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Littérature scientifique sur le sujet « Permian tectonic »

Auteur : Grafiati

Publié le 9 mars 2023

Mis à jour le 31 juillet 2025

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Articles de revues sur le sujet "Permian tectonic"

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Scaramuzzo, Emanuele, Franz A. Livio, Maria Giuditta Fellin, and Colin Maden. "Evidence for multi-rifting in the Variscan–Alpine cycle transition: insights from the European western Southern Alps." Solid Earth 16, no. 7 (2025): 619–40. https://doi.org/10.5194/se-16-619-2025.

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Abstract. We investigate the transition between the Paleozoic Variscan cycle and the Mesozoic–Cenozoic Alpine supercontinent cycle, both of which have played a pivotal role in shaping the central European–Mediterranean plate architecture. Two main scenarios have been proposed so far for this transition: (i) a single, long-lasting, Permo-Triassic rifting event, culminating in the opening of the Alpine Tethys, or (ii) multiple, distinct rifting events, predating the onset of the Alpine cycle. Our study focuses on the European western Southern Alps (Varese area, N. Italy), where we document the t

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Song, Dongfang, Wenjiao Xiao, Brian F. Windley, and Chunming Han. "Provenance and tectonic setting of late Paleozoic sedimentary rocks from the Alxa Tectonic Belt (NW China): Implications for accretionary tectonics of the southern Central Asian Orogenic Belt." GSA Bulletin 133, no. 1-2 (2020): 253–76. http://dx.doi.org/10.1130/b35652.1.

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Abstract The Central Asian Orogenic Belt has long been considered the largest Phanerozoic accretionary orogen in the world; it developed through the subduction and final closure of the Paleo–Asian Ocean. However, the architecture and duration of the accretionary orogenesis of the Central Asian Orogenic Belt are still controversial despite decades of investigation. In this study, we present field, compositional, and stratigraphically controlled detrital zircon geochronological data for late Paleozoic sedimentary rocks from the Alxa Tectonic Belt to constrain their provenance, tectonic setting,

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Li, Yalong, Wei Yue, Xun Yu, et al. "Tectonic Evolution of the West Bogeda: Evidences from Zircon U-Pb Geochronology and Geochemistry Proxies, NW China." Minerals 10, no. 4 (2020): 341. http://dx.doi.org/10.3390/min10040341.

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The Bogeda Shan (Mountain) is in southern part of the Central Asian Orogenic Belt (CAOB) and well preserved Paleozoic stratigraphy, making it an ideal region to study the tectonic evolution of the CAOB. However, there is a long-standing debate on the tectonic setting and onset uplift of the Bogeda Shan. In this study, we report detrital zircon U-Pb geochronology and whole-rock geochemistry of the Permian sandstone samples, to decipher the provenance and tectonic evolution of the West Bogeda Shan. The Lower-Middle Permian sandstone is characterized by a dominant zircon peak age at 300–400 Ma, s

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Chen, Xingyu, Zhijie Zhang, Xuanjun Yuan, et al. "The Evolution of Permian Source-to-Sink Systems and Tectonics Implications in the NW Junggar Basin, China: Evidence from Detrital Zircon Geochronology." Minerals 12, no. 9 (2022): 1169. http://dx.doi.org/10.3390/min12091169.

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The basin type of the Junggar Basin changed during the Permian, but the time constraint of the tectonic evolution remains unclear. Besides, the fan deltas developed in the Permian in the Mahu Sag in the northwestern of the oil-rich basin. However, the provenances of the sedimentary systems remain unclear. Based on petrology and detrital zircon U-Pb ages, this study investigates the source-to-sink systems evolution and tectonics implications. Abundant lithic clasts in sandstones with low compositional and textural maturity imply proximal sources. The dating results showed a dominant peak (310–3

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Wopfner, H., and C. Z. Kaaya. "Stratigraphy and morphotectonics of Karoo deposits of the northern Selous Basin, Tanzania." Geological Magazine 128, no. 4 (1991): 319–34. http://dx.doi.org/10.1017/s0016756800017593.

