ISSN: 1012-0750
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South African Journal of Geology Q2 Unclaimed
South African Journal of Geology is a journal indexed in SJR in Geology with an H index of 56. It has an SJR impact factor of 0,532 and it has a best quartile of Q2. It is published in English. It has an SJR impact factor of 0,532.
Type: Journal
Type of Copyright:
Languages: English
Open Access Policy:
Type of publications:
Publication frecuency: -


- €
Inmediate OANPD
Embargoed OA- €
Non OAMetrics
0,532
SJR Impact factor56
H Index26
Total Docs (Last Year)130
Total Docs (3 years)1957
Total Refs187
Total Cites (3 years)125
Citable Docs (3 years)1.25
Cites/Doc (2 years)75.27
Ref/DocOther journals with similar parameters
Journal of Geochemical Exploration Q2
Geothermal Energy Q2
Yantu Lixue/Rock and Soil Mechanics Q2
Anthropocene Review Q2
International Journal of Geo-Engineering Q2
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Aims and Scope
Best articles by citations
The effect of environmental controls on the metal content in ferromanganese crusts and nodules from the Mozambique Ridge and in the Mozambique Basin, southwestern Indian Ocean
View moreLithostratigraphy of the Palaeoproterozoic Verena Granite
View moreEarth-tide as parameter of crustal motion correction for SLR station displacement
View moreThe Kalahari Epeirogeny and climate change: differentiating cause and effect from core to space
View moreCo-existing low-Ti and high-Ti dolerites in two large dykes in the Gap Dyke swarm, southeastern Karoo Basin (South Africa)
View moreZIRCON U-PB EMPLACEMENT AND ND-HF CRUSTAL RESIDENCE AGES OF THE STRAUSSBURG GRANITE AND FRIERSDALE CHARNOCKITE IN THE NAMAQUA-NATAL PROVINCE, SOUTH AFRICA
View moreSource of the suspended load of the upper Orange River, South Africa
View moreThe magnetic field changing over the southern African continent: a unique behaviour
View more40Ar/39Ar age constraints on low-grade metamorphism and cleavage development in the Transvaal Supergroup (central Kaapvaal craton, South Africa): implications for the tectonic setting of the Bushveld Igneous Complex
View moreThe distribition and diagnostic features of deformed plutonic rocks in two terranes of the Namaque mobile belt along the Orange (Gariep) River, South Africa
View moreTiming and kinematics of the Colenso Fault: The Early Paleozoic shift from collisional to extensional tectonics in the Pan-African Saldania Belt, South Africa
View moreA review of the resistivity structure of the Karoo Supergroup, South Africa, with emphasis on the dolerites: A study in anisotropy
View moreDiscussion of Surface Water and Groundwater Interaction in the Upper Crocodile River Basin, Johannesburg, South Africa: Environmental Isotope Approach by Abiye et al.
View moreGEOPHYSICALLY PLUMBING THE MAIN KAROO BASIN, SOUTH AFRICA
View moreAlbian ammonites of the Benguela Basin (Angola): a biostratigraphic framework
View morePrograde andalusite in kyanite-bearing siliceous rocks in the Ilangwe Greenstone Belt, southeastern margin of the Kaapvaal Craton, South Africa
View morePaleostress Analysis of Karoo Supergroup of the Tshipise-Pafuri Basin, South Africa: Comment
View moreInsights into the Petroleum System Evolution of the southern Orange Basin, South Africa
View more"REPLY ON COMMENTS ON THE PAPER ""PETROLOGY AND GEOCHEMISTRY OF THE GRANITOID ROCKS OF THE JOHANNESBURG DOME, CENTRAL KAAPVAAL CRATON, SOUTH AFRICA"" BY D.M. VAN TONDER AND H. MOURI (SAJG, 113, 257-286)"
View moreVesicle paleobarometry in the Pongola Supergroup: A cautionary note and guidelines for future studies
View moreCRETACEOUS EROSION IN CENTRAL SOUTH AFRICA: EVIDENCE FROM UPPER-CRUSTAL XENOLITHS IN KIMBERLITE DIATREMES
View morePresent denudation rates at selected sections of the South African escarpment and the elevated continental interior based on cosmogenic 3He and 21Ne
View moreTAPHONOMIC ASPECTS OF THE WAGONDRIFT QUARRY SITE, AND THEIR IMPLICATIONS FOR THE DEPOSITIONAL ENVIRONMENT OF THE UPPER PERMIAN ESTCOURT FORMATION (KWAZULU-NATAL, SOUTH AFRICA)
View moreMEGA-SCALE ( 50M) ORDOVICIAN LOAD CASTS AT DE BALIE, SOUTH AFRICA: POSSIBLE SEDIMENT FLUIDIZATION BY THERMAL DESTABILISATION
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