Fig. 2: Lithology, magnetic stratigraphy and paleoclimate proxies of the Ashigong Formation in the Guide Basin, NE Tibet.
From: Moisture variability in northeast Tibet following the middle Miocene Climate transition
(A) redness (a*). (B) magnetic susceptibility (MS). (C) Mn/Fe ratios. (D) illite content, and (E) smectite/(illite+chlorite) ratios. Magnetic stratigraphy, redness and MS data are from Wang et al.32.
