verified COP 3,6 · Q1 • database Scopus / SJR & Web of Science indexed

Netherlands · Elsevier B.V.

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Precambrian Research

Precambrian Research is a journal indexed in SJR in Geology and Geochemistry and Petrology with an H index of 200. It has a COP Index of 3,6 (best band Q1). It is published in English. It has a COP Index of 3,6.

Precambrian Research focuses its scope in these topics and keywords: rocks, events, zimbabwe, paleoproterozoic, late, group, formation, archean, earth, craton, ...

ISSN: 0301-9268

Publisher: Elsevier B.V.

Category: Geology

Indexation: verifiedScopus / SJR verifiedWeb of Science

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schedule CountryOfPapers database fields

COP Index trending_up

3,6 Q1

29 of 117 journals in Geochemistry and Petrology

H-index · SJR 200 · 1,427

Acceptance rate pie_chart

20% Selective

Source Acceptance_Rate

Time to publication hourglass_top

NPD

Field NPD

Publication cost (APC) payments

NPD Subscription

Non-OA path NPD

Metrics

Scimago and CountryOfPapers database fields

Scopus / SJR Web of Science

COP Index

3,6

SJR Impact

1,427

H-index

200

Docs (year)

255

Docs 3y

900

Total refs

29442

Cites 3y

3317

Citable 3y

877

Cites/Doc 2y

3.46

Ref/Doc

115.46

Immediate OA

—

Embargoed OA

NPD

Non OA / Submission

—

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Best articles by citations

Tectono-metamorphic history of Neoproterozoic rocks in eastern Eritrea

U-Pb detrital zircon geochronology of the Turee Creek Group, Hamersley Basin, Western Australia: Timing and correlation of the Paleoproterozoic glaciations

Time constraints on the evolution of the Tennant Creek Block, northern Australia

Three generations of anorthosite-mangerite-charnockite-granite (AMCG) magmatism, contact metamorphism and tectonism in the Saguenay-Lac-Saint-Jean region of the Grenville Province, Canada

Thermal and tectonic evolution of the paleoproterozoic Transamazonian orogen as deduced from 40Ar/39Ar and AMS along the Oyapok river (French Guyana)

The tectonic and metallogenic evolution of the Pilbara Craton: preface

Timing of exhumation of a high-pressure mafic granulite terrane of the Paleoproterozoic Ubende belt (West Tanzania)

The evolution of a Precambrian arc-related granulite facies gold deposit: Evidence from the Glenburgh deposit, Western Australia

The Archaean Ravensthorpe Terrane, Western Australia: synvolcanic Cu-Au mineralization in a deformed island arc complex

The Archaean geology of Sierra Leone

The age of the Ormiston Pound Granite: implications for Mesoproterozoic evolution of the Arunta Inlier, central Australia

Tensile and compressive growth structures: relationships between sedimentation, deformation and granite intrusion in the Archaean Coppin Gap greenstone belt, Eastern Pilbara, Western Australia

SHOW MORE ARTICLES

The evolving continents

Sulfur isotope evidence for the origin of 3.4 to 3.1 Ga pyrite at the Princeton gold mine, Barberton Greenstone Belt, South Africa

Stratigraphic architecture and evolution of the early Paleoproterozoic McGrath Trough, Western Australia

Stratigraphic and structural controls on gold mineralization in the Pilgrim's Rest goldfield, eastern Transvaal, South Africa

Regional variations in the Pb isotopic compositions of ore galena across the Archaean-Proterozoic border in northern Sweden

Recognizing distinct portions of seamounts using volcanic facies analysis: examples from the Archean Slave Province, NWT, Canada

Rapakivi granites and related rocks: an introduction

Professor Stephen Moorbath, F.R.S. -a retirement tribute

Preface

Petrogenesis of Mid-Proterozoic granitic magmas: examples from central and west Texas

Paleozoic deformation and isotopic disturbance in the southeastern Arunta Block, central Australia

Paleoproterozoic late-orogenic and anorogenic alkaline granitic magmatism from northeast Brazil

FAQs

Precambrian Research has a COP Index of 3,6 (Q1), ranked 29 of 117 in Geochemistry and Petrology. SJR: 1,427.

Immediate OA APC is not available (NPD).

The acceptance rate recorded for Precambrian Research is 20%.

Precambrian Research

Metrics

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Best articles by citations

FAQs

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