Continental China is a mosaic of numerous tectonic blocks, which amalgamated from
Neoarchean to Cenozoic broadly coeval with the cycles of global supercontinents such as …

In the present paper, we have compiled data on 565 layered and differentiated igneous
intrusions globally, documenting their (i) location,(ii) age,(iii) size,(iv) geotectonic setting,(v) …

Abstract The **arihamu Ni-Co deposit, located in the East Kunlun orogenic belt, northern
Tibet plateau, is the secondary largest Ni deposit in China and contains~ 157 million metric …

Abstract The Poyi magmatic Ni-Cu sulfide deposit is situated in the Beishan fold belt in the
northeastern rim of the Tarim craton. Many Permian magmatic Ni-Cu sulfide deposits, such …

Although it has been recently demonstrated that Cu isotope fractionation during mantle
melting and basaltic magma differentiation is limited, the behavior of Cu isotopes during …

Magmatic sulfide deposits can be subdivided into 1) Ni-Cu-PGE deposits, which have
relatively smooth mantle-normalized metal patterns, 2) Ni-Cu-(PGE) deposits, which are …

Oxygen fugacity is a key parameter in controlling the petrogenesis of mafic-ultramafic rocks
and their associated sulfide mineralization, especially in convergent settings. This study …

The Huangshannan mafic–ultramafic intrusion is a Permian Ni–Cu sulfide-bearing intrusion
in the southern margin of the Central Asian Orogenic Belt. The intrusion consists of an …

A close relationship between Ni–Cu–(PGE) sulfide deposits and magmatic conduit systems
has been widely accepted, but our present understanding still rests on empirical inductions …

The Huangshan mafic–ultramafic intrusion hosts a large Ni–Cu sulfide deposit and is
situated in the Northern Tianshan at the southern margin of the Central Asian Orogenic Belt …