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AbstractLate Permian Karoo deposits of the northern Selous Basin in south-central Tanzania comprise conglomerates and diamictitic boulder beds of alluvial and scarp-foot fan origin. These merge with grey to greenish sandstones, siltstones and black shales of deltaic and lacustrine environments. Microflora assemblages indicate a late Permian age. Lateral changes and interfingering of various lithofacies units are common. Depositional development was controlled by syndepositional faulting and variations of gradients resulting from fault movements. The position of the fault scarp separating the b

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Guanglong, Shen, Wang Yong-dong, Jun Wang, Liu Huaqing, and Zhang Shuangquan. "Tectonic implications of Permian floras in China." Journal of Palaeosciences 45 (December 31, 1996): 324–28. http://dx.doi.org/10.54991/jop.1996.1251.

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On the basis of comprehensive palaeophytogeographical study, the Permian flora of China may be divided into 4 phytorealms, 5 phytoareas and 13 phytoprovinces. The tectonic implications of the Permian floras and phytoprovinces in China are preliminarily discussed.

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Han, Zuozhen, Jingjing Li, Zhigang Song, et al. "Geochemistry and Zircon U-Pb-Hf Isotopes of Metamorphic Rocks from the Kaiyuan and Hulan Tectonic Mélanges, NE China: Implications for the Tectonic Evolution of the Paleo-Asian and Mudanjiang Oceans." Minerals 10, no. 9 (2020): 836. http://dx.doi.org/10.3390/min10090836.

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The Late Paleozoic–Early Mesozoic tectonic evolution of the Changchun-Yanji suture (CYS) was mainly associated with the Paleo-Asian and Mudanjiang tectonic regimes. However, the spatial and temporal overprinting and variations of these two regimes remains are still dispute. In order to evaluate this issue, in this contribution, we present new zircon U-Pb ages and a whole-rock geochemical and zircon Hf isotopic dataset on a suite of metamorphic rocks, including gneisses, actinolite schist, leptynites, and biotite schists, from tectonic mélanges in northern Liaoning and central Jilin provinces,

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Maystrenko, Y., U. Bayer, and M. Scheck-Wenderoth. "3D reconstruction of salt movements within the deepest post-Permian structure of the Central European Basin System - the Glueckstadt Graben." Netherlands Journal of Geosciences - Geologie en Mijnbouw 85, no. 3 (2006): 181–96. http://dx.doi.org/10.1017/s0016774600021466.

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AbstractThe Glueckstadt Graben is a prominent structure of the Central European Basin System, where the sedimentary patterns are extensively affected by Permian salt movements. The relations of the sedimentary patterns to salt structures have been analyzed through present-day distributions of sediments. In addition, a three-dimensional backward modelling approach has been applied to determine the original salt distribution in response to the unloading due to sequential backstripping of the stratigraphic layers. The results of the modelling reveal the thickness distribution of the Permian salt

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Olšavský, Mário. "Revízia permských sedimentov tatrika z oblasti Nízkych Tatier." Geologické práce, Správy 137 (December 29, 2021): 31–46. https://doi.org/10.5281/zenodo.6417946.

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On the basis of systematic revision mapping the thesis reports the real state of representation of the Permian sedimentary formation in the Tatric tectonic unit in the Nízke Tatry Mts. Permian deposits later called the Vážna Formation, were reported in the area of the Vážna valley in the 1980s. The Permian deposits depicted on two regional geological maps have been revised over a period of more than a decade. Revision mapping from the Baláže and Trango&scaron;ka areas did not confirm presence the Vážna Formation. Permian deposits outcrop in the Okrúhly

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Michaelsen, Per, and Karsten M. Storetvedt. "Tectonic evolution of a sequence of related late Permian transtensive coal-bearing sub-basins, Mongolia: A global wrench tectonics portrait." Mongolian Geoscientist 28, no. 57 (2023): 1–53. http://dx.doi.org/10.5564/mgs.v28i57.3200.

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During the late Permian in Mongolia, inertia-driven transtensive reactivation of primordial fracture zones gave rise to the development of a sequence of related, but isolated, fault-bounded sub-basins; some of these became the locus of substantial peat accumulation that evolved into economically important coal deposits. The present study focuses on late Permian coal measures in two widely separated areas: Area 1: located in central Mongolia, developed along the southern margin of the Mongol-Transbaikalian Seaway. The late Permian coal sequence forms a c. 420 m thick middle part of a Permo-Tria

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Thèses sur le sujet "Permian tectonic"

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Ford, Andrew J. H. "Tectonic influence on permian sedimentation, central portion, Pepita-Wackett-Nockatunga Trend, Cooper Basin, Southwest Queensland /." Title page, contents and abstract only, 1986. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bf699.pdf.

