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The article focuses on a research paper discussing the geology of the Yanshannian porphyry molybdenum-pollymetallic metallogenic belt on the western margin of Yangtze Craton in Southwest China. It discusses the factors affecting the mineralization of the deposit, that takes place in Indosinian post-collision stage, including the Yanshanian new tectonic activities, upwelling of mantle fluid and melting of thickened lower crust.

The article discusses the research study conducted on Laba Yanshanian Porphyry Molybdenum (- Copper) Deposit in Shangri- La, NorthWest Yunnan, China to examine its alteration, mineralization and its genesis. It mentions that geological background of the deposit including quartz diorite porphyry, granodiorite porphyry and other intermediate-acid magmatic rocks. It also informs about early potassic alteration including skarnization and hornfels, and porphyry type mineralization.

The article presents a study focusing on Ore-related Granites and Tectonic Settings of the Qian'echong and Tangjiaping Porphyry Molybdenum (Mo) deposits in Dabie, East China. Topics discussed include identical ages of Monzogranite granite rocks and granite porphyry found in the Porphyry Mo deposits, Strontium (Sr)-Neodymium (Nd)-Lead (Pb) isotopic characteristics exhibited by granitesin Qian'echong deposit and occurrence of ultrahigh pressure minerals in the Qian'echong and Tangjiaping deposit.

The article discusses a study on the application of technology of spectrum induced polarization (SIP) method in No. 534 molybdenum-uranium deposit. It mentions that in cole-cole model of SIP data processing, the frequency domain curves of appearance complex resistivity is affected by electro migration. It also mentions that SIP method can be applied in uranium and multimetallic deposit. It also mentions that uranium and metallic mine shows high resistivity and polarizability.

The article presents a study which discusses characteristics of highly differentiated granite and metallization of tungsten-tin, rare and rare earth metal in the eastern Nanling region, China. Topics discussed include formation of rare earth metals by granite magmatic activity, formation of muscovite type ore deposits, and the formation of garnet type ore deposits, which is related to tungsten and molybdenum ore deposits.

The Leimengou Mo deposit is one of the typical porphyry deposits in the East Qinling molybdenum ore belt. The Mo mineralization mainly hosts in the Leimengou intrusion, with minor by the gneiss of Archean Taihua Group. The Leimengou intrusion is composed of granite porphyry and monzonitic granite porphyry. Zircon U–Pb LA-(MC)-ICP-MS dating of the two rocks yield the same age of 131 ± 0.6 Ma (N = 23, MSWD = 1.6), consistent with 132 ± 2 Ma of Mo mineralization age obtained by the Re–Os method. The Leimengou intrusion is peraluminous (A/CNK = 1.06–1.28) and high-K calc-alkaline series (K2O + Na2O = 7.84%–9.07%). The REE and trace elements are enriched in large ion lithophile elements (LREE, K, Rb, Ba, Sr, Th and U), and depleted in high-field strength elements (HREE, Nb, Ti and P), with moderately negative abnormal of Eu. Both granite porphyry and monzonitic granite porphyry show a large variation in zircon Hf isotopic compositions with εHf(t) values of −27.9 to −16.9 and −26.0 to −15.2, and two-stage model ages of 2259 to 2946 Ma and 2149 to 2827 Ma, respectively. Whole rock geochemistry and zircon Lu–Hf isotopic compositions suggest that the Leimengou intrusion was derived mainly from an ancient continental crust (probably Archean Taihua Group), with the addition of mantle-derived components. [ABSTRACT FROM AUTHOR]

The article presents a study to explore the geological characteristics and metallogeny of Qiushuwan porphyry Type copper-molybdenum (Cu-Mo) deposit in East Qinling, China. Topics include cyptoexplosive breccia type and porphyritic type mineralization in the region, migmatization of the mantle and crust resulting in copper and molybdenum formation, and formation of minerals in three periods, first is pyrrhotite, magnetite, and molybdenite followed by quartz-sulfide and calcite-barite-quartz.

