The Longmen Shan region includes, from west to east, the northeastern part of the Tibetan Plateau, the Sichuan Basin, and the eastern part of the eastern Sichuan fold-and-thrust belt. In the northeast, it merges with the Micang Shan, a part of the Qinling Mountains. The Longmen Shan region can be divided into two major tectonic…
International Geology Review Template
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About the International Geology Review format
International Geology Review is a peer-reviewed journal published by Taylor & Francis, covering Geological and Geochemical Analysis, Geochemistry and Geologic Mapping, Geological Studies and Exploration.
| Publisher | Taylor & Francis |
|---|---|
| Reference style | Author–year (Chicago, T&F) Author–year — (Smith, 2023) in the text Smith, Ada, Ben Jones, and Cara Lee. 2023. "A Representative Article Title." International Geology Review 12 (3): 45–58.
Formats any DOI in International Geology Review style. No sign-up. |
| Publishes research in | Geological and Geochemical Analysis Geochemistry and Geologic Mapping Geological Studies and Exploration earthquake and tectonic studies High-pressure geophysics and materials |
| ISSN | 0020-6814 |
| Citation impact (2-yr) | 1.85 |
| h-index | 117 |
| i10-index | 2,175 |
| Total citations | 100,761 |
| Top institutions publishing here | Geological Institute |
| Journal website | www.tandfonline.com |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Papers published in International Geology Review per year
Citation impact of International Geology Review by publication year
Citations each year’s papers have accumulated so far — the most recent years are still building up.
Most-cited papers in International Geology Review
We use updated rotations within the Pacific-Antarctica-Africa-North America plate circuit to calculate Pacific-North America plate reconstructions for times since chron 13 (33 Ma). The direction of motion of the Pacific plate relative to stable North America was fairly steady between chrons 13 and 4, and then changed and moved in a more northerly direction from…
High-P/T metamorphic belts were classified into types A and B according to their protoliths. The A-type (collision-type) blueschists possess passive-margin protoliths characterized by platform-type carbonates, bimodal volcanics, and peraluminous sediments. B-type (Cordilleran-type) blueschists consist of active continental-margin protoliths in an accretionary complex characterized by bedded chert, MORB and ocean-island basalts, reef limestones, and graywackes. The…
In general, Archean rocks exhibit rather ordinary moderate-P-high-T facies series metamorphism; neither blueschists nor any record of deep continental subduction and return are documented. However, the abundance and scale of ultrahigh-temperature (UHT) metamorphic belts from the Neoarchean to the Cambrian imply a significant change in geodynamics during the Neoarchean Era, after which transient sites of…
The basement rocks in the eastern zone of the North China craton are composed predominantly of pretectonic tonalitic-trondhjemitic-granodioritic gneisses and syntectonic granitoids, with rafts of supracrustal rocks consisting of ultramafic to felsic volcanic and sedimentary rocks, metamorphosed over a range of conditions from greenschist to granulite facies. Most mafic granulites, amphibolites, and some pelitic gneisses…