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Journal articles on the topic 'Klippes'

Author: Grafiati

Published: 4 June 2021

Last updated: 4 February 2022

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1

ILUNGA YANTAMBWE, Maurice, and Jacques L. H. CAILTEUX. "Geological observations in the Five-Klippes area, northwestern Katanga Copperbelt (Democratic Republic of the Congo)." Geologica Belgica 22, no. 3-4 (2019): 111–19. http://dx.doi.org/10.20341/gb.2019.006.

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Surface mapping and exploration in the search license PR-2348, northwest of Kolwezi in the Neoproterozoic Katanga Copperbelt, focussed in the poorly documented Five-Klippes area, and showed that the Roan megabreccias occurring at the ground surface in the klippes are composed mostly of Musonoï, Mines (Kamoto Formation) and Kiubo rocks that form km- to mm-size blocks, fragments and matrix. The megabreccias are bordered by rocks of the Kiubo Formation, that are gently dipping south on the northern side, with few approximatively 10 m-size sharp refolding close to the megabreccia, while they are vertically dipping north on the southern side. A 262 m-long exploration core drilling performed under the megabreccia of one of the klippes highlighted a faulting marked by hydraulic-like fractured-deformed Kiubo rocks and by friction breccias. The Kiubo blocks, fragments and matrix in the megabreccia were teared out most likely from the southern limb of the fault. The faulting in depth is interpreted here as the roots of the ground surface megabreccia. This rupture and shearing is questioning the autochthonous character of the surrounding Kiubo and Mongwe rocks. It is suggested that, similarly as for the eastern Mamfwe anticline, the Nguba and Kundelungu groups succession in the klippes area constituted blocks thrust during the fold-and-thrust event of the Katangan orogeny, and extruded the megabreccias of the klippes before suture during the final stage of the northward compression. A nearly north-south transversal faulting and shearing crosscutting the limbs and megabreccias of the klippes marked the end of the compression. These new observations complement other similar ones in that region, and have important implications for future Cu-Co exploration.

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2

Fabbri, Olivier, Rémi Magott, Marc Fournier, and Lucas Etienne. "Pseudotachylyte in the Monte Maggiore ophiolitic unit (Alpine Corsica): a possible lateral extension of the Cima di Gratera intermediate-depth Wadati-Benioff paleo-seismic zone." BSGF - Earth Sciences Bulletin 189, no. 4-6 (2018): 18. http://dx.doi.org/10.1051/bsgf/2018020.

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At the northern end of the Cap Corse peninsula, several klippes of ultramafic rocks (peridotite and serpentinite), among which the Monte Maggiore klippe is the least serpentinized one, rest upon continental-crust derived rocks (Centuri gneisses) and basic or metasedimentary schists (Schistes Lustrés). The Monte Maggiore ophiolitic klippe shares several characteristics with the Cima di Gratera klippe located 30 km further south. First, the two units are composed of a lherzolitic peridotite. Second, they record the same succession of metamorphic events. Third, in the Cap Corse tectonic pile, the two units occupy the highest structural position. Several differences are also observed. First, mafic rocks are significantly less abundant in the Monte Maggiore unit, where they are restricted to dykes cross-cutting the peridotite, than in the Cima di Gratera unit, where they constitute an entire sub-unit. Second, pyroxenite layers are more common at Monte Maggiore than at Cima di Gratera. Despite these differences, the Monte Maggiore and Cima di Gratera klippes can be considered as possible lateral equivalents of a single ophiolitic unit having covered the entire Cap Corse before subsequent erosion. Pseudotachylyte of seismic origin is newly discovered in the Monte Maggiore klippe. The host rock is a cataclastic serpentinized peridotite affected by a cataclastic foliation that is either flat-lying or steeply dipping. Pseudotachylyte fault veins are parallel to the host rock cataclastic foliation. The small lateral extension and the small thickness of fault veins along with frequent cross-cutting relationships suggest that the exposed pseudotachylyte most likely results from numerous small magnitude seismic events such as swarms or aftershocks rather than from large magnitude shocks. All these characteristics are also observed at the Cima di Gratera klippe where they are interpreted as the testimonies of a fossil intermediate-depth Wadati-Benioff zone at the time of subduction of the Ligurian Tethys oceanic lithosphere. Mineral assemblages that could constrain the depth of formation of the pseudotachylyte lack in the Monte Maggiore area. Despite this uncertainty, and given the similarities with the Cima di Gratera occurrences, the pseudotachylyte veins newly discovered at Monte Maggiore are tentatively related to the seismic activity linked with the subduction of the Piemonte-Ligurian oceanic lithosphere in Eocene times. This interpretation suggests that the fossil Wadati-Benioff zone could be traced further south in Alpine Corsica and further north in the Piemontese zone of the western Alps.

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3

Antal, András, István Pósa, József Varga, Zoltán Kovács, and Gábor Nagy. "Egyszerűsített, gazdaságos laparoszkópos appendectomiar." Magyar Sebészet 60, no. 2 (April 1, 2007): 87–89. http://dx.doi.org/10.1556/maseb.60.2007.2.4.

