Relevant bibliographies by topics / Tectonic factors

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Tectonic factors'

Author: Grafiati
Published: 4 June 2021
Last updated: 12 February 2022

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Journal articles on the topic "Tectonic factors"

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Chandra ; Jonathan Hans Yoas Sihotang, Jansen. "SOPO BATAK TOBA RESILIENCE TECTONICS TOWARD EARTHQUAKE STUDY OBJECT: SOPO NAGARI SIHOTANG." Riset Arsitektur (RISA) 3, no. 03 (2019): 222–39. http://dx.doi.org/10.26593/risa.v3i03.3333.222-239.

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Abstract- Sopo is a granary house in traditional Batak Toba architecture. Sopo is important for Batak Toba community because it serves as a place to store rice which is the source of life. Nowadays sopo is harder to find than ruma. Most of the sopo has transformed into Batak Toba house and uses as a residence. Sopo is located in Lake Toba, North Sumatra, which is prone to earthquakes. Sopo Nagari Sihotang was built in the 1920s and has experienced many earthquakes, now the sopo still survive without any structural damage. The resistance of the sopo over the years proves the sopo resilience to
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Vladimir, Filatov, and Bolotnova Liubov. "Upper Kama potassium salt deposit tectonic scheme based on physical modeling results and geological and geophysical data." Izvestiya vysshikh uchebnykh zavedenii Gornyi zhurnal, no. 5 (August 6, 2020): 38–46. http://dx.doi.org/10.21440/0536-1028-2020-5-38-46.

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Introduction. The territory of the Upper Kama potassium salt deposit (UKPSD) which has been actively developed since 1932, is characterized by abnormal technogenic overload on the geological environment. This load destroys the natural balance of the geological environment, the restoration of which is accompanied by hazardous dynamic events, from rockbursts to induced earthquakes of various magnitudes. Dynamic conditions of UKPSD is determined by many factors, among which a significant role is played by tectonic factors. Tectonic structure in the form of tectonic features or criteria (or other
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Tu, Qingyi, Yuanping Cheng, Sheng Xue, Ting Ren, and Xiang Cheng. "Analysis of the Coal and Gas Outburst Mechanism from the Perspective of Tectonic Movement." Geofluids 2021 (July 1, 2021): 1–18. http://dx.doi.org/10.1155/2021/9988420.

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Coal and gas outburst is the extreme instability caused by stress, gas, and coal. In this review article, dominant factors and inducing factors of outburst were summarized; geologic features of typical outburst cases and the effects of tectonic movement on outbursts were analyzed; the outburst stages with considerations to geologic factors were divided. It was found that inducing factors, including buried depth, tectonic movement, gas composition, coal seam conditions, overlying/underlying rock conditions, and mining mode, control the outburst by influencing the dominant factors (stress, gas,
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Nguyen, Hoang Kim. "Gold metallogenic zoning and mineralized prospect in Dalat zone." Science and Technology Development Journal 16, no. 2 (2013): 85–96. http://dx.doi.org/10.32508/stdj.v16i2.1434.

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Dalat structural zone was had formed in tectonic setting of continental margin arc in late Mesozoic, have given structural and metallogenic zoning. In this Dalat structural zone, gold is one of the few endogenous minerals is significant mineralization in the study and search - exploration. Endogenic gold distribution in Dalat zone are controlled by main factors such as: structure – locally tectonics (structural fold, brittle fault, structure of dome top of granitoid intrusions, tectonic setting), intrusion (related to gold mineralization), stratigraphy-lithology (environmental containments: vo
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Wang, Chen. "Analysis of Controlling Factors of Fuyu Reservoir Accumulation in Zhaoyuan-Taipingchuan Area." Applied Mechanics and Materials 295-298 (February 2013): 2753–56. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.2753.

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In the past decade, no geological research has been done in Zhaoyuan-Taipingchuan area. The research and understanding on the area is still in 1990s and far away from meeting the needs of exploration. What has to be done now is to further analyze the accumulation factors from points-view of tectonic characteristics, tectonic division and tectonic controlling over sedimentation. Deeper understanding on fault-lithology and lithology hydrocarbon reservoir is especially important for favorable hydrocarbon zone evaluation and target zone selection. Taking these into account, accumulation factors ar
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Markejevaitė, Lada. "TRAINING OF TECTONIC SKILLS IN ARCHITECTURAL STUDIES/TEKTONIZAVIMO ĮGŪDŽIŲ UGDYMAS ARCHITEKTŪROS STUDIJOSE." JOURNAL OF ARCHITECTURE AND URBANISM 32, no. 1 (2008): 34–40. http://dx.doi.org/10.3846/13921630.2008.32.34-40.