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Becker, Thomas Patrick. "PALEOGEOGRAPHIC AND TECTONIC IMPLICATIONS OF THE LATE PALEOZOIC ALLEGHANIAN OROGEN DEVELOPED FROM ISOTOPIC SEDIMENTARY PROVENANCE PROXIES FROM THE APPALACHIAN FORELAND BASIN." UKnowledge, 2005. http://uknowledge.uky.edu/gradschool_diss/367.

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The Alleghanian orogeny was a collision between the Gondwanan and Laurentian continents that produced the Pangean supercontinent. Mechanical and kinematic models of collisional orogens are believed to follow a critical taper geometry, where the tectonic imbrication of continental crust begins nearest to the edge of continental plate and advances toward the craton in a break- forward sequence. Studies of shear zones within the Alleghanian collisional orogen, however, suggest that most of the early deformation was translational. Propagation of craton-directed thrusts into the foreland did not oc

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TSUKADA, Kazuhiro, and Yasushi TAKAHASHI. "Redefinition of the Permian strata in the Hida-gaien Tectonic Zone, Fukuji area, Gifu Prefecture, Central Japan." Dept. of Earth and Planetary Sciences, Nagoya University, 2000. http://hdl.handle.net/2237/2848.

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Armin, Richard Alan. "RED CHERT-CLAST CONGLOMERATE IN THE EARP FORMATION (PENNSYLVANIAN-PERMIAN), SOUTHEASTERN ARIZONA: STRATIGRAPHY, SEDIMENTOLOGY, AND TECTONIC SIGNIFICANCE." Diss., The University of Arizona, 1986. http://hdl.handle.net/10150/187538.

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A single interval of red chert-clast conglomerate and associated strata (RCC/CRCC interval) occur within the Earp Formation (pennsylvanian-Permian) at many localities in southeastern Arizona, southwestern New Mexico, and northern Mexico, and record a middle Wolfcampian erosional event in the Pedregosa shelf and northern basin. The RCC and CRCC intervals are respective proximal and distal braidplain deposits, in contrast to the Earp Formation exclusive of the RCC/CRCC interval, which consists of interbedded carbonate and fine-grained siliciclastic strata that were deposited in mostly shallow- a

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Meibos, Joshua Kerst. "Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin." BYU ScholarsArchive, 2019. https://scholarsarchive.byu.edu/etd/7583.

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The stratal architecture of the upper Ely Limestone and Mormon Gap Formation (Pennsylvanian-early Permian) in western Utah reflects the interaction of icehouse sea-level change and tectonic activity in the distal Antler-Sonoma foreland basin. Eighteen physically and biostratigraphically corelated stratigraphic sections provide a database for tracing Permo-Carboniferous boundary strata over a north-south distance of 60 km. These formations comprise 14 unconformity-bounded depositional sequence: three in the upper Ely (UE1-UE3) and 11 in the Mormon Gap Formation (MG1-MG11). Conodont and fusulini

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LOCCHI, SOFIA. "The Post-Variscan evolution of the central Southern Alps: insights from synchronous fault activity, hydrothermalism and magmatism in the Orobic and Collio Basins." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2023. https://hdl.handle.net/10281/404097.

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Durante il Permiano Inferiore, l’evoluzione post-Varisica dell’attuale regione Alpina è stata caratterizzata da una importante estensione crostale combinata con intensa attività magmatica, che ha favorito lo sviluppo di bacini estensionali intra-continentali con deposizione di sedimenti vulcanoclastici (e.g. Bacino Orobico). Nel settore centrale delle Alpi Meridionali, l’apertura di questi bacini era controllata da complessi sistemi di faglia, attivi contemporaneamente con l’intrusione di plutoni e l’attività vulcanica in superficie. Il seguente progetto di dottorato si focalizza sullo studio

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Worthington, James R., Paul Kapp, Vladislav Minaev, et al. "Birth, life, and demise of the Andean-syn-collisional Gissar arc: Late Paleozoic tectono-magmatic-metamorphic evolution of the southwestern Tian Shan, Tajikistan." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/626289.

