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1

Hansen, Vicki L. "Global tectonic evolution of Venus, from exogenic to endogenic over time, and implications for early Earth processes." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 376, no. 2132 (2018): 20170412. http://dx.doi.org/10.1098/rsta.2017.0412.

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Venus provides a rich arena in which to stretch one's tectonic imagination with respect to non-plate tectonic processes of heat transfer on an Earth-like planet. Venus is similar to Earth in density, size, inferred composition and heat budget. However, Venus' lack of plate tectonics and terrestrial surficial processes results in the preservation of a unique surface geologic record of non-plate tectonomagmatic processes. In this paper, I explore three global tectonic domains that represent changes in global conditions and tectonic regimes through time, divided respectively into temporal eras. I
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Barnes, Gina L. "Tectonic Archaeology as a Foundation for Geoarchaeology." Land 10, no. 5 (2021): 453. http://dx.doi.org/10.3390/land10050453.

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This article proposes a new subdiscipline, Tectonic Archaeology, based on the efforts of Japanese archaeologists to deal with the effects of earthquakes, volcanic tephra cover, and tsunami on archaeological sites. Tectonic Archaeology is conceived as an umbrella term for those efforts and as a foundation for Geoarchaeology in general. Comparisons distinguish between Geoarchaeology and Tectonic Archaeology, and a survey of major archaeological journals and textbooks reveals how the concept of ‘tectonics’ and specifically the processes of Plate Tectonics have been treated. Al-though the term ‘te
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Klimczak, Christian, Paul K. Byrne, A. M. Celâl Şengör, and Sean C. Solomon. "Principles of structural geology on rocky planets." Canadian Journal of Earth Sciences 56, no. 12 (2019): 1437–57. http://dx.doi.org/10.1139/cjes-2019-0065.

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Although Earth is the only known planet on which plate tectonics operates, many small- and large-scale tectonic landforms indicate that deformational processes also occur on the other rocky planets. Although the mechanisms of deformation differ on Mercury, Venus, and Mars, the surface manifestations of their tectonics are frequently very similar to those found on Earth. Furthermore, tectonic processes invoked to explain deformation on Earth before the recognition of horizontal mobility of tectonic plates remain relevant for the other rocky planets. These connections highlight the importance of
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Brocklehurst, Simon H. "Tectonics and geomorphology." Progress in Physical Geography: Earth and Environment 34, no. 3 (2010): 357–83. http://dx.doi.org/10.1177/0309133309360632.

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The field of tectonic geomorphology is in a state of tension. The widespread availability of high-quality, high-resolution digital topographic data encourages the development of simple morphological ‘tools’ which can be used to deduce recent tectonic evolution. Meanwhile, process geomorphologists recognize that current models have a significant empirical basis, and lack insight into the underlying physics of erosion processes. Most tectonic geomorphology research is concerned with rivers, but glaciers, debris flows and hillslope processes also play a key role in hypotheses linking climate to t
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Zerkle, Aubrey L. "Biogeodynamics: bridging the gap between surface and deep Earth processes." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 376, no. 2132 (2018): 20170401. http://dx.doi.org/10.1098/rsta.2017.0401.

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Life is sustained by a critical and not insubstantial set of elements, nearly all of which are contained within large rock reservoirs and cycled between Earth's surface and the mantle via subduction zone plate tectonics. Over geologic time scales, plate tectonics plays a critical role in recycling subducted bioactive elements lost to the mantle back to the ocean–biosphere system, via outgassing and volcanism. Biology additionally relies on tectonic processes to supply rock-bound ‘nutrients’ to marine and terrestrial ecosystems via uplift and erosion. Thus, the development of modern-style plate
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A.S.Yo'ldoshaliyev and O.M.Mamalatipov. "STRUCTURAL GEOLOGY AND TECTONICS." JOURNAL OF UNIVERSAL SCIENCE RESEARCH 2, no. 1 (2024): 50–59. https://doi.org/10.5281/zenodo.10464048.