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Tectonic expression of forms maintains the importance developed in architecture for a long time, but changing conditions force it to become more complex and integrate more factors. Tectonics creates preconditions for architecture as a sincretic art. So the tectonic nature of architecture becomes of great interest for the creative process. It becomes meaningful to introduce multiple and diverse problems of tectonics into architectural education. The creative work of a contemporary architect is stimulated by generation of distinctive architectural forms which are based on the nature of materials
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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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Majcin, Dušan, Dušan Bilčík, and Tomáš Klučiar. "Thermal state of the lithosphere in the Danube Basin and its relation to tectonics." Contributions to Geophysics and Geodesy 45, no. 3 (2015): 193–218. http://dx.doi.org/10.1515/congeo-2015-0020.

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Abstract The area of the Danube Basin is interesting in the light of the evaluation both of the lithosphere structure and of various theories of Carpathian-Pannonian region tectonic evolution. The aim of this paper is to analyse both the thermal conditions in the Danube Basin and the mutual relations to geological structure and tectonic development of the region under study. First the improved distributions of the terrestrial heat flow density and of the lithosphere thickness were constructed using recently gained geophysical and geological knowledge. Then the critical analysis of existing mod
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Yartsev, E. I., A. A. Burmistrov, and I. V. Vikentyev. "FACTORS OF LOCALIZATION AND PREDICTION OF MINERALIZATION IN DZHUSA MASSIVE SULFIDE DEPOSIT (SOUTH URALS)." Moscow University Bulletin. Series 4. Geology, no. 2 (April 28, 2018): 48–58. http://dx.doi.org/10.33623/0579-9406-2018-2-48-58.

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Analysis of tectonic displacements along fractures and faults enabled to reveal changes in character of tectonic deformations resulted from tectonic evolution of the Magnitogorsk island arc. Structural conditions of localization of ore mineralization of various types were investigated in the open pit of the Dzhusa deposit. The ore shoot on block diagram of the deposit coincides with intersection of NW-trending and sublongitudinal faults. Trends in distribution of enriched mineralization are slightly different for various metals. The data obtained enable to predict position of rich ore bodies a
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Kluykov, A. A. "Determination of vector Euler parameters." Geodesy and Cartography 932, no. 2 (2018): 2–9. http://dx.doi.org/10.22389/0016-7126-2018-932-2-2-9.

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Improving the accuracy of points coordinates determination from geodetic networks with the use of modern space geodesy techniques (GPS, SLR, VLBI, DORIS) identified factors that were earlier considered as insignificant. Such factors include the movement of tectonic plates. This made possible the transition from the static coordinate system model to the kinematic one. For the effect of the tectonic plates movement on the points coordinates you must know kinematic parameters of the tectonic plates movement – the Euler vector parameters – angular velocity of the tectonic plates rotation and the p
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Dissertations / Theses on the topic "Tectonic factors"

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Chhun, Eath. "Ordovician igneous rocks of the central Lachlan Fold Belt : geochemical signatures of ore-related magmas /." University of Sydney. Geosciences, 2004. http://hdl.handle.net/2123/610.

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The majority of economic gold deposits in NSW are associated with Ordovician-aged igneous rocks and are examples of the Cu-Au porphyry-skarn-epithermal association commonly developed in convergent margin to orogenic settings. They are among the oldest porphyry Cu-Au deposits in the Pacific Rim region. They are similar to younger deposits in terms of tectonic setting and structure, but the largest are chemically distinct, being associated with shoshonite magmas (Cadia, Ridgeway and Northparkes). The Lachlan Fold Belt (LFB) porphyries are subdivided into four sub-groups based mainly on their age
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Pica, Matthew J. "ASSEMBLY & JOINTURE: A Tectonics of Place & Structure in the Mississippi Heartland Delta." OpenSIUC, 2009. https://opensiuc.lib.siu.edu/theses/2.

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The structure can be considered the essence of an architectural solution. However, it is often a forgotten aspect of architecture that isn’t always expressed to its highest potential, commonly left hidden within or behind the façade or the interior finishes. The main question was how the two separate fields could be brought together conceptually to create a project that paired out the ideas to build greater conceptual depth and a possible totality of ideas thus forming an architectonic of knowledge. The design and hands-on building aspect of furniture design as well as that of structural bu
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Gómez, Esteban Galeano. "Characterization of genes involved in lignin biosynthesis in Tectona grandis." Universidade de São Paulo, 2015. http://www.teses.usp.br/teses/disponiveis/11/11151/tde-30042015-153939/.

