Laboratory Simulations of Abiotic Hydrocarbon Formation in Earth's Deep Subsurface

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Items 101–200 of 285

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8. Genomic Analysis of the Yet-Uncultured Binatota Reveals Broad Methylotrophic, Alkane-Degradation, and Pigment Production Capacities
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13. High temperature generation and equilibration of methane in terrestrial geothermal systems: Evidence from clumped isotopologues
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14. Microbial vs abiotic origin of methane in continental serpentinized ultramafic rocks: A critical review and the need of a holistic approach
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15. Carbon Assimilation Strategies in Ultrabasic Groundwater: Clues from the Integrated Study of a Serpentinization-Influenced Aquifer
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16. Distribution and origin of organic compounds in the condensates from a Mexican high-temperature geothermal field
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17. Shallow submarine seep of abiotic methane from serpentinized peridotite off the Island of Elba, Italy
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18. Distribution and Sources of Carbon in Serpentinized Mantle Peridotites at the Atlantis Massif (IODP Expedition 357)
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19. Validity of geochemical signatures of abiotic hydrocarbon gases on Earth
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20. Barren ground depressions, natural H2 and orogenic gold deposits: Spatial link and geochemical model
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21. Microbial biosignatures in ancient deep‐sea hydrothermal sulfides
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22. Extensive hydrothermal activity revealed by multi-tracer survey in the Wallis and Futuna region (SW Pacific)
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23. Composition and Distribution of Saturated Hydrocarbons in the Thermal Waters and Vapor–Water Mixture of the Mutnovskii Geothermal Field and Uzon Caldera, Kamchatka
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24. Along-dip variations of subduction fluids: The 30–80 km depth traverse of the Schistes Lustrés complex (Queyras-Monviso, W. Alps)
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25. Identity and mechanisms of alkane-oxidizing metalloenzymes from deep-sea hydrothermal vents
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26. Organo-mineral associations in chert of the 3.5 Ga Mount Ada Basalt raise questions about the origin of organic matter in Paleoarchean hydrothermally influenced sediments
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28. Organic, Gas, and Element Geochemistry of Hydrothermal Fluids of the Newly Discovered Extensive Hydrothermal Area in the Wallis and Futuna Region (SW Pacific)
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29. Organic carbon generation in 3.5-billion-year-old basalt-hosted seafloor hydrothermal vent systems
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30. The Hyblean xenolith suite (Sicily): an unexpected legacy of the Ionian–Tethys realm
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31. Synthesis of heavy hydrocarbons at the core-mantle boundary
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32. Cool, alkaline serpentinite formation fluid regime with scarce microbial habitability and possible abiotic synthesis beneath the South Chamorro Seamount
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33. The Changing Character of Carbon in Fluids with Pressure
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34. Extending the dataset of fluid geochemistry of the Menez Gwen, Lucky Strike, Rainbow, TAG and Snake Pit hydrothermal vent fields: Investigation of temporal stability and organic contribution
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35. Effects of Deep Fluids on Hydrocarbon Generation and Accumulation in Chinese Petroliferous Basins
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36. Thermally driven organic-inorganic interactions in sedimentary basins: A review from source rocks to reservoirs
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37. Nanoscale relationships between uranium and carbonaceous material in alteration halos around unconformity-related uranium deposits of the Kiggavik camp, Paleoproterozoic Thelon Basin, Nunavut, Canada
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38. Mineral-assisted production of benzene under hydrothermal conditions: Insights from experimental studies on C 6 cyclic hydrocarbons
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39. Carbon and hydrogen isotopes of the wet gases produced by gamma-ray-induced polymerisation of methane: Insights into radiogenic mechanism and natural gas formation
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40. Hydrothermal Chemistry
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41. Vibrational Behavior of Water Adsorbed on Forsterite (Mg2SiO4) Surfaces
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42. Termination and hydration of forsteritic olivine (0 1 0) surface
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43. Metastable equilibrium of substitution reactions among oxygen- and nitrogen-bearing organic compounds at hydrothermal conditions
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44. Compound-specific, intra-molecular, and clumped 13C fractionations in the thermal generation and decomposition of ethane and propane: A DFT and kinetic investigation