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<em>Structural geology and tectonics are fundamental disciplines within the field of geology, providing vital insights into the deformation and displacement processes that shape the Earth's crust. This abstract explores the fundamental principles and methodologies employed in studying the structures and tectonic processes that occur within the Earth's lithosphere. It discusses the classification and characteristics of geological structures, including folds, faults, and fractures, and emphasizes their significance in deciphering the tectonic history of a region.</em>
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7

Heron, Philip J., Russell N. Pysklywec, and Randell Stephenson. "Exploring the theory of plate tectonics: the role of mantle lithosphere structure." Geological Society, London, Special Publications 470, no. 1 (2018): 137–55. http://dx.doi.org/10.1144/sp470.7.

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AbstractThis review of the role of the mantle lithosphere in plate tectonic processes collates a wide range of recent studies from seismology and numerical modelling. A continually growing catalogue of deep geophysical imaging has illuminated the mantle lithosphere and generated new interpretations of how the lithosphere evolves. We review current ideas about the role of continental mantle lithosphere in plate tectonic processes. Evidence seems to be growing that scarring in the continental mantle lithosphere is ubiquitous, which implies a reassessment of the widely held view that it is the in
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8

Zovoili, E., E. Konstantinidi та I. K. Koukouvelas. "TECTONIC GEOMORPHOLOGY OF ESCARPMENTS: THE CASES OF KOMPOTADES AND ΝΕΑ ANCHIALOS FAULTS". Bulletin of the Geological Society of Greece 36, № 4 (2004): 1716. http://dx.doi.org/10.12681/bgsg.16579.

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Most active processes on the surface imply that tectonics and geomorphology converge in a way that landscape change may be used as a tectonic signal, given that erosion and weathering have been taken into account. We selected two faults, the Kompotades and the Nea Anchialos faults in the Sperchios and South Thessaly rift zones respectively, and we performed a morphometric analysis. This analysis comprises geomorphic indices that have been used successfully in studies of active tectonics, as the mountain front sinuosity index (Smf), stream gradient index (SL) and valley floor width to valley he
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9

Kolodyazhny, S. Y. "LONG-LIVED STRUCTURAL ENSEMBLES OF THE EAST EUROPEAN PLATFORM. ARTICLE 1. THE BASEMENT TECTONICS." Proceedings of higher educational establishments. Geology and Exploration, no. 2 (April 30, 2018): 5–13. http://dx.doi.org/10.32454/0016-7762-2018-2-5-13.

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General features of the basement tectonics of the East European platform (EEP) have been considered. The important role of the long-lived Paleoproterozoic tectonic zones has been noted. They were formed due to the cyclic processes of rifting and compression combined with the strike-sleep shearing. They include different structures often superimposed in space: systems of rifts and collisional orogenic belts, transtensional and transpressional zones, ensembles associated with tectonic-plate processes. A special role belongs to the non-linear structures: different scaled rotational structures, co
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10

Mysak, M. "Historical analysis of the hypotheses of tectonic morphogenesis of the Male Polissia Basin." Physical Geography and Geomorphology 89, no. 1 (2018): 16–22. http://dx.doi.org/10.17721/phgg.2018.1.02.

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The hypotheses of morphogenesis of the Male Polissia Basin, where the influence of the tectonic factor is considered, are analyzed in this article. The analysis was carried out on the basis of existing literary and cartographic sources related to geological and geomorphological studies of Male Polissia. Two groups of tectonic hypotheses of morphogenesis of Male Polissia are defined: denudation-tectonic and tectonic-denudation. Suppoters of the denudation-tectonic hypothesis claimed that the main factor in the morphogenesis of the Male Polissia was denudation, and tectonic processes only contri
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11

Miccadei, Enrico, Cristiano Carabella, and Giorgio Paglia. "Morphoneotectonics of the Abruzzo Periadriatic Area (Central Italy): Morphometric Analysis and Morphological Evidence of Tectonics Features." Geosciences 11, no. 9 (2021): 397. http://dx.doi.org/10.3390/geosciences11090397.