The article offers information on the uranium ores in South-East Russia with reference to its geodynamics. Topics discussed include deposits of gold-brannerite and fluorine-molybdenum-uranium formations near the uranium ore-nodes, uranium mineralization in sialic rocks undergoing potassium-silicic metasomatic transformations, and synchronism of the mineralization process present in molybdenum and fluorite.

The article offers information on a study conducted on the Suyunhe Porphyry Molybdenum deposit in West Junggar, Xinjiang in China related to its ore-forming fluid. Topics discussed include Molybdenum mineralization occurring in granite porphyry rocks, the presence of quartz hydrogen and oxygen isotopes in the early formed fluids indicating the fluid containing magmas, and granite bodies at the Burluk metallogenic belt.

The article offers information on the molybdenum polymetallic metallogenic regularity and prediction of the mineral field in Jinduicheng-Huang Longpu in China. It mentions that the lithologic interface control happens during the molybdenum mineralization. It mentions about the combination of lead and zinc in the geochemical development of the molybdenum and lead.

The article offers information on the geological features of the porphyry deposit of Jiama in Tibet, China. Topics discussed include scientific and economic significance of Jiama porphyry at Gangdese metallogenic belt due to the presence of copper metal reserves, molybdenum, and silver reserves, Copper-Molybdenum ore found in bathy-hidden porphyry, and disseminated ore and veinlet ore as the main types of ores found in the porphyry.

The article focuses on a study conducted to determine the geological significance and geochemistry feature of ore-forming granites in Caosiyao molybdenum deposit. Topics discussed include composition of ore-forming parent rock includes quartz porphry, porphyaceous granite, and granite porphyry, characterization of Caosiyao granite rock mass by high potash, acidity, and aluminum, and testing of Caosiyao granite using petrochemistry, factors of granite porphyry, and trace-rare element chemistry.

The article presents a study to determine ages of rhenium (Re)-osmium (Os) and uranium-lead of the Sifangdianzi molybdenite (Mo) deposit in Central Jilin Province, northeast China. Topics discussed include gangue minerals present in Sifangdianzi Mo like quartz, feldspar and biotite, development of wall-rock alteration including silicification, kaolinization and chloritization, and zircons from monzogranite of the Sifangdianzi Mo.

The article presents a study to analyze molybdenite rhenium (Re)-osmium dating results of the Checangyu molybdenum (Mo) deposit to understand the timing of Gold-Mo mineralization in China's Xiaoqinling district. Topics discussed include occurrence of molybdenite as coarse-grained and radial aggregates in altered granite, Re contents in molybdenite, and mineralization of the Checangyu Mo deposit.

The article presents a study to investigate zircon uranium-lead geochronology of the granites obtained from Xiaoliugou tungsten- molybdenum deposit in north Qilian which is one of the most important tungsten metallogenetic belt in northwest China. Topics discussed include zircon grains of monzogranite and granodiorite, analysis of microphotographs of the zircons for the study, and location of orebody in monzogranite and its exocontact zone.

The article discusses the research study to examine the evolution of granitic magmas and implications for Molybdenum (Mo) deposit formation within the Luanchuan Metallogenic Belt, Eastern Qinling Orogen, Central China. Topics discussed include Zircon Uranium (U)? lead (Pb) dating of lithologically distinct plutons, Pb isotope compositions of pyrites that were coprecipitated with molybdenite, and multiple stages of magmatic evolution.

The article discusses the research study conducted to examine the geological characteristics and Molybdenite (Mo) Rhenium (Re)-Osmium (Os) isotopic dating of the Doupo Mo Deposit, Dabie Orogen, Eastern China. It reveals the hydrothermal alteration types of wall rocks and main ore-forming types including disseminated, veinlet, stockwork and laminated molybdenite mineralizations. It also mentions the use of main metallogenic stage of molybdenite samples in Re-Os isotopic dating.

