ISSN: 0301-9268
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Precambrian Research Q1 Unclaimed
Precambrian Research is a journal indexed in SJR in Geology and Geochemistry and Petrology with an H index of 193. It has an SJR impact factor of 1,589 and it has a best quartile of Q1. It is published in English. It has an SJR impact factor of 1,589.
Precambrian Research focuses its scope in these topics and keywords: rocks, earth, archean, formation, paleoproterozoic, constraints, carbonate, events, craton, south, ...
Type: Journal
Type of Copyright:
Languages: English
Open Access Policy:
Type of publications:
Publication frecuency: -
- €
Inmediate OANPD
Embargoed OA- €
Non OAMetrics
1,589
SJR Impact factor193
H Index218
Total Docs (Last Year)1030
Total Docs (3 years)24445
Total Refs3619
Total Cites (3 years)1008
Citable Docs (3 years)3.22
Cites/Doc (2 years)112.13
Ref/DocOther journals with similar parameters
Remote Sensing of Environment Q1
Shiyou Kantan Yu Kaifa/Petroleum Exploration and Development Q1
International Journal of Mining Science and Technology Q1
Engineering Geology Q1
Economic Geology Q1
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Aims and Scope
Best articles by citations
U-Pb constraints for the plutonic and tectonometamorphic evolution of Lake Melville terrane, Labrador and implications for basement reworking in the northeastern Grenville Province
View moreU-Pb detrital zircon geochronology of the Turee Creek Group, Hamersley Basin, Western Australia: Timing and correlation of the Paleoproterozoic glaciations
View moreGeology and tectonic evolution of the Palaeoproterozoic Bryah, Padbury and Yerrida Basins (formerly Glengarry Basin), Western Australia: implications for the history of the south-central Capricorn Orogen
View moreRapakivi granites and related rocks: an introduction
View moreZircon geochronology of migmatite gneisses along the Mylonite Zone (S Sweden): a major Sveconorwegian terrane boundary in the Baltic Shield
View moreAn extensive, crustally-derived, 3325 to 3310 Ma silicic volcanoplutonic suite in the eastern Pilbara Craton: evidence from the Kelly Belt, McPhee Dome and Corunna Downs Batholith
View moreNeoproterozoic strata of the southern Canadian Cordillera and the isotopic evolution of seawater sulfate
View moreThe structure and sequence of geological events in the Basement Complex of the Ibadan area, Western Nigeria
View morePaleoproterozoic hydrothermal reactivation in a neoarchean orogenic lode-gold deposit of the southern Abitibi subprovince: U-Pb monazite geochronological evidence from the Young-Davidson mine, Ontario
View moreA 2.7 Ga depleted tholeiite suite: evidence of plume-arc interaction in the Abitibi Greenstone Belt, Canada
View morePaleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil
View moreThe origin of rapakivi texture by sub-isothermal decompression
View moreRecognizing distinct portions of seamounts using volcanic facies analysis: examples from the Archean Slave Province, NWT, Canada
View moreA 2005-1970 Ma Andean-type batholith in the southern Gascoyne Complex, Western Australia
View moreA world in a grain of sand: regional metamorphic history from 40Ar/39Ar laser probe analyses of proterozoic sediments from the Canadian shield
View moreThe evolution of a Precambrian arc-related granulite facies gold deposit: Evidence from the Glenburgh deposit, Western Australia
View morePaleozoic deformation and isotopic disturbance in the southeastern Arunta Block, central Australia
View moreGeology of Western Gondwana (2000-500 Ma). Pan-African-Brasiliano aggregation of South America and Africa
View moreStratigraphic and structural controls on gold mineralization in the Pilgrim's Rest goldfield, eastern Transvaal, South Africa
View moreThe Archaean geology of Sierra Leone
View moreThe Archaean Ravensthorpe Terrane, Western Australia: synvolcanic Cu-Au mineralization in a deformed island arc complex
View moreStratigraphic architecture and evolution of the early Paleoproterozoic McGrath Trough, Western Australia
View moreObituary
View moreGeochemistry and paleomagnetism of Keweenawan basalt in the subsurface of Nebraska
View more
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