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The amalgamation of the Central Asian Orogenic Belt in the southwestern Tian Shan in Tajikistan is represented by tectono-magmatic-metamorphic processes that accompanied late Paleozoic ocean closure and collision between the Karakum-Tarim and Kazakh-Kyrgyz terranes. Integrated U-Pb geochronology, thermobarometry, pseudosection modeling, and Hf geochemistry constrain the timing and petro-tectonic nature of these processes. The Gissar batholith and the Garm massif represent an eastward, along-strike increase in paleodepth from upper-batholith (similar to 21-7km) to arc-root (similar to 36-19km)

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Venus, Joanne Helen. "Tectono-stratigraphic evolution of fluvial and aeolian systems in a salt mini-basin province during changing climatic conditions : Permian Undifferentiated Cutler Group, South East Utah, USA." Thesis, University of Leeds, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.597094.

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The Permian Cutler Group in the northwest part of the Paradox foreland basin of south-eastern Utah and south-western Colorado comprises a succession of conglomerate and sandstone of mixed fluvial and aeolian affinity up to 4000 m thick: the proximal and medial parts of this basin-fill succession are the focus of this study. Fluctuations in climate and sediment flux resulted in growth and recession of penecontemporaneously operating fluvial and aeolian systems. Fluvial sediment was sourced from the Uncompahgre Uplift of the Ancestral Rocky Mountains. Progressive loading and movement of older sa

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Carasco, Bruno. "Les grabens stéphano-permiens de l'est de la France : Evolution tectono-sédimentaire, développement des facies lacustres carbonates et sapropéliques." Université Louis Pasteur (Strasbourg) (1971-2008), 1987. http://www.theses.fr/1987STR13079.

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Andreas, Dieter. "Der Thüringer Wald im Zeitraum der Stefan-Unterperm-Entwicklung - ein Abschnitt der Zentraleuropäischen N-S-Riftzone innerhalb des Mitteleuropäischen Großschollenscharniers." Doctoral thesis, Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2013. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-130056.

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Die einer unterschiedlichen Genese zuordenbaren tektonischen Strukturen, welche sich im Raum des Thüringer Waldes bündeln, formten in einem gerichteten Entwicklungsablauf das komplizierteste und vielseitigste hochoberkarbonisch-unterpermische Strukturgebäude Mitteleuropas. In dieser Arbeit wird der Versuch einer Synthese der strukturellen und der daran geknüpften vulkanogen-sedimentären Entwicklung innerhalb der permokarbonischen Thüringer Wald-Senke und ihres unmittelbaren mitteleuropäischen Umfeldes unternommen. Sie stützt sich dabei maßgeblich auf die Ergebnisse langfristig durchgeführter K

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Livres sur le sujet "Permian tectonic"

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1947-, Stone Paul, and Geological Society of America, eds. Stratigraphic relations and tectonic significance of rocks near the Permian-Triassic boundary, southern Inyo Mountains, California. Geological Society of America, 2000.

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H, Stevens Calvin, and Stone Paul 1947-, eds. The Pennsylvanian-early Permian Bird Spring carbonate shelf, Southeastern California: Fusulinid biostratigraphy, paleogeographic evolution, and tectonic implications. Geological Society of America, 2007.

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Matthew, Laroche T., Viveiros J. J, and West Texas Geological Society, eds. Structure and tectonics of the Big Bend Area and Southern Permian Basin, Texas: West Texas Geological Society 1994 field trip guidebook. West Texas Geological Society, 1994.

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Stevens, Calvin H., and Paul Stone. The Pennsylvanian-Early Permian Bird Spring Carbonate Shelf, Southeastern California: Fusulinid Biostratigraphy, Paleogeographic Evolution, and Tectonic Implications. Geological Society of America, 2007. http://dx.doi.org/10.1130/spe429.

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Stevens, Calvin H., and Paul Stone. The Pennsylvanian-Early Permian Bird Spring Carbonate Shelf, Southeastern California: Fusulinid Biostratigraphy, Paleogeographic Evolution, and Tectonic Implications (Gsa Special Papers). Geological Society of Amer, 2007.

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Special Paper 429: The Pennsylvanian-Early Permian Bird Spring Carbonate Shelf, Southeastern California: Fusulinid Biostratigraphy, Paleogeographic Evolution, and Tectonic Implications. Geological Society of America, 2007. http://dx.doi.org/10.1130/978-0-8137-2429-4.

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Chen, Hanlin, and Shufeng Yang. Early Permian Tarim Large Igneous Province in Northwest China: Tectonics, Petrology, Geochemistry, and Geophysics. Elsevier, 2018.

