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1. Land-use interactions, Oil-Field infrastructure, and natural processes control hydrocarbon and arsenic concentrations in groundwater, Poso Creek Oil Field, California, USA

5. Noble Gases

12. Gas Emissions and Subsurface Architecture of Fault‐Controlled Geothermal Systems: A Case Study of the North Abaya Geothermal Area

13. Helium

14. Gas emissions and sub-surface architecture of fault-controlled geothermal systems: a case study of the North Abaya geothermal area

17. Primary N2–He gas field formation in intracratonic sedimentary basins.

19. The principles of helium exploration

20. Hydrogeochemical evolution of formation waters responsible for sandstone bleaching and ore mineralization in the Paradox Basin, Colorado Plateau, USA

21. Krypton-81 dating constrains timing of deep groundwater flow activation

27. Crustal Groundwater Volumes Greater than Previously Thought

29. Solubility trapping in formation water as dominant C[O.sub.2] sink in natural gas fields

30. Seawater subduction controls the heavy noble gas composition of the mantle

31. Neon isotopes constrain convection and volatile origin in the Earth's mantle

34. 300-Myr-old magmatic CO2 in natural gas reservoirs of the west Texas Permian basin

39. Recycled components in mantle plumes deduced from variations in halogens (Cl, Br, I), trace elements and 3He/4He along the Hawaiian‐ Emperor Seamount chain

43. Origins of the terrestrial Hf-Nd mantle array: Evidence from a combined geodynamical-geochemical approach

44. Earth holds its breath: some inert-gas isotopes in Earth's atmosphere can only have come from deep inside the planet. We thought we knew how much gas Earth gives up, and how it does it--but a challenge has emerged to the prevailing model

45. Occurrence and Sources of Radium in Groundwater Associated with Oil Fields in the Southern San Joaquin Valley, California

47. Halogen Heterogeneity in the Lithosphere and Evolution of Mantle Halogen Abundances Inferred From Intraplate Mantle Xenoliths

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