Geofluids Q3
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Geofluids is a journal indexed in SJR in Earth and Planetary Sciences (miscellaneous) with an H index of 64. It is an CC BY Journal with a Single blind Peer Review review system, and It has a price of 1440 €. The scope of the journal is focused on groundwater, geothermal fluids, petroleum, geochemistry. It has an SJR impact factor of 0,349 and it has a best quartile of Q3. It is published in English. It has an SJR impact factor of 0,349.
Type: Journal
Type of Copyright: CC BY
Languages: English
Open Access Policy: Open Access
Type of publications:
Publication frecuency: -
1440 €
Inmediate OANPD
Embargoed OA- €
Non OAMetrics
0,349
SJR Impact factor64
H Index879
Total Docs (Last Year)1510
Total Docs (3 years)32869
Total Refs2739
Total Cites (3 years)1505
Citable Docs (3 years)1.67
Cites/Doc (2 years)37.39
Ref/DocOther journals with similar parameters
Russian Journal of Earth Sciences Q3
Acta Geodaetica et Cartographica Sinica Q3
Hydrological Research Letters Q3
International Journal of Astrobiology Q3
Zeitschrift der Deutschen Gesellschaft fur Geowissenschaften Q3
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Aims and Scope
Best articles by citations
Gas breakthrough experiments on pelitic rocks: comparative study with N2, CO2 and CH4
View moreUnderstanding heat and groundwater flow through continental flood basalt provinces: insights gained from alternative models of permeability/depth relationships for the Columbia Plateau, USA
View moreEffects of changes in reservoir thermodynamic conditions on222Rn composition of discharged fluids: study for two wells at Los Azufres geothermal field (Mexico)
View morePore-Scale Imaging of the Oil Cluster Dynamic during Drainage and Imbibition Using In Situ X-Ray Microtomography
View moreHydrothermal control on organic matter alteration and illite precipitation, Mt Isa Basin, Australia
View morePore-Scale Modeling of Mixing-Induced Reaction Transport through a Single Self-Affine Fracture
View moreOrigin of palaeofluids in a normal fault setting in the Aegean region
View moreThe gas flow at mineral springs and mofettes in the Vogtland/NW Bohemia: an enduring long-term increase
View moreCharacterization of natural gases in Japan based on molecular and carbon isotope compositions
View moreHydrothermal dolomitization, mixing corrosion and deep burial porosity formation: numerical results from 1-D reactive transport models
View moreThree-dimensional geometry, ore distribution and time-integrated mass transfer through the quartz-tourmaline-gold vein network of the Sigma deposit (Abitibi belt, Canada)
View moreGeodynamically induced variations in the emission of CO2 gas at San Faustino (Central Apennines, Italy)
View moreFluid mixing induced by hydrothermal activity in the ordovician carbonates in Tarim Basin, China
View moreAlgorithm for determining optimum sequestration depth of CO2trapped by residual gas and solubility trapping mechanisms in a deep saline formation
View moreThe geochemical evolution of very dilute CO2-rich water in Chungcheong Province, Korea: processes and pathways
View moreGranite-related overpressure and volatile release in the mid crust: fluidized breccias from the Cloncurry District, Australia
View moreHydrologic and geochemical controls on soluble benzene migration in sedimentary basins
View moreChemical and isotopic signatures of Na/HCO3/CO2-rich geofluids, North Portugal
View moreFluid sinks within the earth's crust
View moreFluid systems and mineralization in the north German and Polish basin
View moreSedimentary fabrics in the authigenic carbonates from Bush Hill: implication for seabed fluid flow and its dynamic signature
View moreCrustal permeability: Introduction to the special issue
View moreComputing geochemical mass transfer and water/rock ratios in submarine hydrothermal systems: implications for estimating the vigour of convection
View moreCommunication between overpressured compartments
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