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Teak tree (Tectona grandis L.f.) has a high value in the timber trade for fabrication of woody products due to its extraordinary qualities of color, density and durability. Despite the importance of this species, genetic and molecular studies available are limited. Also, the lack of molecular information about secondary xylem and tree maturation has hindered genetic exploration of teak. Therefore, gene expression studies and transcriptomic profiling are essential to explore wood formation and lignin biosynthesis through the development and aging of vascular plants. Aiming the gene expression s
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Drescher, Ronaldo. "Crescimento e produção de Tectona Grandis Linn F., em povoamentos jovens de duas regiões do estado de Mato Grosso - Brasil." Universidade Federal de Santa Maria, 2004. http://repositorio.ufsm.br/handle/1/3722.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior<br>The Tectona grandis Linn F. was introduced in Mato Grosso in the end of the sixties and new planting is made each year in the State with the aim of replacing native woods of noble use. Beyond the expectation of great future gains the teak plantations are, most of the time, made in the mosaic system. This system is certainly the greatest advantage of this wood species, which is conquering more space each year in the Mato Grosso economical set. For this project, information about teak was acquired from the cities of Santo Antonio do
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Hassoun, Virginie. "Analyse multi-échelles des déstabilisations sous-marines de la Marge Ligure : implications sur la répartition spatio-temporelle des facteurs déclenchant [sic]." Thesis, Nice, 2014. http://www.theses.fr/2014NICE4069.

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La marge Ligure est une marge passive soumise à une déformation tectonique compressive associée à la tectonique salifère messinienne. La reprise en compression de la marge s’accompagne d’une sismicité modérée récurrente ponctuée d’évènements plus forts. La marge Ligure est le siège d’une sédimentation importante au Plio-Quaternaire. Elle constitue un environnement propice à l’étude des déstabilisations gravitaires. L’objectif principal de ce travail était de décrire et caractériser les principaux mouvements en masse ayant affecté la marge continentale Ligure au cours du Plio-Quaternaire, de lo
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Wang, Li-Ping, and 王俐蘋. "The Tectonics of Learning Perspectives: Factory, Tribe, and Ocean." Thesis, 2018. http://ndltd.ncl.edu.tw/handle/uj2uk8.

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碩士<br>國立臺灣師範大學<br>教育學系<br>106<br>This study aims for describing learners’ learning perspectives. Factory, tribe and ocean are the metaphors which represent learners’ learning perspectives. Based on the experience of participant observation, the study starts from the concept of holistic life in order to understand learners’ learning perspectives. The concept of “Tectonics” illustrates the process how a human builds the connection with the world through the spatiotemporal approach. “Tectonics”can be considered as an echo of learning process because the concepts are concerned about not only indiv
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Drzewiecki, Peter Anthony. "Mid-cretaceous carbonate platform evolution, south-central Pyrenees, Spain interactions among eustasy, tectonics, environmental factors, and biological factors /." 1996. http://catalog.hathitrust.org/api/volumes/oclc/35745921.html.

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Books on the topic "Tectonic factors"

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Bogdanovic, Jelena. The Framing of Sacred Space. Oxford University Press, 2017. http://dx.doi.org/10.1093/acprof:oso/9780190465186.001.0001.

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The Framing of Sacred Space offers the first topical study of canopies as essential spatial and symbolic units in Byzantine-rite churches. Centrally planned columnar structures—typically comprising four columns and a roof—canopies had a critical role in the modular and additive processes of church design, from actual church furnishings in the shape of a canopy, to the church’s structural core defined by four columns and a dome. As architectonic objects of basic structural and design integrity, canopies integrate an archetypical image of architecture and provide means for an innovative understa
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Mitchell, Graham. How Giraffes Work. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197571194.001.0001.

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There are few creatures more beautiful, more aloof, and more fascinating than giraffes. Once they were plentiful and filled African landscapes, but in 2016 they were re-classified from “least concern” to “vulnerable” by the International Union for Conservation of Nature. Their survival in the wild is not assured. Much has been written about their private lives, about their behavior, social biology, and ecology, and their history in art and diplomacy. But so far no book has been written about their private lives, their physiology, and their anatomy and biochemistry—in short, the normal function
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Book chapters on the topic "Tectonic factors"

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Nash, C. R. "Factors Affecting the Acquisition of Structural Data from Remotely-Sensed Images of Eastern Australia." In Basement Tectonics 9. Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-2654-0_6.