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Absztrakt A szerzők ismertetik a laparoszkópos appendectomia jelenlegi megítélését. Bemutatják a klippes appendix csonk zárással egyszerűsített műtéti technikát. Beszámolnak az első ötven műtétben szerzett kedvező tapasztalataikról. A műtéti technika az endolooposnál egyszerűbb, gyorsabb, az endoszkópos varrógépesnél lényegesen olcsóbb. Az eredmények alapján az ismertetett endoszkópos műtétet a hagyományos appendectomia értékes alternatívájának tekintik.

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4

IVANOV, Kirill Svyatoslavich, and Victor Nikolaevich PUCHKOV. "On the stratigraphy and tectonics of Zilair synclinorium of the Urals." NEWS of the Ural State Mining University, no. 4 (December 20, 2020): 67–72. http://dx.doi.org/10.21440/2307-2091-2020-4-67-72.

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The purpose of the work was to study the tectonic structure of the Zilair synclinorium of the Western slope of the southern Urals, which is important both from the general scientific point of view and for the needs of oil and gas prospecting of the territory. The main method of research was a detailed study of the stratigraphy of key sites with the search for conodonts in siliceous rocks. We also used data from seismic profiling of the territory. Result of work. The Zilair synclinorium of the southern Urals is an asymmetrically different facies structure; its Western and Eastern wings are composed of deposits belonging to different facies zones – the shelf (neritic) in the West and the continental slope and rise (bathyal) in the East. In the axial zone of the synclinorium, among the Famennian graywacke deposits of the Zilair series, several sites composed of cherts are known. It was believed, that the cherts are of Silurian age and are the klippes of a very large overthrust belonging to the ophiolite association. According to occurences of conodonts, we have established that all these cherts have Devonian, mainly Frasnian age. They are not klippes of an overthrust, but the central parts of the anticlinal folds, complicated by steep thrusts. According to our data, the real overthrust with a great horizontal amplitude is Pokrovsky, where two facial zones come into an abrupt contact without any transition between them.

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5

Kravchuk, Yaroslav, Roman Hnatiuk, Myroslav Ivanyk, and Yaroslav Khomyn. "General features of relief of Marmaroshi and Pieniny rocks of Ukrainian Carpathians and their place under system of geomorphological regionalization." Visnyk of the Lviv University. Series Geography, no. 42 (October 15, 2013): 204–20. http://dx.doi.org/10.30970/vgg.2013.42.1860.

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Peculiarities of geological structure and relief of Ukrainian fragment of zones of Marmaroshi and Pieniny rocks located between Outer (Flysch) and Inner Carpathians are considered. Morphostructural differences and common features of relief of these zones are clarified. Territory of zones of Marmaroshi and Pieniny rocks is considered as separate geomorphological region of mountain part of Ukrainian Carpathians – subregion of Intermountain Valleys and Rocky Chains. Expediency of separation and taxonomic class of this geomorphological region are proved, its division into taxonomic units of lower class is realized. Key words: Marmaroshi rocks, Pieniny rocks, klippes (limestone rocks of Jurassic period), morphostructure, geomorphological regionalization, Ukrainian Carpathians.

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6

Puniya, M. K., R. C. Patel, and P. D. Pant. "Structural and thermochronological studies of the Almora klippe, Kumaun, NW India: implications for crustal thickening and exhumation of the NW Himalaya." Geological Society, London, Special Publications 481, no. 1 (December 19, 2018): 81–110. http://dx.doi.org/10.1144/sp481-2017-74.

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AbstractCrystalline klippen over the Lesser Himalayan Metasedimentary Sequence (LHMS) zone in the NW Himalaya have specific syn- and post-emplacement histories. These tectonics also provide a means to understand the driving factors responsible for the exhumation of the rocks of crystalline klippen during the Himalayan Orogeny. New meso- and microscale structural analyses, and thermochronological studies across the LHMS zone, Ramgarh Thrust (RT) sheet and Almora klippe in the eastern Kumaun region, NW Himalaya, indicate that the RT sheet and Almora klippe were a part of the Higher Himalayan Crystalline (HHC) of the Indian Plate which underwent at least one episode of pre-Himalayan deformation and polyepisodic Himalayan deformation in ductile and brittle–ductile regimes. The deformation temperature pattern within the Almora klippe records a normal thermal profile from its base to top but an inverted thermal profile from the base of Almora klippe down towards the LHMS zone. New fission-track data collected across the RT sheet and Almora klippe along Chalthi–Champawat–Pithoragarh traverse in the east Kumaun region document the exhumation of both units since Eocene times. Zircon fission-track (ZFT) ages from the Almora klippe range between 28.7 ± 2.4 and 17.6 ± 1.1 Ma, and from the RT sheet between 29.8 ± 1.6 and 22.6 ± 1.9 Ma; and the apatite fission-track (AFT) ages from the Almora klippe range between 15.1 ± 1.7 and 3.4 ± 0.5 Ma, and from the RT sheet between 8.7 ± 1.2 and 4.6 ± 0.6 Ma. The age pattern and diverse patterns of the exhumation rates reflect a clear tectonic signal in the RT sheet and the Almora klippe which acknowledge that the Cenozoic tectonics influenced the exhumation pattern in the Himalaya.

