Geology, pressure-temperature-composition conditions of hydrothermal fluids, and metallogenesis of the Late Jurassic Mahe and Matoushan Mo deposits in the North Qinling terrane, Central China

• The Mahe and Matoushan are two Late Jurassic collision-type porphyry Mo deposits. • Metallogenic fluids mainly originated from magmatic water. • Metallic components were primarily derived from Late Mesozoic magmas. • CO 2 -rich-H 2 O-NaCl ± CH 4 fluid systems formed at 69–262 MPa and 6.9–9.7 km. • Phase separation, changes in redox state, and pH are critical factors for Mo precipitation. The Mahe and Matoushan Mo deposits, as representatives in the North Qinling terrane, are insufficiently understood in terms of their geology, mineralization ages, fluid systems, and metallogenesis. Molybdenum mineralization at Mahe and Matoushan primarily occurs as veins and veinlets within the quartz schist of the Meso-Neoproterozoic Sichakou Formation and actinolite schist of the Meso-Neoproterozoic Guangdongping Formation, respectively. The metallogenic processes can be categorized into three stages: quartz-molybdenite veins (stage Ⅰ), quartz-molybdenite-polymetallic sulfide veins or veinlets (stage Ⅱ), and calcite-quartz ± fluorite veins (stage Ⅲ). Four predominate inclusion types are identified, including the type 1 H 2 O-CO 2 -NaCl ± CH 4 inclusions, type 2 CO 2 ± CH 4 inclusions, type 3 solid-bearing multiphase inclusions, and type 4 H 2 O-NaCl inclusions. Fluid inclusion studies show that initial mineralizing fluids of stage Ⅰ are medium to high temperature (peaking at ca. 240–340°C), low to medium salinity (2.2–14.8 wt% NaCl eqv.), medium density (0.747–0.993 g/cm 3 ), relatively oxidized, and CO 2 -rich (X CO2 = 0.04–0.39) H 2 O-CO 2 -NaCl systems, formed at about 73–222 MPa (corresponding to a paleodepth of 7.3–8.2 km). The main ore-forming fluids of stage Ⅱ are featured by medium to high temperature (peaking at ca. 240–380°C), low to high salinity (2.4–45.7 wt% NaCl eqv.), medium to high density (0.713–1.189 g/cm 3 ), reduced, and CO 2 -rich (X CO2 = 0.03–0.76) H 2 O-CO 2 -NaCl ± CH 4 systems. The estimated trapping pressures at Mahe and Matoushan are 69–208 MPa and 133–262 MPa, respectively, while the corresponding mineralization paleodepths are 6.9–7.7 km and ∼ 9.7 km. The stage Ⅲ barren fluids are defined as low temperature (peaking at ca. 140–180°C), low salinity (0.4–2.2 wt% NaCl eqv.), medium density (0.832–0.940 g/cm 3 ), and CO 2 -poor-H 2 O-NaCl systems. Isotopic analyses of H, O, and C in quartz and calcite reveal that the metallogenic fluids of stage Ⅰ and Ⅱ were mainly from magmatic water, with massive meteoric water mixing at shallow crustal levels during stage Ⅲ. Sulfide S and Pb isotopes indicate that the metallic components predominantly originated from Late Jurassic granitoids. Immiscibility (phase separation) and remarkable transitions in redox state (from oxidized to reduced) and pH (from alkaline to acidic) of fluid systems were key factors for Mo precipitation. Molybdenite Re–Os dating provided the Late Jurassic isochron ages of 145.3 ± 3.7 Ma and 147.7 ± 4.7 Ma for Mahe and Matoushan, respectively, suggesting a post-collisional tectonic regime. Compared to porphyry Mo systems globally, the Mahe and Matoushan Mo deposits are classified as collision-type porphyry deposits, differing from rift- and subduction-related systems.