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This study analyzes reduced gas seepages in ophiolitic complexes from Oman, the Philippines, Turkey, and New Caledonia, focusing on the chemical composition of gas mixtures primarily consisting of H2, CH4, and N2. Four distinct types of gas mixtures are identified, reflecting different zones of gas generation, with H2-rich gases associated with ultrabasic spring waters and serpentinization processes. The findings suggest multiple origins for these gas mixtures, influenced by geological conditions and the pr

Author

Jairo Pérez

Language

EN