Scientific Exchange

• Geochemical Indicators of Crustal Permeability for Improving Seismic Catalogs...
• Beyond Serpentinization: Chloritization of Fe-Rich Diabase Intrusions as an A...
• Origin of Helium and Main Controlling Factors of Helium Accumulationto the We...
• Competitive Dissolution and Occurrence Behavior of Helium-Bearing Natural Ga...
• Natural Hydrogen Generation via Chloritization versus Serpentinization: Contr...
• Fault-Controlled Crustal CO2 Degassing Revealed by CO2-He Geochemistry of the...
• Geochemical characteristics and geological significance of noble gas in natur...
• Isotopic (δ¹³C, δ²H, δ¹⁵N) Signatures of Gases from Mud Volcano Syste...
• Noble gas constraints on charge preservation in tight sandstone reservoirs of...
• Dynamic Enrichment Mechanisms of Natural Hydrogen and Identification ofHigh-P...
• Role of Mineral Trace Metals in Modulating Methane Cycling-(17-ICGG-Abstact)
• Post-Seismic Fluid and Gas Geochemistry Along Major Active Fault Zones in Tü...
• Helium and argon isotopes in fluid inclusions of coated and polycrystalline d...
• Deep-seated volatile migration through fractures: Integrated CO₂ and He isot...
• Introducing a New Web-based Platform Calculating Thermodynamic Properties of...
• Characteristics of noble gas isotopic compositions and their tracing signific...
• Multistage Carbon–Sulfur Coupling in the Ordovician Majiagou Carbonate–Evap...
• From Hidden Mantle Melting to Shallow Geothermal Circulation: Helium and Carb...
• Coupled Kinetic–Thermodynamic Controls on Hydrogen Generation during Serpent...
• Seismic Fluid Geochemistry: Observations and Studies of Active Faults in Chin...
• Gas geochemistry and deep carbon emissions in the Sangri-Cona rift, southern ...
• C-He-Ne-Ar Isotopic Compositions and Implications of Volatiles in the Langmur...
• Isotopic Anomalies in Highly Evolved Natural Gas: Implications for Organic–I...
• Distribution Characteristics and Genesis of Paleozoic Natural Hydrogen in the...
• Active Hydrothermal Hydrogen Emissions in Continental Collision Zones: Insigh...