Tectonics

Papers
(The H4-Index of Tectonics is 20. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2021-09-01 to 2025-09-01.)
ArticleCitations
79
New 40Ar/39Ar Dating and Paleomagnetism of the Pana Formation Rocks From the Linzhou Basin, Lhasa Block: Implications for the India‐Asia Collision45
Kinematic Evolution of the Santa Bárbara System in the Foreland of the Central Andes of Northwestern Argentina (26°S)45
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A Newly Identified “Proto‐Kenting Mélange (S. Taiwan)” Represents a Missing Link for a Continuous Early Cretaceous Paleo–Pacific Subduction–Accretion System30
Wide Versus Narrow Back‐Arc Rifting: Control of Subduction Velocity and Convective Back‐Arc Thinning30
Differential Extrusion of Indochina‐South China Block and Its Interplay With Slab‐Pull Tectonics: Evidence for End‐Oligocene Basin Inversion in the Beibuwan Basin29
Paleolatitudinal Drift and Major Rotation of the Wrangellia Superterrane in the Mesozoic: A Signal of East‐Panthalassa Plate Motion?28
Reconstructing the Iberian Salt‐Bearing Rifted Margin of the Southern Pyrenees: Insights From the Organyà Basin27
Detachment and Transfer Fault Systems in the Northern South China Sea, Insights Into 3D Tectonic Segmentation of Rifted Margins24
Provenance Analysis of the Andrée Land Basin and Implications for the Paleogeography of Svalbard in the Devonian24
Along‐Strike Variation in the Initiation Timing of the North‐Trending Rifts in Southern Tibet as Revealed From the Yadong‐Gulu Rift24
Jurassic Evolution of the Dunhuang Basin and Its Implications for the Early History of the Altyn Tagh Fault, Northeast Tibet Plateau23
22
Time Constraints on the Late Cenozoic Fault Evolution Along the Northern Margin of the Iranian Plateau in the Arabia‐Eurasia Collision Zone22
Discovery of the William's Ridge and Rig Seismic Seamount Microcontinents, Kerguelen Plateau: Signatures of a Fragmented Rifted Margin21
Multi‐Stage Growth in the North Margin of the Qinling Orogen, Central China, Revealed by Both Low‐Temperature Thermochronology and River Profile Inversion21
Basal Décollement Splaying Induces Mid‐Crustal Tectonic Imbrication in an Intracontinental Orogen20
Crustal Stresses in the East Arctic Region From New Data on Earthquake Focal Mechanisms20
Oligocene/Early Miocene E/W‐Shortening in the Oman Mountains Related to Oblique Arabia‐India Convergence20
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