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7

Liu, Demin, Weiran Yang, Tieying Guo, Jiangtao Ru, and Aimin Xiong. "Discussion on the Cenozoic tectonic evolution and dynamics of southern Tibet." Earth sciences and subsoil use 43, no. 3 (October 7, 2020): 307–24. http://dx.doi.org/10.21285/2686-9993-2020-43-3-307-324.

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Opening-closing tectonics is a new idea for exploring the global tectonics, which holds that every tectonic movement of all materials and geological bodies on earth is characterized by opening and closing. The opening-closing tectonic view can be used to explain some geological phenomena developing in continents which cannot be reasonably explained by the theory of plate tectonics. Based on the available basic geological data and combining with the opening-closing view, we analyzed the divisions and characteristics of tectonic units in South Tibet, and propose that Tibet can be divided into gravitational detachment and detachment fault zones, which are superimposed thrust fault zones and reconstructed normal fault zones, respectively. Although the mainstream opinion believed that the Tibetan Plateau is formed by collision-compression orogenesis, field investigation revealed the existence of the Rongbu Temple normal fault in the 1970s. We consider that the Rongbu Temple normal fault and the Main Central Thrust were formed earlier than the South Tibet detachment fault, and the former two faults constitute the two boundaries of the southern Tibet extrusion structure. The South Tibet detachment fault partially superimposes on the Main Central Thrust and manifests a relatively high angle in following the Rongbu Temple normal fault north of the Chomolangma. We suggest that the three fault systems are the products of different periods and tectonic backgrounds. The tectonic units, such as klippes and windows identified by previous researchers in southern Tibet, belong to thrust fault system but usually have no obvious extrusion or thrust characteristics; however, they are characterized by missing strata columns as younger strata overlapping the older ones. These klippes and windows should be the results of later gravitational decollement and must be characterized as extensions and slips, respectively. Based on opening-closing theory, we suggest that since the Cenozoic the study area had undergone multistage development, which can be divided into the oceanic crust expansion (opening) and subduction (closing) and the continental collision (closing) and intracontinental extension (opening) stages. Geothermal energy from the deep earth, gravitational potential energy from the earth’s interior, and additional stress energy from tectonic movements, all played a key role in the multistage tectonic evolutionary process.

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8

Saksa, Martin, and Jozef Minár. "Assessing the natural hazard of gully erosion through a Geoecological Information System (GeIS): a case study from the Western Carpathians." Geografie 117, no. 2 (2012): 152–69. http://dx.doi.org/10.37040/geografie2012117020152.

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The development of gullies represents a specific type of fluvial erosion that is triggered when surface runoff becomes concentrated during extreme rainfall events. This study investigates a part of the Považské Valley and Strážovské Mountains in Slovakia to assess the potential susceptibility and gully erosion hazard using a Geoecological Information System (GeIS). The landscape of the area was studied through primary field research and the analysis of secondary materials. The GeIS was then constructed in order to undertake specific multidimensional statistical methods. These were used to assess the potential susceptibly and gully erosion hazard. Those areas with the greatest potential susceptibility occur in Butkovská Furrow and the Podmanínska Hills whilst those with the least potential susceptibility occur in Butkovské Klippes and the Trenčianska Upland. The greatest gully erosion hazard was identified on arable land in the Podmanínska Hills and on the river terraces in the Ilavská Basin. It is clear that the majority of the permanent gullies within the study area are controlled by the course of existing anthropogenic linear features such as unpaved field and forest roads and balks in arable land.

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9

de Wever, P., G. Duee, and K. El Kadiri. "Les series stratigraphiques des klippes de Chrafate (Rif septentrional, Maroc); temoins d'une marge continentale subsidente au cours du Jurassique-Cretace." Bulletin de la Société Géologique de France I, no. 3 (May 1, 1985): 363–79. http://dx.doi.org/10.2113/gssgfbull.i.3.363.

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10

Dommergues, Jean-Louis, and Christian Meister. "Succession des faunes d'Ammonites du Sinémurien supérieurdans le Chablais méridional et les Klippes de Savoie (Préalpes Médianes, Haute-Savoie, France)." Geobios 22, no. 4 (January 1989): 455–83. http://dx.doi.org/10.1016/s0016-6995(89)80099-3.

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11

Richter, Dieter (gest )., Arne Mihm, and Carla Müller. "The Pelagonian Klippes on the Flysch of the East-Pindos Synclinorium (Pindos Zone) west of the Iti Mountains (Central Greece)." Zeitschrift der Deutschen Geologischen Gesellschaft 148, no. 2 (September 8, 1997): 237–46. http://dx.doi.org/10.1127/zdgg/148/1997/237.

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12

Dommergues, J. L., and C. Meister. "De la "grosse pierre des encombres" aux klippes de Suisse centrale; un test d'homogeneite des paleoenvironnements subbrianconnais et des contraintes paleobiogeographiques alpines par les ammonites du Lias moyen (Jurassique inferieur)." Bulletin de la Société Géologique de France VI, no. 4 (July 1, 1990): 635–46. http://dx.doi.org/10.2113/gssgfbull.vi.4.635.

