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Journal of Petrology is a peer-reviewed journal published by Oxford University Press, covering Geological and Geochemical Analysis, earthquake and tectonic studies, High-pressure geophysics and materials.
| Publisher | Oxford University Press |
|---|---|
| Reference style | Author–year (OUP) Author–year — (Smith, 2023) in the text Smith, A., Jones, B. and Lee, C. (2023) 'A representative article title', Journal of Petrology, 12(3), pp. 45–58.
Formats any DOI in the closest standard style — Journal of Petrology has no published style definition, so this is an approximation. No sign-up. |
| Publishes research in | Geological and Geochemical Analysis earthquake and tectonic studies High-pressure geophysics and materials Geochemistry and Geologic Mapping Geology and Paleoclimatology Research |
| ISSN | 0022-3530 |
| Citation impact (2-yr) | 3.5 |
| h-index | 260 |
| i10-index | 3,492 |
| Total citations | 392,230 |
| Article processing charge | $3,987 |
| Top institutions publishing here | Centre National de la Recherche Scientifique |
| Journal website | petrology.oxfordjournals.org |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Citations each year’s papers have accumulated so far — the most recent years are still building up.
Granites may be subdivided according to their intrusive settings into four main groups—ocean ridge granites (ORG), volcanic arc granites (VAG), within plate granites (WPG) and collision granites (COLG)—and the granites within each group may be further subdivided according to their precise settings and petrological characteristics. Using a data bank containing over 600 high quality trace…
This contribution summarizes and brings up to date the recommendations made by the IUGS Subcommission on the Systematics of Igneous Rocks for the classification of volcanic rocks when modal analyses are lacking. The classification is on a non-genetic basis using the total alkali-silica (TAS) diagram, and is as nearly consistent as possible with the QAPF…
This geochemical classification of granitic rocks is based upon three INTRODUCTION variables. These are FeO/(FeO + MgO) = Fe-number [or Although granitoids are the most abundant rock types FeO tot /(FeO tot + MgO) = Fe * ], the modified alkali-lime index in the continental crust, no single classification scheme (MALI) (Na 2 O +…
We present the first finding of continental crust-derived Precambrian zircons in garnet/spinel pyroxenite veins within mantle xenoliths carried by the Neogene Hannuoba basalt in the central zone of the North China Craton (NCC). Petrological and geochemical features indicate that these mantle-derived composite xenoliths were formed by silicic melt^lherzolite interaction. The Precambrian zircon ages can be…
Abstract We report the results of partial melting experiments between 8 and 32 kbar, on four natural amphibolites representative of metamorphosed Archean tholeiite (greenstone), high-alumina basalt, low-potassium tholeiite and alkali-rich basalt. For each rock, we monitor changes in the relative proportions and composition of partial melt and coexisting residual (crystalline) phases from 1000 to 1150°C,…
