Geofluids Q3
Unclaimed
Geofluids is a journal indexed in SJR in Earth and Planetary Sciences (miscellaneous) with an H index of 68. 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 0,328 and it has a best quartile of Q3. It is published in English. It has an SJR impact factor of 0,328.
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
0,328
SJR Impact factor68
H Index242
Total Docs (Last Year)2130
Total Docs (3 years)9212
Total Refs2927
Total Cites (3 years)2128
Citable Docs (3 years)1.27
Cites/Doc (2 years)38.07
Ref/DocOther journals with similar parameters
Zeitschrift der Deutschen Gesellschaft fur Geowissenschaften Q3
Italian Journal of Geosciences Q3
Terrestrial, Atmospheric and Oceanic Sciences Q3
Quarterly Journal of Engineering Geology and Hydrogeology Q3
Journal of Geosciences 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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