Note: Intro -- Contents -- 1 An Overview -- 1.1 Introduction -- 1.2 Regional Geology -- 1.2.1 Langshan-Zhaertai Area -- 1.2.2 The Bainaimiao Area -- 1.2.3 A Special Focus on the Paleozoic Orogenesis -- References -- 2 The Bainaimiao Cu-Au-Mo Deposit -- 2.1 Introduction -- 2.2 Geology of the Bainaimiao Deposit -- 2.3 Geochronologic Constraints -- 2.3.1 Geochronology of the Mineralized Granodiorite Porphyry -- 2.3.2 Ages of the Host Rocks -- 2.3.3 Timing of Regional Metamorphism -- 2.3.4 Age of the Mineralization -- 2.4 Fluid Inclusions Research -- 2.4.1 The Sample Characters and Methods -- 2.4.2 The Type of Fluid Inclusions -- 2.4.3 The Distribution of Fluid Inclusions -- 2.4.4 The Fluid Inclusion Micro-thermometric Analysis Results -- 2.4.5 Raman Spectra Results -- 2.4.6 The Features and Evolution of Ore Fluids at Bainaimiao Deposit -- 2.5 Discussion -- 2.5.1 Evolutionary History of the Bainamiao Arc -- 2.5.2 Timing and Genesis of Mineralization at Bainaimiao -- 2.5.3 Implications for Mineral Exploration -- 2.6 Conclusion -- References -- 3 The Huogeqi Cu-Pb-Zn Deposit -- 3.1 Introduction -- 3.2 Geology of the Huogeqi Deposit -- 3.3 Characteristics of Iron Formations in the Mining Area -- 3.4 Shear Zone-Controlled Cu-Pb-Zn Mineralization -- 3.4.1 Ore Fabrics, Mineral Paragenesis and Mineral Chemistry -- 3.4.2 Shear Zone-Controlled Mineralization During the Uplift of the Host Rocks -- 3.4.3 Copper Mineralization Controlled by Fe-Rich Host Rocks -- 3.5 Ore-Forming Fluids -- 3.5.1 Sampling and Analytical Methods -- 3.5.2 Fluid Inclusion Petrography -- 3.5.3 Micro-thermometric and Raman Analysis -- 3.5.4 Fluid Composition and Density -- 3.5.5 Pressures and Temperatures of Cu Mineralization -- 3.5.6 Origin and Evolution of Cu-Mineralizing Fluids -- 3.6 Constraints from the H, O, S, and Fe Isotopes -- 3.6.1 Sampling and Analytical Methods. , 3.6.2 Stable Isotope Compositions -- 3.6.3 Constraints on the Sources of Ore-Forming Materials -- 3.6.4 An Interpretation in the Context of a Multi-stage Ore-Formation Model -- 3.7 39Ar/40Ar Geochronology -- 3.7.1 The Occurrence of Amphibole and Biotite -- 3.7.2 39Ar/40Ar Dating Method -- 3.7.3 The Mineralization Age -- 3.7.4 Geodynamic Background of Ore Formation -- 3.8 Conclusion and Discussion -- 3.8.1 The Multistage Genetic Model -- 3.8.2 The Relationship Between Cu-Pb-Zn and Orogenic Gold Deposits -- 3.8.3 Implications for Mineral Exploration -- References -- 4 The Dongshengmiao Zn-Pb-Cu Deposit -- 4.1 Introduction -- 4.2 Geology of the Dongshengmiao Deposit -- 4.3 Two Stages of Sulfides: Syngenetic Pyrite and Shear Zone-Controlled Zn-Pb-Cu -- 4.3.1 Syngenetic Sulfide -- 4.3.2 Shear Zone-Controlled Zn-Pb-Cu Mineralization -- 4.4 Isotopic Constraints on the Sources of Metal, Sulfur and Ore-Forming Fluid -- 4.4.1 Lead Isotopes of Sulfides -- 4.4.2 Sulfur Isotope of Sulfides -- 4.4.3 Oxygen and Hydrogen Isotopes of Ore-Forming Fluids -- 4.4.4 Interpretations: Synmetamorphic Remobilization of Stratabound Sulfides -- 4.5 Redistribution of Base Metals Controlled by Host Rock Lithology: Thermodynamic Constraints -- 4.5.1 The Initial Ore-Fluid -- 4.5.2 The Flow-Through Modeling -- 4.6 Ore-Forming Age and Geodynamic Background -- 4.6.1 Sampling and Analysis Methods -- 4.6.2 Results and Interpretations -- 4.6.3 Tectonic Background of Early Cretaceous Zn-Pb-Cu Remobilization -- 4.7 Discussion and Conclusions -- 4.7.1 The Genetic Model -- 4.7.2 Implications for Mineral Exploration -- References -- 5 The Jiashengpan Zn-Pb Deposit -- 5.1 Introduction -- 5.2 Geology of the Jiashengpan Deposit -- 5.3 Geochronology Constraints on the Age of Zn-Pb Mineralization -- 5.3.1 39Ar/40Ar Dating of Syn-ore Hydrothermal Muscovite. , 5.3.2 Zircon U-Pb Dating of Post-ore Granite -- 5.4 Discussion -- 5.4.1 Orogenic-Type Zn-Pb Mineralization During Orogenesis -- 5.4.2 Implications for Mineral Exploration -- References -- 6 Understanding Orogenic-Type Base Metal Deposits: A Summary -- References.