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45. Graphitic inclusions in zircon from early Phanerozoic S-type granite: Implications for the preservation of Hadean biosignatures
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46. UV-Induced Nanoparticles-Formation, Properties and Their Potential Role in Origin of Life
    Lukáš Nejdl, Kristýna Zemánková, Martina Havlíková, Michaela Buresova, David Hynek, Kledi Xhaxhiu, Filip Mravec, Martina Matoušková, Vojtěch Adam, Martin Ferus et al. · 2020 · Nanomaterials
47. Carboxylate anion generation in aqueous solution from carbonate radiolysis, a potential route for abiotic organic acid synthesis on Earth and beyond
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48. Origin of Petroleum
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49. Activity of Silica‐Rich Hydrothermal Fluid and Its Impact on Deep Dolomite Reservoirs in the Sichuan Basin, Southern China
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50. Transition metal catalysis in natural gas generation: Evidence from nonhydrous pyrolysis experiment
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51. Water adsorption on olivine(010) surfaces: Effect of alkali and transition metal cation doping
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52. Organic Compounds of Medium Volatility in the Thermal Fields of Urup Island, Kuriles, and the Kamchatka Peninsula: A Comparative Analysis
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53. Formation of hydrocarbons favored by high pressure at subduction zone conditions
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54. Abyssal serpentinites as gigantic factories of marine salts and oil
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55. Correlating trace element compositions, petrology, and Raman spectroscopy data in the ∼3.46 Ga Apex chert, Pilbara Craton, Australia
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56. Drilling-induced hydrogen: A challenge for natural hydrogen exploration
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57. Organic geochemical evidence for life in Archean rocks identified by pyrolysis–GC–MS and supervised machine learning
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58. CO2 storage and conversion to CH4 by wet mechanochemical activation of olivine at room temperature
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59. Chemistry of springs across the Mariana forearc: Carbon flux from the subducting plate triggered by the lawsonite-to-epidote transition?
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60. A kinetic pressure effect on the experimental abiotic reduction of aqueous CO2 to methane from 1 to 3.5 kbar at 300 °C
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61. Statistical approach for the geochemical signature of two active normal faults in the western Corinth Gulf Rift (Greece)
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62. Catalytic Hydrogenation of Post-Mature Hydrocarbon Source Rocks Under Deep-Derived Fluids: An Example of Early Cambrian Yurtus Formation, Tarim Basin, NW China
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63. Hydrothermal Transformations of Alcohols with Copper(II) and Iron(III) Salts
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64. Organic Matter and Molecular-Weight Distribution of Hydrocarbons in the Annenskoe Thermal Waters (Far East, Russia)
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65. Extremely deuterium depleted methane revealed in high-temperature volcanic gases
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69. A dynamic H2 system with multi-source methane in chromitite-rich ophiolitic settings
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70. The Potential for Organic Synthesis in the Ocean of Enceladus
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71. Unraveling abiotic organic synthesis pathways in the mafic crust of mid-ocean ridges
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72. Hydrogen isotope fractionation in land-based serpentinization systems. Comment on “Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hydrogen isotope systematics of the Hakuba Happo hot spring” by Suda et al. [Earth Planet. Sci. Lett. 386 (2014) 112–125]
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73. A Method for Detection of Trace Concentrations of Underivatized Amino Acid in Hydrothermal Fluids by Ion-Pairing Reversed-Phase UPLC-ESI-QTOF-MS
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74. Effect of Copper Salts on Amide Hydrothermal Formation and Reactivity
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75. Crystallographic Orientation and Geochemical Features of Mineral Inclusions in Diamonds
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76. Abiotic Methane Generation via CO 2 Hydrogenation With Natural Chromitite Under Hydrothermal Conditions
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77. X-ray micro-computed tomography-based approach to estimate the upper limit of natural H2 generation by Fe2+ oxidation in the intracratonic lithologies
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84. Methylotrophy, alkane-degradation, and pigment production as defining features of the globally distributed yet-uncultured phylum Binatota
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95. Pyrite and Organic Compounds Coexisting in Intrusive Mafic Xenoliths (Hyblean Plateau, Sicily): Implications for Subsurface Abiogenesis
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