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Palabras clave – provistas por la editorial

Southeast Guizhou; n/a; Nibao gold deposit; arsenopyrite; gold selenide; mineralization age; thermodynamic modeling; S)-oxides; Cu-Fe-Ni-S system; chlorargyrite; colloids; Fe-Sb(Te; pyrite; mustard gold; Mössbauer Effect; platinum; gold mineralization; nanoparticles; magnetite veins; dyscrasite; chloride complexes; calaverite; metalloid elements; maletoyvayamite; gold ore deposits; ligand surroundings; platinum-group elements; fractional crystallization; fluid regime; native gold; Southern Urals; monolithic and porous gold; Rb–Sr isotopic composition; Gaching ore deposit; antigorite serpentinites; Fennoscandian Shield; zircon U–Pb age; Ag; karst cavities; gold sulfoselenide; Yunnan–Guizhou–Guangxi “Golden Triangle” region; As)-oxides; distribution; sulfide minerals; Tl tellurates and antimonates; gold ore field; valleriite; gold; Tl oxides (avicennite); nucleation; drop-shaped inclusions; As; structural and surficial modes; Kolmozero–Voronya belt; gold source; S; Au; non-equal positions; ore genesis; XPS; liquid intermediates; crystal lattice; Chaoyangzhai gold deposit; Au-Sb(Te; Kagan ultramafic massif; deposition; invisible species; noble metals; in situ sulfur isotopes; Se; “invisible” gold; Oleninskoe deposit; ore-forming fluid; Tl carbonates