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Drainage basin-scale morphometric analysis and morphological evidence of tectonics represent helpful tools to evaluate and investigate morphoneotectonic processes in tectonically active regions. In this perspective, we applied an integrated analysis to the Abruzzo Periadriatic Area, between the Tronto and Sinello rivers (Central Italy). It involved morphometric analysis, structural geomorphological field mapping, and detailed analysis of fluvial terraces. Geomorphic indexes and markers (e.g., Irta, SL index, ksn, and knickpoints) were used in this study to detect the response of landscapes to
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Baibatsha, Adilkhan, Yuriy Vyazovetsky, Maxat Kembayev, Sayat Rais, and Bakytgul Agaliyeva. "On the use of remote sensing data to study the geological structure and forecast mineral resources of the Shu-Ile suture." Mining of Mineral Deposits 18, no. 4 (2024): 56–70. https://doi.org/10.33271/mining18.04.056.

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Purpose. This article focuses on analyzing the geodynamic processes that underline the formation of the Shu-Ile ore zone. The study is based on the principles of plume tectonics, which have gained widespread recognition in the geological community in recent decades. Methods. The article considers the main aspects of the plume-tectonic concept, including the mechanisms of mantle material flows and their impact on regional geological processes. Special attention is paid to analyzing tectonic and magmatic events associated with forming the Shu-Ile ore zone within plume-tectonic mechanisms. Findin
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13

Coulthard, T. J., and M. J. Van de Wiel. "Climate, tectonics or morphology: what signals can we see in drainage basin sediment yields?" Earth Surface Dynamics 1, no. 1 (2013): 13–27. http://dx.doi.org/10.5194/esurf-1-13-2013.

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Abstract. Sediment yields from river basins are typically considered to be controlled by tectonic and climatic drivers. However, climate and tectonics can operate simultaneously and the impact of autogenic processes scrambling or shredding these inputs can make it hard to unpick the role of these drivers from the sedimentary record. Thus an understanding of the relative dominance of climate, tectonics or other processes in the output of sediment from a basin is vital. Here, we use a numerical landscape evolution model (CAESAR) to specifically examine the relative impact of climate change, tect
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14

Coulthard, T. J., and M. J. Van de Wiel. "Climate, tectonics or morphology: what signals can we see in drainage basin sediment yields?" Earth Surface Dynamics Discussions 1, no. 1 (2013): 67–91. http://dx.doi.org/10.5194/esurfd-1-67-2013.

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Abstract. Sediment yields from river basins are typically considered to be controlled by tectonic and climatic drivers. However, climate and tectonics can operate simultaneously and the impact of autogenic processes scrambling or shredding these inputs can make it hard to unpick the role of these drivers from the sedimentary record. Thus an understanding of the relative dominance of climate, tectonics or other processes in the output of sediment from a basin is vital. Here, we use a numerical landscape evolution model (CAESAR) to specifically examine the relative impact of climate change, tect
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15

Beakhouse, Gary P., Shoufa Lin, and Sandra L. Kamo. "Magmatic and tectonic emplacement of the Pukaskwa batholith, Superior Province, Ontario, CanadaThis article is one of a series of papers published in this Special Issue on the theme of Geochronology in honour of Tom Krogh." Canadian Journal of Earth Sciences 48, no. 2 (2011): 187–204. http://dx.doi.org/10.1139/e10-048.

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The Neoarchean Pukaskwa batholith consists of pre-, syn-, and post-tectonic phases emplaced over an interval of 50 million years. Pre-tectonic phases are broadly synvolcanic and have a high-Al tonalite–trondhjemite–granodiorite (TTG) affinity interpreted to reflect derivation by partial melting of basaltic crust at lower crustal or upper mantle depths. Minor syn-tectonic phases slightly post-date volcanism and have geochemical characteristics suggesting some involvement or interaction with an ultramafic (mantle) source component. Magmatic emplacement of pre- and syn-tectonic phases occurred in
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16

Scheidegger, A. E., and N. S. Ai. "Tectonic processes and geomorphological design." Tectonophysics 126, no. 2-4 (1986): 285–300. http://dx.doi.org/10.1016/0040-1951(86)90234-9.

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17

Foulger, G. R. "Plumes, or plate tectonic processes?" Astronomy & Geophysics 43, no. 6 (2002): 6.19–6.23. http://dx.doi.org/10.1046/j.1468-4004.2002.43619.x.

