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Earth and Environmental Science Transactions of the Royal Society of Edinburgh is a peer-reviewed journal published by Cambridge University Press, covering Geological and Geochemical Analysis, Diverse Scientific and Economic Studies, Paleontology and Stratigraphy of Fossils.
| Publisher | Cambridge University Press |
|---|---|
| Reference style | Numbered Numbered — [1], [2] in the text [1] A. Smith, B. Jones, and C. Lee, A representative article title, Earth and Environmental Science Transactions of the Royal Society of Edinburgh 12 (2023) 45–58.
Formats any DOI in the closest standard style — Earth and Environmental Science Transactions of the Royal Society of Edinburgh has no published style definition, so this is an approximation. No sign-up. |
| Publishes research in | Geological and Geochemical Analysis Diverse Scientific and Economic Studies Paleontology and Stratigraphy of Fossils Legal case studies and regulations Paleontology and Evolutionary Biology |
| ISSN | 1755-6910 |
| Citation impact (2-yr) | 0.65 |
| h-index | 76 |
| i10-index | 472 |
| Total citations | 26,041 |
| Top institutions publishing here | British Geological Survey |
| Journal website | journals.cambridge.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.
ABSTRACT Granites and related volcanic rocks of the Lachlan Fold Belt can be grouped into suites using chemical and petrographic data. The distinctive characteristics of suites reflect source-rock features. The first-order subdivision within the suites is between those derived from igneous and from sedimentary source rocks, the I- and S-types. Differences between the two types…
The Central Asian Orogenic Belt (CAOB), also known as the Altaid Tectonic Collage, is characterised by a vast distribution of Paleozoic and Mesozoic granitic intrusions. The granitoids have a wide range of compositions and roughly show a temporal evolution from calcalkaline to alkaline to peralkaline series. The emplacement times for most granitic plutons fall between…
ABSTRACT: The prospect of partial melting of the subducted oceanic crust to produce arc magmatism has been debated for over 30 years. Debate has centred on the physical conditions of slab melting and the lack of a definitive, unambiguous geochemical signature and petrogenetic process. Experimental partial melting data for basalt over a wide range of…
ABSTRACT This paper is a structural and tectonic approach to the emplacement and deformation of granitoids. The main methods available in structural geology are briefly reviewed and this emphasises that (a) a wealth of data, particularly strain and shear sense, which pertain to these problems, can be determined in and around plutons; (b) given the…
ABSTRACT: Finite difference numerical simulations were used to characterise the rates of diffusion-controlled dissolution and growth of zircon in melts of granitic composition under geologically realistic conditions. The simulations incorporated known solubility and Zr diffusivity relationships for melts containing 3 wt% dissolved H 2 O and were carried out in both one and thre dimensions…
