Abstract Stratigraphy and isotope geochronology in the crystalline core of the Appalachians suggest revised interpretations of the extent, nature and timing of Paleozoic orogens in New England. Five major episodes of magmatism, deformation, and high-grade regional metamorphism are recognized: Taconian (455-442 Ma), Acadian (423-385 Ma), Neo-Acadian (366-350 Ma), Late Pennsylvanian (300-290 Ma) and Alleghanian (280-260…
GFF Template
Write in a clean editor, then format for GFF in one click — DocuGuru applies the official Taylor & Francis template with author–year references and exports a submission-ready PDF plus the editable LaTeX source. Free to start.
About the GFF format
GFF is a peer-reviewed journal published by Taylor & Francis, covering Paleontology and Stratigraphy of Fossils, Geology and Paleoclimatology Research, Geological and Geochemical Analysis.
| 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." GFF 12 (3): 45–58.
Formats any DOI in GFF style. No sign-up. |
| Publishes research in | Paleontology and Stratigraphy of Fossils Geology and Paleoclimatology Research Geological and Geochemical Analysis Geochemistry and Geologic Mapping High-pressure geophysics and materials |
| ISSN | 1103-5897 |
| Citation impact (2-yr) | 0.46 |
| h-index | 50 |
| i10-index | 521 |
| Total citations | 16,805 |
| Top institutions publishing here | Lund University |
| Journal website | www.tandfonline.com |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Papers published in GFF per year
Citation impact of GFF by publication year
Citations each year’s papers have accumulated so far — the most recent years are still building up.
Most-cited papers in GFF
Abstract Eight distinct highstands in sea level emerged from the author's study of the Silurian System on a continent-to-continent basis during the 1980s and 1990s. Some emendations are needed to accommodate other trends recognized since that time, but the overall pattern is strong. Five major highstands and one minor highstand fit the Lower Silurian (Llandovery…
Abstract During the late Palaeoproterozoic, western Baltica was characterised by convergent-margin tectonics that resulted in the formation of N–S trending crustal units: the Transscandinavian Igneous Belt (TIB) and the westward younging Gothian growth zones. Together, these occupy a 200–300 km wide belt between Svecofennian (c. 1.9 Ga) crust in the east and the Skagerrak Sea/Oslo…
Abstract Palaeozoic palaeogeography, highlighting the North Atlantic Caledonian evolution and the destruction of the Iapetus Ocean and the Tornquist Sea, is recapitulated with reconstruction maps from Early Ordovician to Mid-Devonian times. In the Early Ordovician (Trem-adoc-Arenig), Laurentia, Siberia, and the North China Block were positioned in equatorial latitudes, Baltica was located at intermediate southerly latitudes,…
Abstract Based on biostratigraphic position, chemical fingerprinting, and lithic characteristics such as relative thickness, several of the numerous K‐bentonite beds, or complexes of beds, in the Middle Ordovician of Baltoscandia are shown to be traceable over large areas. Because the type of volcanic eruptions that produced such widespread ash beds lasts only a short time…