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18

Ren, Zhikun, Peizhen Zhang, Takashi Oguchi, and Zhongtai He. "Remote Sensing Perspectives on Geomorphology and Tectonic Processes." Remote Sensing 15, no. 9 (2023): 2327. http://dx.doi.org/10.3390/rs15092327.

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The quantity and quality of remote sensing measurements of tectonic deformation have increased dramatically over the past two decades, improving our ability to observe active geomorphological tectonic processes. High-precision and high-resolution topography is the basis for the quantitative study of active geomorphological and tectonic processes. Recently, with the rapid development of computer visual science and the growing application of light detection and ranging (LiDAR), small unmanned aerial vehicles (UAVs) and structure from motion (SfM) photogrammetry have shown great potential in prov
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19

Pei, Rongfu. "Deep tectonic processes and super-accumulation of metals." Global Tectonics and Metallogeny 8, no. 1-4 (2003): 67–69. http://dx.doi.org/10.1127/gtm/8/2003/67.

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20

Paunikar, S. K., B. S. Manjare, and J. R. Shrivatra. "Evaluation of Tectonics along Western Extension of Gavilgarh Fault Zone, Central India using Geomorphic Indices." Journal Of The Geological Society Of India 100, no. 8 (2024): 1171–88. http://dx.doi.org/10.17491/jgsi/2024/173965.

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ABSTRACT The study examines various morphometric parameters and geomorphic indices within sub-basins along the Western extension of the Gavilgarh Fault zone. The combined analysis of these factors serves as a crucial tool for assessing tectonic activity in the region, showing strong correlations with structural discontinuities and geomorphological anomalies. The study area, located Southeast of Jalgaon, Maharashtra, demonstrates recent tectonic activity, especially in sub-basins P1 to P6. Fluvial patterns within the region reflect tectonic influences, as evidenced by various geomorphic indices
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21

Verrios, S., V. Zygouri, and S. Kokkalas. "MORPHOTECTONIC ANALYSIS IN THE ELIKI FAULT ZONE (GULF OF CORINTH, GREECE)." Bulletin of the Geological Society of Greece 36, no. 4 (2004): 1706. http://dx.doi.org/10.12681/bgsg.16578.

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Morphotectonic analysis using geomorphic indices has been developed as a basic reconnaissance tool in order to identify areas experiencing rapid tectonic deformation or estimate relative variations of tectonic activity in a specific area. We applied this analysis in Eliki fault zone, which is located in the western part of the Gulf of Corinth. Eliki fault zone was selected because it displays a spectacular geomorphic expression and hosts historic and recent seismicity. The intensity of active tectonics is interpreted through a detailed geomorphic study of the fault-generated mountain fronts an
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Ivanik, O., L. Tustanovska, and K. Hadiatska. "MAIN CAUSES OF GRAVITATION PROCESSES WITHIN THE MIDDLE DNIEPER REGION." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 1 (88) (2020): 6–11. http://dx.doi.org/10.17721/1728-2713.88.01.

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Integrated assessment and analyses of gravitational geological processes impact on the technogene objects is based on a systematic approach to the analysis of the geological environment; creation of geological, mathematical and spatial models of the geological environment, development of analytical tools. The complex application of geological and geomorphological methods (structural-morphometric analysis, comparative tectonics and structural analysis), remote sensing data and GIS technologies made it possible to identify the relationship between the processes of geomorphogenesis and tectogenes
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Petrova, Hristina, Uroš Stojadinović, Boris Vakanjac, et al. "Link between active tectonics/faulting and mineral and thermal water occurrence in Republic of North Macedonia." Review of the Bulgarian Geological Society 85, no. 3 (2024): 221–24. https://doi.org/10.52215/rev.bgs.2024.85.3.221.

