The paper gives a brief description of the metallogenic types and distinguishing features of mineralization connected with the Emeishan mantle plume.

New advances in geochronologic study related to Emei mantle plume and their significance;

The picrite field, located in the southwest of Emeishan continental flood basalts (ECFB) and with the center in Lijiang—Dali—Panzhihua triangular area, is about 5×104 km2 and regarded as the axial area of the Emei mantle plume.

Chinese carlin-type gold deposits are mainly located in the "Yunnan -Guizhou -Guangxi", "Sichuan-Gansu-Shanxi" and the west of Yunnan region, which are located in the area of Emei mantle plume activity.

Dynamic Change of Chemical Composition of Rain in 1998 on Mt.Emei;

Study and Estimation of Wild Coptis Resource in Mt.Emei;

Wild Medicinal Resources of Fern Plant in Mt.Emei and Their Exploitation and Utilization;

Petrology and Geochemistry of the Late-Stage Acidic Volcanic Rocks of the Emeishan Large Igneous Province;

Discovery of High-Os Picrites in the Large Emeishan Igneous Province and Its Geological Significance;

~(40)Ar/~(39)Arand U-Th-Pb dating for native copper mineralizations of two stages from the Emeishan flood basalts in northeastern Yunnan Province, China;