Zeyu E’s scientific contributions

... The clastic parent rocks of TJG and JGD were predominantly comprised of high-grade metamorphic rocks, characterized Table 1 Comparison and delineation of the Southeastern Depression of the Tarim Basin and adjacent areas (Modified form Zhao et al., 2020) Mb = Member Gr. = Group (The others of legends are the same as those in Fig. 1 Saccites-Piceites by high GZi indices (Figs. 9 and 10), and displayed northward, northeast and eastward paleocurrent direction which indicated that potential sources was Altyn Mountains (Fig. 1). The abundance of pyrite heavy minerals in the sandstones of the PL and the YM deposits was not authigenic but was associated with pyrite beds in the East Kunlun area, which proved that the Kunlun Mountains was the source (Yue and Zhou, 2022;Cong et al., 2023;Hu et al., 2023b) (Fig. 9). Theof these deposits. ...

Reference:

Sedimentary infill of Early-Middle Jurassic in the southeastern Tarim Basin and its constraints on the evolution of the Altyn Tagh Fault in the Northeast Tibet Plateau