Compilation of stable isotope fractionation factors of geochemical interest

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5. Isotope palaeotemperatures from the Tjörnes beds in Iceland: evidence of Pliocene cooling
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6. Vapor hydrogen and oxygen isotopes reflect water of combustion in the urban atmosphere
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   A. Jull, J. Beck, G. Burr · 2000 · Geochimica et Cosmochimica Acta
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    Paul Ferguson, Ján Veizer · 2007 · Journal of Geophysical Research Atmospheres
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14. Assessing the past thermal and chemical history of fluids in crystalline rock by combining fluid inclusion and isotopic investigations of fracture calcite
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15. Origin of dolomite in Miocene Monterey Shale and related formations in the Temblor Range, California
    Friedman, Irving, Murata, K.J. · 1979 · Geochimica et Cosmochimica Acta
16. Diagenesis of fibrous magnesian calcite marine cement: Implications for the interpretation of δ18O and δ13C values of ancient equivalents
    Tracy D. Frank, Kyger C. Lohmann · 1996 · Geochimica et Cosmochimica Acta
17. Geochemistry and diagenesis of stratabound calcite cement layers within the Rannoch Formation of the Brent Group, Murchison Field, North Viking Graben (northern North Sea)
    D. J. Prosser, J.A. Daws, Anthony Edward Fallick, B.P.J. Williams · 1993 · Sedimentary Geology
18. Dolomitization and Dolomite Neomorphism: Trenton and Black River Limestones (Middle Ordovician) Northern Indiana, U.S.A.
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19. Are oxygen and carbon isotopes of mollusc shells reliable palaeosalinity indicators in marginal marine environments? A case study from the Middle Jurassic of England
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22. Oxygen and carbon isotopes of Recent calcareous nannofossils as paleoceanographic indicators
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27. Distribution of carbonate cements within depositional facies and sequence stratigraphic framework of shoreface and deltaic arenites, Lower Miocene, the Gulf of Suez rift, Egypt
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28. Paragenesis, Elemental Distribution, and Stable Isotopes at the Pena Colorada Iron Skarn, Colima, Mexico
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33. The atmospheric oxygen cycle: The oxygen isotopes of atmospheric CO2 and 02 and the 02/N2 ratio
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34. Organic- and carbonate-rich soil formation ∼2.6 billion years ago at Schagen, East Transvaal district, South Africa
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35. Hydrogeochemistry and stable isotopes of ground and surface waters from two adjacent closed basins, Atacama Desert, northern Chile
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36. Sandstone diagenesis in the Pattani Basin (Gulf of Thailand): history of water-rock interaction and comparison with the Gulf of Mexico
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37. Genesis of the Olympias carbonate-hosted Pb-Zn (Au, Ag) sulfide ore deposit, eastern Chalkidiki Peninsula, northern Greece
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38. Carbon isotopic composition and lattice-bound carbonate of Peru-Chile margin phosphorites
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39. Mineralogical controls on the oxygen isotopic compositions of UOCs
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40. DOLOMITIZATION AND RELATED FLUID EVOLUTION IN THE OLIGOCENE – MIOCENE ASMARI FORMATION, GACHSARAN AREA, SW IRAN: PETROGRAPHIC AND ISOTOPIC EVIDENCE
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41. Authigenic barite nodules and carbonate concretions in the Upper Devonian shale succession of western New York – A record of variable methane flux during burial
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42. Migration of geothermal fluids in extensional terrains: the ore deposits of the Boccheggiano-Montieri area (southern Tuscany, Italy)
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43. Diet and environment of a mid-Pliocene fauna from southwestern Himalaya: Paleo-elevation implications
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45. Oxygen isotope study of mid-ocean ridge hydrothermal fluids: Implication for the oxygen-18 budget of the oceans
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46. Stable isotope composition of siderite as an indicator of the paleoenvironmental history of oil shale lakes
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47. Hydrogeochemical and isotopic investigations of the Han River basin, South Korea
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48. DEPOSITIONAL AND DIAGENETIC HISTORY OF THE KERENDAN CARBONATE PLATFORM, OLIGOCENE, CENTRAL KALIMANTAN, INDONESIA
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49. Origin of ultramafic-hosted vein magnesite deposits
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50. Dashuigou Tellurium Deposit in Sichuan Province, China: S, C, O, and H Isotope Data and Their Implications on Hydrothermal Mineralization
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51. Source and evolution of ore-forming hydrothermal fluids in the northern Iberian Pyrite Belt massive sulphide deposits (SW Spain): evidence from fluid inclusions and stable isotopes
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52. Trace elements (REE) and isotopes (O, C, Sr) to characterize the metasomatic fluid sources: evidence from the skarn deposit (Fe, W, Cu) of Traversella (Ivrea, Italy)
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53. Oxygen isotope fractionation between oxygen of different sites in illite minerals: a potential single-mineral thermometer
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54. Open and restricted hydrologies in Brent Group diagenesis: North Sea
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55. Stable isotope composition of waters in southeastern California: 2. Groundwaters and their relation to modern precipitation
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56. Origin and migration of palaeofluids in the Upper Visean of the Campine Basin, northern Belgium
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57. An oxygen isotope study of illite and calcite in three Appalachian Paleozoic vertic Paleosols
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58. C–O isotope geochemistry of the Dashiqiao magnesite belt, North China Craton: implications for the Great Oxidation Event and ore genesis
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60. Seasonal variation in stable oxygen and carbon isotope values recovered from modern lacustrine freshwater mollusks: paleoclimatological implications for sub-weekly temperature records
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61. Oxygen Isotope Variability within Nautilus Shell Growth Bands
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62. Diagenetic history and reservoir quality of tight sandstones: A case study from Shiqianfeng sandstones in upper Permian of Dongpu Depression, Bohai Bay Basin, eastern China
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64. The Stable Isotopic Composition of Atmospheric CO2
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65. IMPACT OF DIAGENESIS ON RESERVOIR‐QUALITY EVOLUTION IN FLUVIAL AND LACUSTRINE‐DELTAIC SANDSTONES: EVIDENCE FROM JURASSIC AND TRIASSIC SANDSTONES FROM THE ORDOS BASIN, CHINA
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67. Geochemistry, isotopic composition, and origin of fluids emanating from mud volcanoes in the Copper River basin, Alaska
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68. Stable isotope signatures associated with palaeosols, Pennsylvanian Holder Formation, New Mexico
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69. Regional Carbonate Alteration of the Crust by Mantle-Derived Magmatic Fluids, Tamil Nadu, South India
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70. Lacustrine oxygen isotope record of 20th-century climate change in central EuropeL evaluation of climatic controls on oxygen isotopes in precipitation
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71. Synchronous oil migration and cementation in sandstone reservoirs demonstrated by quantitative description of diagenesis
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