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13

Ślączka, Andrzej, Marta Bąk, Clemens Pfersmann, Veronika Koukal, Michael Wagreich, Szymon Kowalik, and Martin Maslo. "Jurassic–Cretaceous radiolarian-bearing strata from the Gresten Klippen Zone and the St. Veit Klippen Zone (Wienerwald, Eastern Alps, Austria): Implications for stratigraphy and paleogeography." Austrian Journal of Earth Sciences 111, no. 2 (December 1, 2018): 204–22. http://dx.doi.org/10.17738/ajes.2018.0013.

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AbstractTwo sections of the klippen zones in the Wienerwald area have been investigated for their stratigraphy: (1) The Gern section of the Main Klippen Zone, a part of the Gresten Klippen Zone, and (2) the St. Veit Klippen Zone in the Lainz Tunnel and the neighboring outcrops in western Vienna. New biostratigraphic data are based on radiolaria from siliceous intervals and a few findings of calcareous nannofossils from marlstones. In the Gresten Klippen Zone, radiolarian assemblages from limestones of the Gern locality indicate a middle Oxfordian to early Kimmeridgian age of the Scheibbsbach Formation.Radiolarian and nannofossil data from the St. Veit Klippen Zone in the Lainz railway tunnel locality, as well as correlated outcrops from the Lainzer Tiergarten and the Gemeindeberg in the southwest of Vienna, indicate the presence of mainly Bajocian to lower Oxfordian red radiolarites and cherts (Rotenberg Formation). Siliceous, grey limestones and cherts of the Fasselgraben Formation range from the upper Oxfordian–Kimmeridgian to the Valanginian–Barremian.The Main Klippen Zone was derived from the European margin to the north, and this zone is regarded as a Helvetic paleogeographic unit. The St. Veit Klippen Zone in the Lainz Tunnel section contains no ophiolitic material and shows a tectonic contact with the surrounding Rhenodanubian nappe system, which indicates no primary sedimentary contact of the St. Veit Klippen Zone with the Flysch units, as well as demonstrating the presence of two structurally separated Alpine tectonic units. Thus, a direct correlation with the Ybbsitz Zone is not supported, and an original paleogeographic position in the transition from the Penninic Ocean to the Austroalpine continental fragment is proposed.

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14

Keepanasseril, Anish, K. Keerthana, Arun Keepanasseril, Dilip K. Maurya, D. Kadambari, and Sharath Sistla. "Pregnancy in women with Klippel-Trenaunay syndrome: Report of three pregnancies in a single patient and review of literature." Obstetric Medicine 10, no. 4 (September 13, 2017): 177–82. http://dx.doi.org/10.1177/1753495x17719181.

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Klippel-Trenaunay syndrome is characterised by vascular abnormality which increases the risk of thromboembolism and haemorrhage. Physiological changes in pregnancy pose an increased risk to these complications. Being an uncommon disorder, there is limited literature about the management of women with pregnancy and Klippel-Trenaunay syndrome. We report in detail two of three pregnancies in a woman with Klippel-Trenaunay syndrome who had repeated episodes of haematochezia leading to anaemia, managed with Argon laser Photo-Coagulation in pregnancy and also reviewed the complications and the management of pregnant women with Klippel-Trenaunay syndrome.

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15

Farias, Luis Arthur Brasil Gadelha, Mariana Fátima Cabral De Oliveira, Maycon Fellipe Da Ponte, and Aglaerton Silva Pinheiro. "TROMBOEMBOLISMO PULMONAR EM PACIENTE COM SÍNDROME DE KLIPPEL-TRENAUNAY-WEBER: RELATO DE CASO." Revista de Patologia do Tocantins 5, no. 2 (September 8, 2018): 55–57. http://dx.doi.org/10.20873/uft.2446-6492.2018v5n2p55.

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RESUMO A síndrome de Klippel-Trenaunay-Weber (KTW) é uma doença rara caracterizada por distúrbio vascular com malformação capilar, venosa e linfática, grandes hemangiomas e hipertrofia óssea ou de tecidos moles. Relatamos o caso de uma mulher de 24 anos de idade, obesa, com história prévia de linfedema e hemangioma unilateral da perna direita que evoluiu com tromboembolismo pulmonar. Ela possuia diagnóstico clínico e ultrassonográfico de síndrome de Klippel-Trenaunay-Weber há 5 anos. Após a anticoagulação, a paciente evoluiu assintomática e sem novos eventos tromboembólicos. Palavras-chave: Síndrome de Klippel-Trenaunay-Weber; Embolia Pulmonar; Tromboembolia; Tromboembolia Venosa. ABSTRACT Klippel-Trenaunay-Weber syndrome (KTW) is a rare disease characterized by vascular disorder with capillary, venous and lymphatic malformation, large hemangiomas and bone or soft tissue hypertrophy. Herein we report the case of a 24-years-old women, obese, with previous history of unilateral lymphedema and hemangioma in right leg witch evolves to pulmonar tromboembolism. She had clinical and ultrasonographic diagnosis of Klippel-Trenaunay-Weber Syndrome five years before. After anticoagulation, the patient evolves assymptomatic and without new tromboembolic events. Keywords: Klippel-Trenaunay-Weber Syndrome; Pulmonary Embolism; Thromboembolism; Venous Thromboembolism.

