The impact of orbital parameters on the climate of China in the Holocene is simulated from 1lkaBP to 0kaBP with an interval of lka using National Center for Atm
By using daily air temperature and precipitation data, and the weather phenomena data of daily snowfall from 98 meteorological stations over the Qinghai-Tibetan
Platinum group element (PGE) mineralization is mostly related to mafic-ultramafic complexes of the dominant magmatic deposit type. Mineralization of this type m