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According to the tectonic architecture of the Balkan Peninsula, the territory of Macedonia belongs to the Dinarides, Rhodope and Carpatho-Balkanides. In a relatively small area, Macedonia has a very complex geological and tectonic structure, which was shaped by intense and long-term processes, followed by magmatism of a wide spectrum, from the ultrabasic to the acidic. From a stratigraphic point of view, geological formations consist of the oldest Precambrian high-grade metamorphic rocks to the youngest Quaternary deposits, and such a complex geological structure conditions the creation of dif
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Pereira, Inês, and Patrícia João. "A story of lithospheric plates." Project Repository Journal 23, no. 1 (2025): 86–89. https://doi.org/10.54050/prj23232.

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A story of lithospheric plates Whether plate tectonics began 850 million years ago or earlier is uncertain. FINGER-PT hypothesises that preservation bias obscures evidence of earlier modern-like tectonics. To test this, the project analyses detrital minerals in sedimentary rocks, employing experimental petrology, elastic barometry, and geochemistry to uncover when tectonic processes as we know them began.
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Bashir, Bashar, Abdullah Alsalman, Hussein Bachir, and Mahmoud Elnobi. "GIS-Analysis for Active Tectonics Assessment of Wadi Al-Arish, Egypt." Applied Sciences 13, no. 4 (2023): 2659. http://dx.doi.org/10.3390/app13042659.

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In this paper, we apply an effective method to evaluate relative tectonic activity by applying several morph-tectonic indices that are useful in evaluating topography and tectonics. These indices include stream length-gradient, asymmetric factor, hypsometric index, hypsometric curves, valley floor width to valley height ratio, drainage basin shape, and mountain front sinuosity. The study region of Wadi Al-Arish in northern Sinai Peninsula in northern Egypt is a natural laboratory to examine relative tectonic activity levels for calculating morpho-tectonic indices of several catchments and sub-
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Hematang, Yashinta Irma Pratami, and Ikaputra Ikaputra. "Four Aspects of Architectural Tectonics Through Exploration of the Meaning of Tectonics with a Systematic Literature Review Method." Journal of Architectural Design and Urbanism 5, no. 1 (2022): 1–11. http://dx.doi.org/10.14710/jadu.v5i1.15470.

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Architectural tectonics which has a meaningful relationship with aesthetic and construction aspects in buildings is still sometimes understood separately from one another. In addition to the need for architectural practice and education, in this context, this article seeks to enrich the meaning of architectural tectonics by exploring and synthesizing meaning from leading online and architectural dictionaries as well as various libraries of journals, proceedings, reports, and architectural books. Tectonics in architectural research and design still needs to be explored where this concept can be
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Hidayat, Edi, Dicky Muslim, Dimas Aryo Wibowo, et al. "Appraisal of active tectonics in Karangsambung Amphitheater: Insights from DEM-derived geomorphic indices and geological data." IOP Conference Series: Earth and Environmental Science 1314, no. 1 (2024): 012092. http://dx.doi.org/10.1088/1755-1315/1314/1/012092.

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Abstract The morphology of the Karangsambung area shows a unique form, namely the morphology of the amphitheater. This area results from the complexity of tectonic, erosion, and depositional processes. The active tectonics in this region greatly influence the drainage system and geomorphic expression. The study area provides evidence of subduction in Java. It is an ideal natural laboratory for studying evidence of tectonic activity due to the subduction of the Indo-Australian plate with the Eurasian plate during the Cretaceous period. We evaluated active tectonics using the DEM to assess the c
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Tenzer, Robert, and Ali Fadil. "Tectonic classification of vertical crustal motions – a case study for New Zealand." Contributions to Geophysics and Geodesy 46, no. 2 (2016): 91–109. http://dx.doi.org/10.1515/congeo-2016-0007.

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Abstract We investigate the relationship between vertical crustal motion and tectonic block configuration. The study is conducted along the active tectonic margin between the Australian and Pacific tectonic plates in New Zealand with a well-defined tectonic block configuration. For this purpose, the rates of vertical crustal motions relative to the ITRF2008 reference frame are estimated based on processing the GPS data (provided by the GeoNET project) collected at 123 continuous and semi-continuous GPS sites. The numerical results confirmed the uplift of the central Southern Alps at the curren
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Mouslopoulou, Vasiliki, John Begg, Alexander Fülling, Daniel Moraetis, Panagiotis Partsinevelos, and Onno Oncken. "Distinct phases of eustatic and tectonic forcing for late Quaternary landscape evolution in southwest Crete, Greece." Earth Surface Dynamics 5, no. 3 (2017): 511–27. http://dx.doi.org/10.5194/esurf-5-511-2017.

