supported by the National Natural Science Foundation of China(Grant Nos.41873058 and 41462001);the Natural Science and Technology Foundation of Guizhou Province,China(Grant No.JZ[2015]2009)。
The Wuchuan-Sihui-Shaoguan(WSS)exhalative sedimentary pyrite belt in the southwestern part of the Qinzhou-Hangzhou(Qin-Hang)belt is the most important sulfur industry base in China.However,a wide range of metallogenet...
supported by the National Natural Science Foundation of China(Grant Nos.41072054,40672053,41462001)
Global abrupt climate change from Marinoan snowball Earth to greenhouse Earth, recorded as cap carbonate overlain on diamictite, had shed the first light on Cambrian bio-radiation. The most documented cap carbonate se...
supported by National Science Foundation of China (Nos. 41072054, 40963002)
The Meishucun section in Yunnan is the stratotype section for stratigraphic correlation of the Lower Cambrian strata across the Yangtze Block. Known for enriched small shelly fossils, it is a prominent section for inv...
supported by National Natural Science Foundation of China(Grant Nos.40963002;40672053&40803016)
The Lower Cambrian on the Yangtze Platform in South China (internationally equivalent to the Nerreneuvian and 2nd series of the Cambrian) is valuable for understanding the early evolution of life, the global biogeoc...
supported by the National Natural Science Foundation of China (40372057 and 40772076);the SINOPEC Project (G0800-06-ZS-319);the China Geological Survey (CGS) project (1212010611802)
A SHRIMP U-Pb zircon age of 1437±21 Ma was obtained for a recently discovered K-bentonite bed in the Tieling Formation,situated northeast of Beijing at the boundary between Liaoning and Hebei provinces,on the norther...
the Notional Natural Science Foundation of China (Grant No.40525010)
The Global boundary Stratotype Section and Point (GSSP) for the base of the Hirnantian Stage (the latest stage of the Ordovician System) is defined at a point 0.39m below the base of the Kuanyinchiao Bed in the Wangji...
the National Natural Science Foundation of China(Grant No.49802002);the State Key Project of Sequence Stratigraphy and Earth Rhythms ; the Lab of Earth Surface Systems of Hubei Province.
More than 20 K-bentonite beds were discovered from the Wufeng Formation and the lowest Longmaxi Formation in two sections, both adjacent to the Ordovician-Silurian (O-S) bound-ary and located in Tongzi, Guizhou Provin...