The article discusses the study conducted to examine the Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS) Zircon Uranium (U)?Lead (Pb) and Molybdenite Rhenium (Re)?Osmium (Os) isotopic dating of the Tungsten Deposits in the Dengfuxian Tungsten (W)?Tin (Sn) Orefield, Eastern Hunan Province, South China, and their Geological Implications. It reveals that deposits are related to mesozoic granitic intrusions. Also discusses the mineralization of Dengfuxian tungsten deposits.

The article discusses the research study that examines the geological characteristics and origin of the Hashitu molybdenum deposit, located in Inner Mongolia, China. It reveals geological setting of the deposit having the molybdenum grade of its ores within a Late Paleozoic accretion orogenic belt between the West Lamulun River fault and the Hegenshan fault (suture). It further mentions the ore district have same magma that undergo same rock forming process.

The article presents a study focusing on the geology and genesis of the Donggou Porphyry Molybdenum Deposit in Henan Province in Central China. It states that the mineralization process in the Donggou Porphyry Molybdenum Deposit can be divided into two magmatism periods including the late magmatic period and the hydrothermal period. It discusses the geochronological data which suggests that granite porphyry and mineralization occurred in early Cretaceous period.

The article presents a study conducted to investigate mineralogical characterization of the 460 uranium-molybdenum polymetallic deposit situated in Guyuan Area, Hebei Province, China. Topics discussed include three types of ores found in the region such as black-blue disseminated ore, black-blue disseminated ore and red vein like ore; two stages of uranium mineralization such as early disseminated stage and superimposed vein type stage and techniques used such as scanning electron microscopy.

The article discusses relationship between porphyry copper occurrences, amount of exploration in magmatic belts and crustal preservation levels of Central Tethys Region of Turkey, Iran and western Pakistan. It mentions that the study was performed to delineate areas as permissive tracts for occurrence of porphyry copper-molybdenum (Cu-Mo) and copper-gold (Cu-Au) deposits, and also to provide estimates of Cu, Mo, and Au contained in undiscovered porphyry deposits.

The article focuses on a study on spatial distribution of rhenium (Re) in the Luoboling porphyry copper-molybdenum (Cu-Mo) deposit in Shanghang, China. Topics discussed include use of inductively coupled plasma mass spectrometry (ICP-MS) technology in the study, correlation of grades of Re and Mo in ores with the Luoboling porphyry Cu-Mo deposit, and leaching and recrystallization of rhenium caused by phyllic overprinting.

The article discusses a study on ore-forming fluid of Shiyaogou porphyry molybdenum deposit in Henan Province, China. Topics discussed include use of fluid inclusions stages and laser Raman technique in the study, types of fluid inclusions containing sodium chloride, water and carbon dioxide, and fluid boiling as dominant factor in formation of molybdenum deposits.

The article discusses a study that focuses on the geochemical and diagenetic characteristics of magmatic rock in Qiushuwan copper-molybdenum ore district of Eastern Qinling, China. Topics discussed include variation in silica and alumina content when onzonitic granite is ignited, normalized distribution of rare earth elements and derivation of granitic porphyry through mantle-derived magma due to tectonic stress.

The article discusses metallogenic chronology of the Shierpai molybdenum polymetallic deposit in Wuping, Fujian and highlights its geological significance. Topics include association of ore body of Shierpai molybdenum polymetallic deposit with metamorphic rock, correlation between ore-bearing biotitic granite and molybdenite, and a study on isotopic geochronology of the biotitic granite and molybdenite revealing a biotitic granite zircon.

The article discusses the geology and geochemistry of Makeng iron and molybdenum (Fe-Mo) Deposit, Fujian, China. Topics include Juzhu-Dayang granite found to be weak peraluminous-metaluminous granite, mineral assemblages consisting of minerals including pyroxene, garnet and bustamite, and the ore-forming fluids of the skarn stage mainly derived from magmatic water.