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16

Peeters, Piet-hein. "Klippen." Zorg + Welzijn 23, no. 1-2 (January 2017): 7. http://dx.doi.org/10.1007/s41185-017-0002-x.

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17

Ivanitskaya, Olga, Elena Andreeva, and Natalia Odegova. "Prenatal diagnosis of Klippel–Trenaunay syndrome: Series of four cases and review of the literature." Ultrasound 28, no. 2 (October 17, 2019): 91–102. http://dx.doi.org/10.1177/1742271x19880327.

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Klippel–Trenaunay syndrome is a rare disease with a classic triad of port wine stains, varicose veins, and bony and soft tissue hypertrophy of an extremity. The quality of life in these patients is significantly affected, making the prenatal diagnosis of Klippel–Trenaunay syndrome important. We present four prenatally diagnosed cases of this anomaly with a unique case of ectrodactyly of the hand in foetus with Klippel–Trenaunay syndrome. Such a combination has not been previously reported prenatally. A review of the literature for similar cases is also presented.

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18

Clarke, Raymond A., Pamela J. Davis, and John Tonkin. "Klippel-Feil Syndrome Associated with Malformed Larynx." Annals of Otology, Rhinology & Laryngology 103, no. 3 (March 1994): 201–7. http://dx.doi.org/10.1177/000348949410300306.

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We report a case of a 45-year-old man with Klippel-Feil syndrome with fusion of the C2–3 and C4–5 cervical vertebrae and severe voice impairment associated with malformation of the laryngeal cartilages. The condition was also complicated by bilateral inflexibility of the arms and legs and external malformation of the ears. This case broadens the spectrum of anomalies, of branchial arch derivation, now identified in association with Klippel-Feil syndrome. We discuss the possibility that perturbation of segmentation, distinct from somitogenesis, may be linked to Klippel-Feil syndrome—associated craniofacial abnormalities.

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Seth, Raghav, Anindita Sinha, Navneet Singla, and Debajyoti Chatterjee. "Rare cause of paraparesis in a young man: cervico-dorsal neurenteric cysts associated with Klippel-Feil syndrome." BMJ Case Reports 14, no. 3 (March 2021): e235327. http://dx.doi.org/10.1136/bcr-2020-235327.

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Klippel-Feil syndrome is an entity presenting with short neck, low hairline and reduced range of motion of cervical spine. Neurenteric cyst is a congenital abnormality, in which mucus-secreting epithelium of the gastrointestinal tract is seen in the spinal axis. The association of a neurenteric cyst with Klippel-Feil syndrome has been reported very rarely. We report the case of a young man, affected by Klippel-Feil syndrome, who presented with bilateral paraplegia. Imaging of the spine revealed features suggestive of cervico-dorsal neurenteric cyst. Subsequently, surgical resection of the cysts was done, which resulted in resolution of the symptoms.

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20

Mneimneh, Sirin, Ali Tabaja, and Mariam Rajab. "Klippel-Trenaunay Syndrome with Extensive Lymphangiomas." Case Reports in Pediatrics 2015 (2015): 1–6. http://dx.doi.org/10.1155/2015/581394.

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Klippel-Trenaunay syndrome (KTS) is a rare disorder characterized by the triad of vascular malformations, venous varicosities, and bone and soft-tissue hypertrophy. We present a case of Klippel-Trenaunay syndrome with limb hypertrophy, port-wine stains, lymphangiomas, and venous varicosities in the limbs.

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21

Anand, Pradeep S., and T. Roshna. "Rare Instance of Gingival Enlargement in Klippel-Trenaunay Syndrome: A Case Report." Journal of Contemporary Dental Practice 7, no. 3 (2006): 92–98. http://dx.doi.org/10.5005/jcdp-7-3-92.

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Abstract Klippel-Trenaunay Syndrome is a rare congenital malformation that may include port-wine stain, soft tissue and bony hypertrophy, and venous malformations and lymphatic abnormalities. Although it usually involves the limbs, it may also rarely involve the head, neck, and orofacial regions. Despite its rarity, Klippel-Trenaunay Syndrome should be considered in the differential diagnosis of gingival enlargement. The condition can be easily recognized clinically, but further investigations including imaging studies have to be carried out in order to better understand the nature of the lesion. This report describes a case of gingival enlargement in Klippel- Trenaunay Syndrome in a 16-year-old female patient. The diagnosis of the condition was made based on the patient history, clinical and radiographic examination, computed tomography (CT), and angiogram. Citation Anand PS, Roshna T. Rare Instance of Gingival Enlargement in Klippel-Trenaunay Syndrome: A Case Report. J Contemp Dent Pract 2006 July;(7)3:092-098.

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22

Soucy La Roche, Renaud, Laurent Godin, John M. Cottle, and Dawn A. Kellett. "Preservation of the Early Evolution of the Himalayan Middle Crust in Foreland Klippen: Insights from the Karnali Klippe, West Nepal." Tectonics 37, no. 5 (May 2018): 1161–93. http://dx.doi.org/10.1002/2017tc004847.