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Abstract. The extent to which climate, eustasy and tectonics interact to shape the late Quaternary landscape is poorly known. Alluvial fans often provide useful indexes that allow the decoding of information recorded on complex coastal landscapes, such as those of the eastern Mediterranean. In this paper we analyse and date (using infrared stimulated luminescence (IRSL) dating) a double alluvial fan system on southwest Crete, an island straddling the forearc of the Hellenic subduction margin, in order to constrain the timing and magnitude of its vertical deformation and discuss the factors con
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KUDRYAVTSEV, Anatoly. "MANTLE-LITHOSPHERE INTERACTION PROCESSES AND THEIR INFLUENCE ON FLOOD BASALT PROVINCES: PLUME-THEORY AND ALTERNATIVE MODELS." LIFE OF THE EARTH 42, no. 4 (2020): 433–42. http://dx.doi.org/10.29003/m1772.0514-7468.2020_42_4/433-442.

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Different geotectonic hypotheses with respect to flood basalt provinces formation interpretation were analysed. Geotectonic models are proposed to unite in two groups: II. Traditional: plume-tectonic interpretation; I. Alternative models: delamination hypothesis and others.The flood basalt provinces properties (geological structure, history of development) study permits finding the best mantle-lithosphere interaction model.Keywords: flood basalt provinces, plume-tectonics, magmatism.
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Murphy, Brendan, Stephen T. Johnston, and Boswell Wing. "Prologue: Andrew Hynes Series: Tectonic Processes." Geoscience Canada 42, no. 3 (2015): 303. http://dx.doi.org/10.12789/geocanj.2015.42.075.

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Price, N. J., and M. G. Audley-Charles. "Tectonic collision processes after plate rupture." Tectonophysics 140, no. 2-4 (1987): 121–29. http://dx.doi.org/10.1016/0040-1951(87)90224-1.

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Audley-Charles, M. G. "Tectonic post-collision processes in Timor." Geological Society, London, Special Publications 355, no. 1 (2011): 241–66. http://dx.doi.org/10.1144/sp355.12.

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Widera, Marek. "Tectonic and Glaciotectonic Deformations in the Areas of Polish Lignite Deposits." Civil and Environmental Engineering Reports 28, no. 1 (2018): 182–93. http://dx.doi.org/10.2478/ceer-2018-0015.

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Abstract This study addresses the complex geology caused mainly by tectonic and glaciotectonic processes in lignite-bearing areas of Poland. Tectonics played a dominant role in the deformation of peat/lignite seams during their deposition. This is especially true for deep grabens where the thickest lignite seams were deposited (e.g., Bełchatów). Conversely, glaciotectonics led to the post-depositional deformation of other deposits (e.g., Sieniawa). The effects of tectonic and glaciotectonic processes in this region are investigated using both simplified geological cross-sections and photograph
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Abramova, L. M., I. M. Varentsov, and D. Yu Abramova. "Image of Mantle Plume Processes in the Satellite Magnetic Field Over Africa Territory." Исследования Земли из космоса 2023, no. 2 (2023): 31–42. http://dx.doi.org/10.31857/s0205961423010025.

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The spatial distribution of the lithospheric magnetic anomalies field carries information about its sources – deep tectonic structures – and reflects the processes occurring at mantle depths. Based on the geomagnetic data measured by the CHAMP satellite at an observation altitude of ~290 km, the lithospheric magnetic field parameters over the territory of the African continent were calculated. A lot of maps of the lithospheric magnetic anomalies field total intensity Ta based on various scales and degrees have been constructed. The distribution of Ta over the territories of South and East Afri
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Hang, Phung Thi Thu, Renat Shakirov, Bui Van Thom, et al. "Assessment of the Tectonic Activity of the Muong La–Bac Yen–Cho Bo Fault (Northwest Vietnam) by Analysis of Geomorphological Indices." GeoHazards 6, no. 2 (2025): 16. https://doi.org/10.3390/geohazards6020016.

