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Bibliografías temáticas / Cimmerian blocs

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Artículos de revistas

Literatura académica sobre el tema "Cimmerian blocs"

Autor: Grafiati

Publicado: 25 de mayo de 2024

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Artículos de revistas sobre el tema "Cimmerian blocs"

1

Huang, Hao, Xiaochi Jin, and Yukun Shi. "Permian Fusulinid Rugososchwagerina (Xiaoxinzhaiella) from the Shan Plateau, Myanmar: Systematics and Paleogeography." Journal of Foraminiferal Research 50, no. 1 (2020): 11–24. http://dx.doi.org/10.2113/gsjfr.50.1.11.

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Abstract Eastern Myanmar is an indispensable part of the Cimmerian Continent with Gondwana provenance. Fusulinids from Eastern Myanmar remain poorly known despite their biochronological and paleogeographical significance. This paper describes Rugososchwagerina (Xiaoxinzhaiella) subrotunda sp. nov. and Chusenella quasidouvillei of Murgabian age (Middle Permian) from the Thitsipin Formation at the Pindaya in the Shan Plateau, Eastern Myanmar. Taxonomic analysis of this new collection and of Rugososchwagerina (s.l.) in the literature leads us to suppress Xiaoxinzhaiella Shi, Yang & Jin, 2005

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2

Larvet, Tiphaine, Laetitia Le Pourhiet, and Philippe Agard. "Cimmerian block detachment from Gondwana: A slab pull origin?" Earth and Planetary Science Letters 596 (October 2022): 117790. http://dx.doi.org/10.1016/j.epsl.2022.117790.

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3

Motuza, Gediminas, and Saulius Šliaupa. "Palaeogene plutonic magmatism in Central Afghanistan, and its relation to the India-Eurasia collision." Baltica 33, no. 2 (2020): 128–45. http://dx.doi.org/10.5200/baltica.2020.2.2.

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Numerous granitic intrusions occur along the southern margin of the Tajik Block and the Band-e-Bayan Zone in the Ghor Province of Central Afghanistan. Previously, they used to be linked to the Cimmerian igneous episodes of Triassic and Cretaceous ages. However, the new U-Pb dating has revealed that these granite intrusions occurred during the Eocene within a narrow time span of 41–36 Ma. They are related to the number of local depressions filled with the volcanic-sedimentary sequence of the same age. These data indicate an intense short-termed magmatic event that affected the region in the Pal

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4

Wilmsen, Markus, Franz Theodor Fürsich, Kazem Seyed-Emami, and Mahmoud Reza Majidifard. "The Upper Jurassic Garedu Red Bed Formation of the northern Tabas Block: elucidating Late Cimmerian tectonics in east-Central Iran." International Journal of Earth Sciences 110, no. 3 (2021): 767–90. http://dx.doi.org/10.1007/s00531-021-01988-z.

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AbstractThe Garedu Red Bed Formation (GRBF) of the northern Tabas Block (Central-East Iranian Microcontinent, CEIM) is a lithologically variable, up to 500-m-thick, predominantly continental unit. It rests gradually or unconformably on marine limestones of the Esfandiar Subgroup (Callovian–Oxfordian) and is assigned to the Kimmeridgian–Tithonian. In the lower part, it consists of pebble- to boulder-sized conglomerates/breccias composed of limestone clasts intercalated with calcareous sandstones, litho-/bioclastic rudstones and lacustrine carbonates. Up-section, sharp-based pebbly sandstones an

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5

KOZLENKO, M., and Yu KOZLENKO. "The structure of the lithosphere, tectonics and evolution of the Scythian Plate and adjacent structures in the section of the Bs05-22 profile (according to 2-d density modeling)." Geology and Mineral Resources of World Ocean 16, no. 3 (2020): 13–29. http://dx.doi.org/10.15407/gpimo2020.03.013.

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A density model was built along the Bs05-22 profile, which made it possible to identify individual blocks with different crustal parameters. The consolidated crust of the East European Platform (EEP) has a “key” structure. The southern boundary of the EEP is clearly fractured and falls to the south at an angle of about 83° The South Ukrainian monocline (SUM) covers not only the basement of the EEP but also the northern part of the Scythian Plate (SP). The central part of SP block overlapped by the SUM is characterized by the maximum capacity of the folded-metamorphic base. The axial part of th

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6

SPAHIĆ, Darko, and Tivadar GAUDENYI. "The role of the pre-Alpine polycrystalline basement in the paleogeographic configuration of multiple Neotethyan oceanic basins." Geologija 64, no. 2 (2021): 143–58. http://dx.doi.org/10.5474/geologija.2021.008.