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23

Patel, Prakash R., and William C. Lauerman. "Maurice Klippel." Spine 20, no. 19 (October 1995): 2157–60. http://dx.doi.org/10.1097/00007632-199510000-00016.

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24

Maelicke, Bernd. "Wie Wasser von Klippe zu Klippe geworfen." Forensische Psychiatrie, Psychologie, Kriminologie 5, no. 4 (September 30, 2011): 215–18. http://dx.doi.org/10.1007/s11757-011-0131-6.

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25

Zhao, Zhi Gen, Jia Chen, and Jia Ping Yan. "Features of Jianshanchong Klippe and its Control to Gas Geology at Qingshan Coal Mine, Jiangxi Province." Applied Mechanics and Materials 164 (April 2012): 501–5. http://dx.doi.org/10.4028/www.scientific.net/amm.164.501.

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The coal and gas outburst is serious at Qingshan Coal Mine of Jiangxi Province, so it is of significance to research the features of Jianshanchong klippe and its control to gas geology. The research reveals that: Jianshanchong klippe is distributed from the east boundary of Qingshan Coal Mine to No. 45 Exploration Line, its transverse profile is like a funnel while its longitudinal profile is like a wedge, northwest side of the klippe is thicker and deeper while southeast side is thinner and more shallow. Because of the cover and insert of Jianshanchong klippe, the structure of coal-bearing strata is more complex, some secondary folds are formed, and also, the coal seam is changed greatly, the tectonic coal is well developed and the coal seam is suddenly thickening or thinning. Due to the effect of Jianshanchong klippe, the coal and gas outbursts occur in the area of secondary folds, thicker coal seams or tectonic coals. Concerning the prediction of gas geology in deep area, in view of the facts including simpler structure, stable coal seam and decreased thickness, the gas emission rate and the coal and gas outburst will decrease in Fifth and Sixth Mining Level than that in Second and Third Mining Level

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26

Nagib, Mahmoud G., David A. Larson, Robert E. Maxwell, and Shelly N. Chou. "Neuroschisis of the Cervical Spinal Cord in a Patient with Klippel-Feil Syndrome." Neurosurgery 20, no. 4 (April 1, 1987): 629–31. http://dx.doi.org/10.1227/00006123-198704000-00022.

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Abstract During the neurological work-up of a young patient with Klippel-Feil syndrome, the presence of a neuroschisis of the cervical spinal cord was detected. The patient presented with a transient and acute hemisensory loss and a Horner's syndrome of the opposite side. The unusual presentation and radiological findings in a patient with Klippel-Feil syndrome prompted this report.

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27

Diekmann-Guiroy, Bernadette, and Peter S. Huang. "Klippel-Feil Syndrome in Association with a Craniocervical Dermoid Cyst Presenting as Aseptic Meningitis in an Adult: Case Report." Neurosurgery 25, no. 4 (October 1, 1989): 652–55. http://dx.doi.org/10.1227/00006123-198910000-00025.

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Abstract Intracranial tumors associated with Klippel-Feil syndrome usually occur in children, with spinal tumors being more common in adults affected by the syndrome. A rare case of a dermoid cyst at the craniocervical junction presenting as aseptic meningitis in an adult with Klippel-Feil syndrome is described. A review of the literature on tumors associated with this syndrome is also presented.

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28

Cakiroglu, Yigit, Emek Doğer, Sule Yildirim Kopuk, Yasemin Dogan, Eray Calıskan, and Gülseren Yucesoy. "Sonographic Identification of Klippel-Trenaunay-Weber Syndrome." Case Reports in Obstetrics and Gynecology 2013 (2013): 1–3. http://dx.doi.org/10.1155/2013/595476.

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Klippel-Trenaunay-Weber syndrome is a rare cutaneous vascular disorder characterized by the presence of multiple hemangiomata, arteriovenous fistulas, and limb hypertrophy. We report the prenatal sonographic findings in a case of Klippel-Trenaunay-Weber (KTW) syndrome including fetal limb hypertrophy and large subcutaneous cystic lesions. Prenatal diagnosis is possible by ultrasound examination and recognition important for prevention of complications and future management.

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29

Colpron, Maurice, Kaesy Gladwin, Stephen T. Johnston, James K. Mortensen, and George E. Gehrels. "Geology and juxtaposition history of the Yukon-Tanana, Slide Mountain, and Cassiar terranes in the Glenlyon area of central Yukon." Canadian Journal of Earth Sciences 42, no. 8 (August 1, 2005): 1431–48. http://dx.doi.org/10.1139/e05-046.