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The Muong La–Bac Yen–Cho Bo fault is one of the seismic faults in the northwest region of Vietnam. Neo-tectonic activities and exogenous processes have influenced the drainage system and topographic–geomorphologic features on both walls of the fault. The results of topographic analysis and geomorphological indices have confirmed the active tectonics of the fault during the Neo-tectonic period (Pliocene–Quaternary, about 5 million years). The valley floor width-to-height ratio (Vf) of less than 0.5 indicates the “rejuvenation” of the streams and the obvious influence of tectonic activities on t
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O’Neill, C., S. Marchi, W. Bottke, and R. Fu. "The role of impacts on Archaean tectonics." Geology 48, no. 2 (2019): 174–78. http://dx.doi.org/10.1130/g46533.1.

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Abstract Field evidence from the Pilbara craton (Australia) and Kaapvaal craton (South Africa) indicate that modern tectonic processes may have been operating at ca. 3.2 Ga, a time also associated with a high density of preserved Archaean impact indicators. Recent work has suggested a causative association between large impacts and tectonic processes for the Hadean. However, impact flux estimates and spherule bed characteristics suggest impactor diameters of &amp;lt;100 km at ca. 3.5 Ga, and it is unclear whether such impacts could perturb the global tectonic system. In this work, we develop n
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Ghazaryan, K. S., and R. S. Sargsyan. "Seismotectonic analysis of the Viraayots–Karabakh zone (Armenia) and the adjacent areas of Lesser Caucasus." Geodynamics & Tectonophysics 12, no. 1 (2021): 157–65. http://dx.doi.org/10.5800/gt-2021-12-1-0519.

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The territory of Armenia, although relatively small, is geologically and tectonically complex. Its complexity is not only due to a dense network of faults. It results from a complicated history of tectonic development including several phases of mountain formation and planation, and the extensive development of fold-block, tectonic and magmatic processes. An important scientific task is identification of earthquake-prone structural blocks by analysing seismotectonic data on geotectonic zones in Armenia. This article describes the seismotectonic analysis of geological and geophysical data on th
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Coltice, Nicolas, Laurent Husson, Claudio Faccenna, and Maëlis Arnould. "What drives tectonic plates?" Science Advances 5, no. 10 (2019): eaax4295. http://dx.doi.org/10.1126/sciadv.aax4295.

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Does Earth’s mantle drive plates, or do plates drive mantle flow? This long-standing question may be ill posed, however, as both the lithosphere and mantle belong to a single self-organizing system. Alternatively, this question is better recast as follows: Does the dynamic balance between plates and mantle change over long-term tectonic reorganizations, and at what spatial wavelengths are those processes operating? A hurdle in answering this question is in designing dynamic models of mantle convection with realistic tectonic behavior evolving over supercontinent cycles. By devising these model
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Noltimier, Hal, and Dork Sahagian. "Tectonic style of venus: An analog to polar “icepack tectonics”." Journal of Geodynamics 16, no. 1-2 (1992): 65–79. http://dx.doi.org/10.1016/0264-3707(92)90019-o.

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Cavadas, Bento, and Sara Aboim. "Using PhET™ interactive simulation plate tectonics for initial teacher education." Geoscience Communication 4, no. 1 (2021): 43–56. http://dx.doi.org/10.5194/gc-4-43-2021.

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Abstract. Using digital educational resources (DERs) in science education is an effective way of promoting students' content knowledge of complex natural processes. This work presents the usage of the digital educational resource CreativeLab_Sci&amp;amp;Math | Plate Tectonics, designed for exploring the PhET™ Plate Tectonics simulator, in the context of the education of pre-service teachers (PSTs) in Portugal. The performance of the PSTs was analysed based on the five tasks into which the DER was organized. Results show that the DER contributed to the successful achievement of the following le
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O'Neill, Craig, Simon Turner, and Tracy Rushmer. "The inception of plate tectonics: a record of failure." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 376, no. 2132 (2018): 20170414. http://dx.doi.org/10.1098/rsta.2017.0414.