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The study provides a deeper understanding of the early Mesozoic paleogeogeographic spatial-temporal relationship by studying the two Adria-Europe intervening basement blocks. The Drina-Ivanjica and Pelagonian crustal fragments play important role in the internal early Alpine oceanic constitution further controlling the late Jurassic emplacement of Tethyan Dinaric-Hellenic ophiolites. The proposed paleogeographic reassessment is driven by the new paleocontinental inheritance data associated with the Variscan – pre-Variscan basement terranes. The recently published data suggest an Avalonian-type

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7

Yichun, Zhang, Wang Yue, and Shen Shuzhong. "Middle Permian (Guadalupian) Fusulines from the Xilanta Formation in the Gyanyima area of Burang County, southwestern Tibet, China." Micropaleontology 55, no. 5 (2009): 463–86. http://dx.doi.org/10.47894/mpal.55.5.02.

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This paper reports a diversified fusuline fauna from the Middle Permian (Guadalupian) Xilanta Formation in the Gyanyima area, Burang County, southwestern Tibet, China. Nine genera, Lantschichites, Kahlerina, Nankinella, Yangchienia, Chusenella, Verbeekina, Armenina, Paraverbeekina and Neoschwagerina are recognized.Anew species Yangchienia gyanyimaensis n. sp. is established. This fauna indicates a Midian age in terms of the coexistence of Kahlerina, Lantschichites and Neoschwagerina. Paleobiogeographically, the fauna closely resembles that from the Lasaila exotic limestone block of Tibet, both

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8

Montenat, Christian. "The Mesozoic of Afghanistan." GeoArabia 14, no. 1 (2009): 147–210. http://dx.doi.org/10.2113/geoarabia1401147.

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ABSTRACT This paper is a review of the geology of the widely distributed Mesozoic rocks of Afghanistan. The country is a mosaic of structural blocks in a variety of geodynamic settings that were juxtaposed during the evolution of the Tethyan Ocean; the Mesozoic sedimentary, volcanic, and plutonic rocks therefore differ greatly from one block to another. Because of the adverse security situation, fieldwork has not been possible since the late 1970s and the data used in this review are therefore relatively old but are the best available. Interest in the geology of Afghanistan remains strong due

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9

Wang, Xiangdong, Mohammad N. Gorgij, and Le Yao. "A Cathaysian rugose coral fauna from the upper Carboniferous of central Iran." Journal of Paleontology 93, no. 3 (2018): 399–415. http://dx.doi.org/10.1017/jpa.2018.89.

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AbstractTwelve rugose coral species belonging to seven genera are described and discussed based on 70 thin sections of 32 specimens collected from the Anarak section, northeast of Nain, Esfahan Province, Yazd Block, central Iran. These species include two new colonial rugose coral species,Antheria fedorowskiiandAntheria robusta, and five previously named species of colonial rugose corals,Antheria lanceolataandStreptophyllidium scitulum, and solitary rugose corals,Arctophyllum jiangsiense,Caninophyllumcf.somtaiense, andPseudotimania delicata. Five species are left in open nomenclature:Antherias

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10

KOZLENKO, M. V., and Yu V. KOZLENKO. "Deep structure, tectonics, evolution and hydrocarbon potential of the north-western shelf of the Black Sea along 31°20’E." Geology and Mineral Resources of World Ocean 17, no. 3 (2021): 3–21. http://dx.doi.org/10.15407/gpimo2021.03.003.

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A density modeling of the north-western shelf of the Black Sea along 31°20’ E was carried out. According to its results, a complex block structure of the area is determined, which is closely connected with the history of its development. Signs of Baikal tectonic activation of the southern edge of the pre-Riphean Eastern European platform, as well as the adjacent part of the Scythian plate have been revealed. Areas formed during the Hercynian and Cimmerian epochs of tectogenesis have been identified within the Scythian plate. At the base of the Karkinit Trough, two areas of reduced crust result

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