Abstract The Aqishan-Yamansu belt in the Eastern Tianshan (NW China) contains many
intermediate to felsic intrusive rocks and spatially and temporally associated Fe (-Cu) …

Abstract In the Zajkan Pb–Zn–Cu (Au–Ag) deposit of the Tarom–Hashtjin metallogenic belt
(THMB), northwest Iran, mineralization occurs as quartz-base metal sulfide veins hosted by …

Abstract The Xinjiang Uygur Autonomous Region in NW China occupies around 1/6 of the
total China land size, and contains components of both the Central Asian Orogenic Belt …

Abstract The Aqishan-Yamansu Fe-Cu-Au metallogenic belt in the Eastern Tianshan, NW
China, hosts numerous Fe and Fe-Cu deposits that may have different genetic models, such …

Abstract The Abbasabad epithermal Pb–Zn–Cu deposit is located in the Tarom–Hashtjin
Metallogenic Belt (THMB), northwest Iran. Mineralization occurs as quartz-base metal sulfide …

Abstract The Tuwu deposit (557 Mt at 0.58% Cu) is the most typical and economically
significant one of several porphyry copper deposits in the Dananhu-Tousuquan Arc Belt …

The formation of the Eastern Tianshan orogen (northern Xinjiang, NW China) with a number
of EW-trending mineralization belts was closely linked to the evolution of the Junggar and …

Geochemistry of sulfides is widely used to constrain sources and ore-forming processes of
various mineral deposits. However its application on Fe–oxide Cu–Au (IOCG) deposits is not …

Chlorite is one of the most widely developed minerals in propylitic alteration around
porphyry deposits and can be used to investigate element transport and enrichment …

The Shaquanzi deposit is an important Fe-Cu deposit in the Yamansu Fe mineralization belt,
Eastern Tianshan. Three types of magnetite were distinguished based on the textural and …