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In central Yukon, the pericratonic YukonTanana terrane (YT) is juxtaposed with the Cassiar terrane (CT, parautochthonous North America) along the Tummel fault zone (TFZ), a 34 km wide, northwest-trending belt comprising imbricate fault slices of Slide Mountain terrane (SM, greenstone, chert, serpentinite) and synorogenic clastic rocks. Northeast of the TFZ, the CT comprises Paleozoic metapelitic rocks, marble, and amphibolite of continental margin affinity. To the southwest, the YT consists of a pre-Late Devonian metasedimentary complex overlain and intruded by Mississippian clastic, volcanic, and plutonic successions of continental arc affinity. In the TFZ, Middle to Late Permian ocean-floor basalt of the SM shows evidence of crustal contamination, suggesting deposition at the edge of a marginal ocean basin. Deformation features in the TFZ include early ductile fabrics overprinted by younger brittle structures. Triassic synorogenic clastic rocks in the TFZ, and at the base of a klippen above the YT, suggest that terrane imbrication began shortly after the Early Triassic. 40Ar/39Ar mica ages from the region suggest cooling of the YT, SM, and part of CT below 300 °C by Early Jurassic time. Pervasive brittle structures in the Ragged Lake klippe, which roots into the TFZ, indicate brittle thrusting of the SM over the CT in post-Triassic time. Early Cretaceous plutons intrude the CT (Glenlyon Batholith) and the TFZ (leucogabbro) and impose a contact aureole that extends westward into the YT. Steep brittle structures that deformed the TFZ also affect, in part, the Glenlyon Batholith but do not significantly offset its contact aureole. Consequently, little displacement can have occurred along the TFZ after Early Cretaceous time.

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30

Ballhause, Tobias M., Mirko Velickovic, Darius M. Thiesen, and Marc Dreimann. "Congenital deformation of the posterior arch of the atlas: Subluxation of the atlanto-axial joint with temporary quadriplegia." SAGE Open Medical Case Reports 7 (January 2019): 2050313X1882338. http://dx.doi.org/10.1177/2050313x18823387.

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Instabilities of the craniocervical junction can be of rheumatic, traumatic, or congenital origin. The reported patient has a congenital malformation of the cervical spine, which is frequently observed in patients with Klippel–Feil syndrome. Her posterior arch of the atlas (C1) is hypoplastic and a chronic subluxation of the atlanto-axial joint would be possible. Although most common fusions in Klippel–Feil syndrome patients exist at C2/3, the majority of studies about Klippel–Feil syndrome deal with pediatric or adolescent individuals. Through extreme flexion of her neck, there was a compression of the spinal cord by the odontoid process. This led to a quadriplegia lasting about 10 min. Over the following weeks, all of her symptoms started to diminish. This situation turned out to be the third episode involving temporary neurological disorders in this 60-year-old female’s life.

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31

Subramaniam, Priya, KL Girish Babu, and Sony Sugnani. "Rare Association of Klippel Feil Syndrome with Cleft Palate and Congenital Cardiac Deformities: A Case Report." Journal of Clinical Pediatric Dentistry 35, no. 2 (December 1, 2010): 213–16. http://dx.doi.org/10.17796/jcpd.35.2.y803m42274301u65.

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Klippel Feil Syndrome comprises of three characteristic deformities of short neck, a low dorsal hair line and restricted neck mobility. This is a case report of Klippel Feil Syndrome and its rare association with cleft of hard and soft palate, coarctation of aorta, dextrocardia and situs inversus. An interdisciplinary approach towards the management included cardiac surgery, cleft repair and complete oral rehabilitation of the patient. Presently the patient is undergoing speech therapy and is under regular follow up.

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Khan, Imad Saeed, Osama Ahmed, Jai Deep Thakur, Cedric D. Shorter, and Bharat Guthikonda. "Craniocervical arachnoid cyst in a patient with Klippel-Feil syndrome: a unique case." Journal of Neurosurgery: Spine 18, no. 2 (February 2013): 161–64. http://dx.doi.org/10.3171/2012.11.spine12463.

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Klippel-Feil syndrome, or brevicollis, is a complex congenital disorder caused by the improper segmentation of the cervical vertebrae. The authors present the very rare case of a patient with Klippel-Feil syndrome who presented with an intradural arachnoid cyst at the craniocervical junction. They also examine possible factors contributing to this association. A 46-year-old woman presented with complaints of progressively worsening headaches and dizziness of 18 months' duration. She also demonstrated mild bilateral upper-extremity weakness. Magnetic resonance imaging revealed fused cervical vertebrae and a dorsal intradural arachnoid cyst at the craniocervical junction, extending down to the fourth cervical level. Because of worsening myelopathy and the presence of brainstem compression, the patient underwent surgical excision of the arachnoid cyst, which was approached via a midline posterior suboccipital/upper cervical route. An endoscope was introduced through a gap between the occiput and fused upper cervical vertebrae, and the arachnoid cyst was widely fenestrated. Postoperatively, the patient has remained symptom free for more than 2 years with evidence of good radiological decompression. The authors report a unique association between craniocervical arachnoid cyst and Klippel-Feil syndrome. To their knowledge, no other cases of this association have been reported in the literature. Arachnoid cysts should be part of the differential diagnosis in the presence of worsening myelopathic symptoms or pain in patients with Klippel-Feil syndrome.

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Usta, Sefer. "Klippel Trenaunay syndrome." Turkish Journal of Thoracic and Cardiovascular Surgery 21, no. 1 (January 20, 2013): 179–82. http://dx.doi.org/10.5606/tgkdc.dergisi.2013.4861.

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34

Mahmoud, Somaia Fathy, Mohamed O. El-Benhawi, M. Hany El-Tonsy, and S. M. Kalantar. "Klippel-Trenaunay syndrome." Journal of the American Academy of Dermatology 18, no. 5 (May 1988): 1169–72. http://dx.doi.org/10.1016/s0190-9622(88)70118-8.