The article offers information on the research "Characteristics of Ore-forming Fluid in the Baoxingchang Porphyry Cu-Mo-Au Deposit, Western Yunnan, China" by Sun Nuo and colleagues. Topics discussed include characteristics of mineralized veins, systematic microthermometric studies on fluid inclusions of quartz, and salinity and temperature characteristics of the ore genesis.

The article focuses on the research "Porphyry Mo Mineralization in Different Tectonic Setting: Indication from Fluid Inclusions in Shapinggou and Zhilingtou Mo Deposits, China" by Ni Pei. It mentions the stages of hydrothermal alteration and mineralization at Shapinggou which includes ore-barren quartz veins with silicification, quartz-molybdenite veins, and quartz-polymetallic sulfide veins. It presents ore fluid features and tectonic setting of the Zhilingtou deposit.

The article offers information on the research "The Curves of Seven REE and Their Geological Significances of Porphyry Mo (Cu) Deposit of Chengba, Tibet, China" by Song Xuebing and colleagues. It concludes that the curve types of seven rare earth elements (REE) which significance is clearly useful in determining the successions of intrusive, interpreting the genesis and evolution of magma as well as analyzing the process of mineralization.

The article offers information on the research "Molybdenite Re-Os Isochron Age of the Huoshenmiao Mo Deposit in Luanchuan Henan Province, China and Its Geological Implications" by Wang Sai and colleagues. It mentions the determination of the mineralization age and clarification of the relationships with Nannihu-Sandaozhuang and Shangfanggou molybdenum deposits. Topics discussed include tonalite and granite porphyry, polymetallic pyrite deposits and silver-lead-zinc deposits, and intrusion.

The article offers information on the research "Geology, Geochemistry, and Genesis of the Tongcun Porphyry Mo (Cu) Deposit, NW Zhejiang Province, China" by Tang Yanwen and colleagues. Topics discussed include granodiorite porphyry, molybdenum-copper mineralization, and mineral assemblages and fluid inclusion. Also mentioned are ore minerals including molybdenite, chalcopyrite, and pyrite; microthermometry and isotopic analysis; and ore genesis.

The article offers information on the research "Petrogenesis of Granite complex in the Jiudingshan porphyry Cu-Mo Deposit, Western Yunnan, China: Constraints from Geochronology, Geochemistry and Sr-Nd-Hf Isotopes" by Wang Rong and colleagues. Topics discussed include geochemical compositions of the rock, isotopic analysis of hafnium isotope zircon uranium-lead dating, and rock formation due to crust-mantle interaction.

The article offers information on the research "The Geochemical Characteristics and Prospecting Target of the Manley?Mandah Copper-molybdenum Deposit in Omnogovi Province of Mongolia" by Wang Wei and colleagues. Topics discussed include the mining geological characteristics of Manley?Mandah Copper molybdenum metallogenic belt, the adakitic characteristics of the granodiorite rocks, and the Hercynian porphyry Copper Molybdenum deposit.

The article offers information on the research "Metallogeny Study of Molybdenum Deposits in Jiaodong Mesozoic Metallogenic Province, China" by Liu Zhenjiang and colleagues. Topics include metallogeny relationship between the coexistence of gold and molybdenum deposits in the province, mineralization of molybdenum in the Early Yanshanian and the Late Yanshanian, and Molybdenite Re-Os dating. Also mentioned are magmatism, the mineralization pattern and deposits of granites, and high-sulfur magma.

The article discusses the discovery of the world's third largest molybdenum deposit in the Caosiyao area of Xinghe County, Inner Montolia, Northeast China. The deposit is of a porphyry-type, super-large scale and exploration type is I. It cites the deposit's characterization such as its occurrence in the leucoleptite of the 3rd lithological member in the Archean Huangruyao Fm and the delineation of 4 molybdenum orebodies i.e. No. Mo1, lower Mo2, lower Mo3 and lower Mo4.