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Chen, Hanlin, and Shufeng Yang. Early Permian Tarim Large Igneous Province in Northwest China: Tectonics, Petrology, Geochemistry, and Geophysics. Elsevier, 2018.

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Maddin, Hillary Catherine. Cranial anatomy of Ennatosaurus tecton (Synapsida: Caseidae) from the Middle Permian of Russia, and the evolutionary relationships of Caseidae. 2006.

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Ramberg, I. B., and E. R. Neumann. Tectonics and Geophysics of Continental Rifts: Volume Two of the Proceedings of the NATO Advanced Study Institute Paleorift Systems with Emphasis on the Permian Oslo Rift, Held in Oslo, Norway, July 27 - August 5 1977. Springer London, Limited, 2012.

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Chapitres de livres sur le sujet "Permian tectonic"

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Su, Ben-Xun. "Permian Mantle Plume and Paleozoic Tectonic Evolution." In Mafic-ultramafic Intrusions in Beishan and Eastern Tianshan at Southern CAOB: Petrogenesis, Mineralization and Tectonic Implication. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-54262-6_9.

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Wan, Tianfeng. "Tectonics of Late Permian-Triassic (The Indosinian Tectonic Period, 260–200 Ma)." In The Tectonics of China. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-11868-5_6.

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Wan, Tianfeng. "Tectonics of Middle Devonian-Middle Permian (The Tianshan Tectonic Period, 397–260 Ma)." In The Tectonics of China. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-11868-5_5.

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Uliana, M. A., and K. T. Biddle. "Permian to Late Cenozoic Evolution of Northern Patagonia: Main Tectonic Events, Magmatic Activity, and Depositional Trends." In Gondwana Six: Structure, Tectonics, and Geophysics. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm040p0271.

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Hozik, Michael J. "Tectonic implications of the brittle fracture history of the Permian Narragansett Pier Granite, Rhode Island." In Proceedings of the International Conferences on Basement Tectonics. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-1614-5_34.

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Vackiner, Anna Alexandra. "Syndepositional Tectonic Controls and Palaeo-Topography of a Permian Tight Gas Reservoir in NW Germany." In Springer Theses. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-36047-3_4.

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Al-Helal, Anwar, Yaqoub AlRefai, Abdullah AlKandari, and Mohammad Abdullah. "Subsurface Stratigraphy of Kuwait." In The Geology of Kuwait. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-16727-0_2.

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AbstractThis chapter reviews the subsurface stratigraphy of Kuwait targeting geosciences educators. The lithostratigraphy and chronostratigraphy of the reviewed formations (association of rocks whose components are paragenetically related to each other, both vertically and laterally) followed the formal stratigraphic nomenclature in Kuwait. The exposed stratigraphic formations of the Miocene–Pleistocene epochs represented by the Dibdibba, Lower Fars, and Ghar clastic sediments (Kuwait Group) were reviewed in the previous chapter as part of near-surface geology. In this chapter, the description

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Forsythe, Randall D., Dennis V. Kent, Constantino Mpodozis, and John Davidson. "Paleomagnetism of Permian and Triassic Rock, Central Chilean Andes." In Gondwana Six: Structure, Tectonics, and Geophysics. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm040p0241.

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Korsch, R. J., K. D. Wake-Dyster, P. E. O’brien, D. M. Finlayson, and D. W. Johnstone. "Geometry of Permian to Mesozoic Sedimentary Basins in Eastern Australia and their Relationship to the New England Orogen." In Basement Tectonics 9. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2654-0_5.

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Tanczyk, Elizabeth I. "Permian Tectonics from the Gulf of St. Lawrence: Evidence from Paleomagnetism." In Proceedings of the International Conferences on Basement Tectonics. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-017-0833-3_40.

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Actes de conférences sur le sujet "Permian tectonic"

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Riggs, Nancy R., Andrew P. Barth, J. Douglas Walker, et al. "IMPLICATIONS OF PERMIAN MAGMATISM IN SOUTHWEST LAURENTIA FOR TECTONIC RECONSTRUCTIONS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-279985.

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Song, Dongfang, Wenjiao Xiao, and Chunming Han. "LATE CARBONIFEROUS-PERMIAN SUBDUCTION-ACCRETION TECTONICS OF THE ALXA TECTONIC BELT (NW CHINA), SOUTHERN CENTRAL ASIAN OROGENIC BELT." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-317543.

