Abstract: Thick sediments from foreland basins usually provide valuable information for understanding the relationships between mountain building, rock denudation, and sediment deposition. In this paper, we report environmental magnetic measurements performed on the Miocene sediments in the Subei Basin, northeastern Tibetan Plateau. Our results show two different patterns. First, the bulk susceptibility and SIRM, ARM, and HIRM mainly reflect the absolute-concentration of magnetic minerals; all have increased remarkably since 13.7 Ma, related to provenance change rather than climate change. Second, the ratios of IRM 100mT /SIRM, IRM 100mT /IRM 30mT , and IRM 100mT /IRM 60mT , together with the redness and S ratio, reflect the relative-concentration of hematite, being climate-dependent. Their vertical changes correlate in general with the long-term Miocene climatic records of marine oxygen isotope variations, marked by the existence of higher ratios between 17 and 14 Ma. This may imply that global climate change, rather than uplift of the Tibetan Plateau, played a dominant role in the long-term climatic evolution of the Subei area from the early to middle Miocene.