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The development of plate tectonics from a pre-plate tectonics regime requires both the initiation of subduction and the development of nascent subduction zones into long-lived contiguous features. Subduction itself has been shown to be sensitive to system parameters such as thermal state and the specific rheology. While generally it has been shown that cold-interior high-Rayleigh-number convection (such as on the Earth today) favours plates and subduction, due to the ability of the interior stresses to couple with the lid, a given system may or may not have plate tectonics depending on its ini
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Harrison, R. W., W. L. Newell, H. Batıhanlı, et al. "Tectonic framework and Late Cenozoic tectonic history of the northern part of Cyprus: implications for earthquake hazards and regional tectonics." Journal of Asian Earth Sciences 23, no. 2 (2004): 191–210. http://dx.doi.org/10.1016/s1367-9120(03)00095-6.

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Ruban, Dmitry A. "Did plate tectonics control the generic diversity of Jurassic brachiopods? One point of view." Geologos 24, no. 1 (2018): 79–84. http://dx.doi.org/10.2478/logos-2018-0006.

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Abstract Possible plate tectonic controls on faunal diversity dynamics have been discussed in the geological literature for around 50 years. The new model of plate tectonic processes is here linked to Jurassic generic diversity (simple α-diversity) of brachiopods. This comparison offers three observations, four hypotheses and three unresolved issues. Most importantly, changes in the global plate root mean square speed coincided with brachiopod diversity dynamics, which can be explained hypothetically by either environmental disturbance triggered by more active plate motion or activity of any p
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McCall, G. J. H., M. G. Audley-Charles, and A. Hallam. "Tectonic Processes and Palaeontological Patterns Uneasily Joined." Journal of Biogeography 17, no. 1 (1990): 110. http://dx.doi.org/10.2307/2845201.

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Trifonov, V. G., and S. Yu Sokolov. "Tectonic Phenomena and Supervising Underlying Geodynamic Processes." Geotectonics 52, no. 5 (2018): 564–77. http://dx.doi.org/10.1134/s0016852118050072.

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Sharp, Martin, Wendy Lawson, and Robert S. Anderson. "Tectonic processes in a surge-type glacier." Journal of Structural Geology 10, no. 5 (1988): 499–515. http://dx.doi.org/10.1016/0191-8141(88)90037-5.

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Kusky, T. M., R. J. Stern, and J. F. Dewey. "Secular changes in geologic and tectonic processes." Gondwana Research 24, no. 2 (2013): 451–52. http://dx.doi.org/10.1016/j.gr.2013.03.015.

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Li, Shiyuan. "Modeling of stringer deformation and displacement in Ara salt after the end of salt tectonics." Open Geosciences 10, no. 1 (2018): 323–32. http://dx.doi.org/10.1515/geo-2018-0025.

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Abstract The present work considers numerical models of large rock inclusions (stringers) are embedded in many salt bodies. The study has been made to investigate the influence of salt tectonic process, such as downbuilding, on the deformation and displacement of stringers. In this research, the focus has been on establishing numerical models of the deformation and displacement of stringer embedded in salt (at rest) after occurrences of salt tectonics. The problem of influence of eventual tectonic processes at larger stage is addressed on the development of stringers. The numerical model is ba
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Yin, An, Günther Brandl, and Alfred Kröner. "Plate-tectonic processes at ca. 2.0 Ga: Evidence from >600 km of plate convergence." Geology 48, no. 2 (2019): 103–7. http://dx.doi.org/10.1130/g47070.1.

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Abstract We addressed when plate-tectonic processes first started on Earth by examining the ca. 2.0 Ga Limpopo orogenic belt in southern Africa. We show through palinspastic reconstruction that the Limpopo orogen originated from &amp;gt;600 km of west-directed thrusting, and the thrust sheet was subsequently folded by north-south compression. The common 2.7–2.6 Ga felsic plutons in the Limpopo thrust sheet and the absence of an arc immediately predating the 2.0 Ga Limpopo thrusting require the Limpopo belt to be an intracontinental structure. The similar duration (∼40 m.y.), slip magnitude (&a
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