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35

Ozoh, J. O., L. D. R. Tsatsi, and H. B. Broudie. "Klippel-Feil syndrome." South African Journal of Radiology 6, no. 3 (September 30, 2002): 30–31. http://dx.doi.org/10.4102/sajr.v6i3.1433.

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We present a 38-year-old male patient who sustained a minor and superficial stab injury in the left flank as well as a laceration on the scalp overlying the right parietal bone. On examination the classical triad of Klippel-Feil syndrome (short neck, low posterior hair line, limitation of neck movements) were observed. Further investigations revealed a plethora of congenital anomalies, including atlanto-occipital fusion, basilar impression, congenital fusion of CS and C6 vertebrae, scoliosis with convexity to the right side, complete situs inversus, and bilateral pelvic kidneys. Despite these multiple anomalies our patient still lives a relatively normal life and only sought medical help after minor injuries sustained during a brawl, for which he was treated in the hospital and discharged the following day.

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36

Gulati, YS, K. Pathak, SS Naware, and RS Negi. "Klippel - Trenaunay Syndrome." Medical Journal Armed Forces India 60, no. 1 (January 2004): 73–74. http://dx.doi.org/10.1016/s0377-1237(04)80167-9.

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37

John, Philip R. "Klippel-Trenaunay Syndrome." Techniques in Vascular and Interventional Radiology 22, no. 4 (December 2019): 100634. http://dx.doi.org/10.1016/j.tvir.2019.100634.

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38

Smith, Brent A., and Christopher Griffin. "Klippel-feil syndrome." Annals of Emergency Medicine 21, no. 7 (July 1992): 876–79. http://dx.doi.org/10.1016/s0196-0644(05)81038-8.

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39

Tracy, M. R., J. P. Dormans, and K. Kusumi. "Klippel-Feil Syndrome." Clinical Orthopaedics and Related Research 424 (July 2004): 183–90. http://dx.doi.org/10.1097/01.blo.0000130267.49895.20.

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40

Greipp, Mary Elizabeth. "Klippel-Feil Syndrome." Orthopaedic Nursing 11, no. 5 (September 1992): 13–18. http://dx.doi.org/10.1097/00006416-199209000-00004.

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41

Meier, Susan. "Klippel—Trenaunay Syndrome." Advances in Neonatal Care 9, no. 3 (June 2009): 120–24. http://dx.doi.org/10.1097/anc.0b013e3181a68b15.

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42

Auluck, A., S. Suhas, and KM Pai. "Klippel-Trenaunay syndrome." Oral Diseases 11, no. 4 (July 2005): 255–58. http://dx.doi.org/10.1111/j.1601-0825.2005.01072.x.

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43

Frikha, Rim. "Klippel-Feil syndrome." Clinical Dysmorphology 29, no. 1 (January 2020): 35–37. http://dx.doi.org/10.1097/mcd.0000000000000301.

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44

Pawel, B. R. "Klippel-Trenaunay syndrome." Archives of Disease in Childhood 90, no. 11 (November 1, 2005): 1127. http://dx.doi.org/10.1136/adc.2005.082784.

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45

Capraro, Philippe A., Jay Fisher, Dennis C. Hammond, and John A. Grossman. "Klippel-Trenaunay Syndrome." Plastic and Reconstructive Surgery 109, no. 6 (May 2002): 2052–62. http://dx.doi.org/10.1097/00006534-200205000-00041.

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46

Naik, R. S. "Klippel-Trenaunay Syndrome." Indian Journal of Surgery 69, no. 4 (August 2007): 158–59. http://dx.doi.org/10.1007/s12262-007-0011-7.

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47

Hachem, Laureen D., Francois Mathieu, Maria Lamberti-Pasculli, Brian W. Hanak, Reinhard Zeller, Abhaya V. Kulkarni, James Drake, and George M. Ibrahim. "Klippel Feil Syndrome." SPINE 45, no. 11 (June 2020): 718–26. http://dx.doi.org/10.1097/brs.0000000000003368.

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48

Kumar, K. Jagadish, Abhishek Chavan, Mitun Jain, V. G. Manjunath, and Perumal Satya. "Klippel Trenaunay syndrome." Sri Lanka Journal of Child Health 41, no. 4 (December 5, 2012): 209. http://dx.doi.org/10.4038/sljch.v41i4.4991.

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49

Berry, Susan A., Carrie Peterson, William Mize, Kenneth Bloom, Christopher Zachary, Peter Blasco, and David Hunter. "Klippel-Trenaunay syndrome." American Journal of Medical Genetics 79, no. 4 (October 2, 1998): 319–26. http://dx.doi.org/10.1002/(sici)1096-8628(19981002)79:4<319::aid-ajmg15>3.0.co;2-u.

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50

Cohen, M. Michael. "Klippel-Trenaunay syndrome." American Journal of Medical Genetics 93, no. 3 (2000): 171–75. http://dx.doi.org/10.1002/1096-8628(20000731)93:3<171::aid-ajmg1>3.0.co;2-k.

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