ISSN: 0022-3530

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Journal of Petrology Q1 Unclaimed

Oxford University Press United Kingdom

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Journal of Petrology is a journal indexed in SJR in Geophysics and Geochemistry and Petrology with an H index of 195. It has a price of 3100 €. It has an SJR impact factor of 1,976 and it has a best quartile of Q1. It is published in English. It has an SJR impact factor of 1,976.

Journal of Petrology focuses its scope in these topics and keywords: province, lavas, japan, intrusive, indian, idaho, history, granulite, geothermometry, magma, ...

Type: Journal

Type of Copyright:

Languages: English

Open Access Policy:

Type of publications:

Publication frecuency: -

Categories: Geochemistry and Petrology (Q1) Geophysics (Q1)

Price

3100 €

Inmediate OA

NPD

Embargoed OA

0 €

Non OA

Metrics

1,976

SJR Impact factor

195

H Index

86

Total Docs (Last Year)

336

Total Docs (3 years)

9378

Total Refs

1241

Total Cites (3 years)

330

Citable Docs (3 years)

3.13

Cites/Doc (2 years)

109.05

Ref/Doc

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Aims and Scope

Best articles by citations

New Thermodynamic Models and Calculated Phase Equilibria in NCFMAS for Basic and Ultrabasic Compositions through the Transition Zone into the Uppermost Lower Mantle

A Carbon Isotope Study of Diamond Fades Pyroxenites and Associated Rocks from the Beni Bousera Peridotite, North Morocco

Source of the Quaternary Alkalic Basalts, Picrites and Basanites of the Potrillo Volcanic Field, New Mexico, USA: Lithosphere or Convecting Mantle?

The Origin of Rapakivi Texture

U-series Isotope Data on Lau Basin Glasses: the Role of Subduction-related Fluids during Melt Generation in Back-arc Basins

Model for the Origin and Significance of Microgranular Enclaves in Calc-alkaline Granitoids

Continuous Gradations among Primary Carbonatitic, Kimberlitic, Melilititic, Basaltic, Picritic, and Komatiitic Melts in Equilibrium with Garnet Lherzolite at 3-8GPa

A Garnet-Zircon Oxygen Isotope Record of Subduction and Exhumation Fluids from the Franciscan Complex, California

Burial Metamorphism in the Hamersley Basin, Western Australia

Lower Crustal Heterogeneity and Fractional Crystallization Control Evolution of Small-volume Magma Batches at Ocean Island Volcanoes (Ascension Island, South Atlantic)

Mantle Heterogeneity and Crustal Contamination in the Genesis of Low-Ti Continental Flood Basalts from the Paran Plateau (Brazil): Sr-Nd Isotope and Geochemical Evidence

New Constraints on the P-T Evolution of the Alpe Arami Garnet Peridotite Body (Central Alps, Switzerland)': Reply to Comment by Nimis & Trommsdorff (2001)

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Plastic Deformation and Recrystallization of Garnet: A Mechanism to Facilitate Diffusion Creep

Mantle Recycling: Transition Zone Metamorphism of Tibetan Ophiolitic Peridotites and its Tectonic Implications

Mantle Structure Beneath the SW Slave Craton, Canada: Constraints from Garnet Geochemistry in the Drybones Bay Kimberlite

Origin of the Pegmatitic Pyroxenite in the Merensky Unit, Bushveld Complex, South Africa

Tertiary Ultrapotassic Volcanism in Serbia: Constraints on Petrogenesis and Mantle Source Characteristics

Mantle-melt Evolution (Dynamic Source) in the Origin of a Single MORB Suite: a Perspective from Magnesian Glasses of Macquarie Island

High-T, Low-P Formation of Rare Olivine-bearing Symplectites in Variscan Eclogite

Sr, Nd, Pb and O Isotopes of Minettes from Schirmacher Oasis, East Antarctica: a Case of Mantle Metasomatism involving Subducted Continental Material

Slab-Derived Fluids in the Magma Sources of St. Vincent (Lesser Antilles Arc): Volatile and Light Element Imprints

Two Disequilibrium Quartz-Feldspar 18O/16O Fractionations within the Aral Granite Batholith, Altay Mountains of China: Evidence for Occurrence of Two Stages of O and H Isotopic Exchange of a Heterogeneous Granite System with Aqueous Fluids

Exhumation Paths of High-Pressure-Low-Temperature Metamorphic Rocks from the Lycian Nappes and the Menderes Massif (SW Turkey): a Multi-Equilibrium Approach

Petrology and Geochronology of Granulites from the McKaskle Hills, Eastern Amery Ice Shelf, Antarctica, and Implications for the Evolution of the Prydz Belt