Results 151 to 160 of about 351,119 (215)
Mantle oxidation by sulfur drives the formation of giant gold deposits in subduction zones. [PDF]
He DY +10 more
europepmc +1 more source
Copper sulfide deposition and remobilisation triggered by non-magmatic fluid incursion in the single-intrusion Tongchang porphyry system, SE China. [PDF]
Liu X, Richard A, Pironon J, Yang K.
europepmc +1 more source
Magmatic-hydrothermal fluid evolution of the tin-polymetallic metallogenic systems from the Weilasituo ore district, Northeast China. [PDF]
Gao X +6 more
europepmc +1 more source
Transient non-soluble noble metal transport in hydrothermal ore systems. [PDF]
Cano N +4 more
europepmc +1 more source
Petrogenesis of the granitoids related to skarn-type mineralization in the Nyainqentanglha Metallogenic Belt, Tibet. [PDF]
Yangang F +6 more
europepmc +1 more source
Porphyry-Cu Deposits of Turkey
Turkey, located within the western Tethyan-Eurasian Belt contains numerous porphyry copper deposits formed by the subduction, collision and post-collisional events during the closure of NeoTethys Ocean between the latest Cretaceous and late Miocene. These porphyry systems and associated epithermal and skarn deposits are associated with the subduction ...
Kuşcu, İlkay +2 more
openaire +3 more sources
Porphyry deposits of the Urals: Geological framework and metallogeny
Most of the Cu (± Mo,Au) porphyry and porphyry-related deposits of the Urals are located in the Tagil-Magnitogorsk, East-Uralian Volcanic and Trans-Uralian volcanic arc megaterranes.
Olga Plotinskaya +2 more
exaly +3 more sources
Geochemistry of Porphyry Deposits
Porphyry ore deposits typically form in convergent plate margin or postsubduction settings at depths of 1-6 km. Oxidized hydrous melts derived from the metasomatized mantle wedge transport Cu, Au, Mo, and other metals to upper-crustal magma chambers ...
D.R. Cooke +3 more
openaire +2 more sources