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Soreghan, Gerilyn S., and Michael J. Soreghan. "TECTONIC AND CLIMATIC IMPLICATIONS OF CLASTIC DISPERSAL PATHWAYS IN THE PERMIAN MID-CONTINENT." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-282227.

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Gao, Zihui, and Nicholas Perez. "LATE PALEOZOIC TECTONIC FRAMEWORK OF THE SOUTH-CENTRAL REGION AND EVOLUTION OF THE PERMIAN BASIN." In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289647.

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Farag, Adel, Kirsten N. Nicholson, Shawn J. Malone, Jeffry D. Grigsby, and Eric S. Lange. "WHOLE ROCK CHEMISTRY AND TECTONIC EVALUATION OF PERMIAN- TRIASSIC SEVEN DEVILS JUVENILE ARC, WESTERN IDAHO." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321527.

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Taghdisi Nikbakht, S., Y. Nasiri, P. Rezaee, and R. Moussavi-Harami. "Provenance and Tectonic Setting of Early Permian Strata in the Kalmard Area, Central Iran Zone." In 83rd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202210808.

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Wenke, A., L. Rohrer, R. Zühlke, H. Kreuter, F. Spath, and S. Bißmann and E. Zöllner. "Tectonic Evolution, Reservoir Distribution and Hydrothermal Potential of the Permian in the Northern Upper Rhine Graben." In 1st Sustainable Earth Sciences Conference and Exhibition (SES2011). EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144132.

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Kennedy, Rebekah, Ryan J. McAleer, Phillip Resor, and Robert P. Wintsch. "THE ALLEGHANIAN TECTONIC SETTING OF THE ACADIAN HIGHLANDS OF WESTERN CONNECTICUT REVEALED BY PERMIAN INTRUSIVE FELSITES." In Northeastern Section - 57th Annual Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022ne-374611.

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Saldin, V. S. "The situation of studies of the Upper Paleozoic reefogenic formations on the Podcherem River (Bol'shaya Synya Depression, Pre-Urals Foredeep)." In All-Russia Lithological Meeting «Geology of reefs». Institute of Geology FRC Komi SC UB RAS, 2020. http://dx.doi.org/10.19110/98491-013-108-110.

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Different views on the Upper Paleozoic reefogenic limestones in the section of the Podcherem River during the period from 1960 to 2003 are presented. There are contradictory opinions of thickness, age, and section structure of the Upper Carboniferous (?) — Lower Permian reefogenic limestones of the Podcherem River. Underscore, a different interpretation of their paleogeographic position in the sedimentation basin and modern tectonic structure. To resolve controversial questions, focused research on theis reefogenic limestones is necessary.

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Kosmacheva, Alina Yu, Sergey S. Semenov, and Marina O. Fedorovich. "History of tectonic development and quantitative assessment of source rock generation power in the tolon field (Sakha Yakutia)." In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-013.

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The paper is aimed at the geoseismic interpretation, picking principal reflection horizons, structure and isopach map generation. The maps, seismic- and paleosections are an integral part not only of the structure-and-tectonic description, but also history analysis of the Tolon field. The research identifies gas-window-entry time of the Permian source rock, initial development and power of intense gas generation, present-day generation points in the source rocks. Funding: The reported study was funded by RFBR, project number 19-35-90039.

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Rapports d'organisations sur le sujet "Permian tectonic"

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Zagorevski, A., C. R. van Staal, J. H. Bédard, et al. Overview of Cordilleran oceanic terranes and their significance for the tectonic evolution of the northern Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326053.

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Ophiolite complexes are an important component of oceanic terranes in the northern Cordillera and constitute a significant amount of juvenile crust added to the Mesozoic Laurentian continental margin during Cordilleran orogenesis. Despite their tectonic importance, few systematic studies of these complexes have been conducted. Detailed studies of the pseudostratigraphy, age, geochemistry, and structural setting of ophiolitic rocks in the northern Cordillera indicate that ophiolites formed in Permian to Middle Triassic suprasubduction zone settings and were obducted onto passive margin sequence

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Theriault, P., and B. Beauchamp. Preliminary Interpretation of the Depositional History and Tectonic Significance of the Carboniferous To Permian Canyon Fiord Formation, West - Central Ellesmere Island, Arctic Archipelago. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132551.

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