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Lehmann, Bernd. "Petrochemical Factors Governing the Metallogeny of the Bolivian Tin Belt." In Tectonics of the Southern Central Andes. Springer Berlin Heidelberg, 1994. http://dx.doi.org/10.1007/978-3-642-77353-2_23.

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Scott, T. B. "Factors Affecting Limiting Angles for Fault Reactivation in Basement Rocks." In Proceedings of the International Conferences on Basement Tectonics. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5098-9_46.

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Basilevsky, A. T. "Factors Controlling Volcanism and Tectonism in Solar System Solid Bodies." In Comparative Planetology with an Earth Perspective. Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-017-1092-3_5.

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Leonov, M. G. "Plastic Deformation as a Factor of Material Transformation of Rocks (Southern Tien Shan)." In Proceedings of the International Conferences on Basement Tectonics. Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5098-9_31.

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Doglioni, Angelo, Annalisa Galeandro, Alessandro Guerricchio, and Vincenzo Simeone. "Tectonic Stress as Possible Co-predisposing Factor for Landslides Along the Central Adriatic Coast of Italy." In Engineering Geology for Society and Territory - Volume 2. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_42.

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Sequero, Cristina, Beatriz Bádenas, and Marcos Aurell. "Factors Controlling Oncoid Distribution in the Inner Areas of a Late Kimmeridgian Carbonate Ramp (Northeast Spain)." In Paleobiodiversity and Tectono-Sedimentary Records in the Mediterranean Tethys and Related Eastern Areas. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01452-0_41.

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Kassymkanova, Khaini-Kamal, Gulnara Jangulova, Gulnura Issanova, Venera Turekhanova, and Yermek Zhalgasbekov. "Geological Setting Structural-Tectonic Features and Physical—Mechanical Properties of Mountain Rocks on the Stability of Slopes with the Account of the Time Factor and Large-Scale Explosions." In Geomechanical Processes and Their Assessment in the Rock Massifs in Central Kazakhstan. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-33993-7_2.

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Cohen, Andrew S. "Facies Models at the Lake Basin Scale." In Paleolimnology. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195133530.003.0012.

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Understanding the historical evolution of sedimentation in a lake requires not only a grounding in facies interpretation but also an understanding of the larger-scale, lakewide linkages between deposition and those factors influencing sedimentation. The facies models we examined in chapter 7 can be linked to understand the differences in deposits between lake basins. Basin-scale facies models focus on the major interactions between climate or tectonic/ volcanic activity and sedimentation, attempting to explain why particular facies types develop in particular areas or at particular times in a lake’s history. Here I will focus on a few examples from the most intensively studied depositional settings, including lake types defined by mode of origin and evolution (rifts, glacial lakes, etc.) as well as saline lakes and playas, which share chemical and climatic attributes. Large-scale facies modeling in rift lakes has been driven by a need to understand the occurrence of hydrocarbons in ancient rifts (Lambiase, 1990; Katz, 2001). This in turn spurred a rapid accumulation of seismic reflection and facies data in the East African rift lakes and Lake Baikal (Russia) during the 1980s and 1990s, as well as attempts to synthesize these data and integrate them into general models. As we saw in chapter 2, the evolution of rift basins involves the development of asymmetric half-grabens and, in larger lake systems, the linkage of these half-grabens in a linear chain. As rift basins age, progressive deformation will eventually cause extensive deformation on both sides of the basin, transforming them into asymmetric full grabens, as seen in Lake Baikal today. This pattern of tectonic development has consequences for geomorphology, sediment delivery rates and locations, and sediment composition, that also vary depending on whether the lake basin is relatively full (high-stand conditions) or empty (low-stand) (Rosendahl et al., 1986; Cohen, 1990; Scholz and Rosendahl, 1990; Tiercelin et al., 1992; Soreghan and Cohen, 1996). Large-scale depositional patterns in a rift lake therefore represent an interplay between tectonic and climatic forces, factors that operate on somewhat different time scales.
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Araya-Vergara, José. "Ocean Coasts and Continental Shelves." In The Physical Geography of South America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195313413.003.0023.

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Suess (1900) provided the first scientific treatment of the South American coast from a tectonic perspective when he distinguished between the Atlantic and Pacific structural styles on opposite sides of the continent. Inman and Nordstrom (1971) later complemented this approach by relating these styles to the concepts of plate tectonics that had emerged during the 1960s. Useful keys to understanding South American coastal processes and sediment supplies were then offered by Davies (1977) and Potter (1994), respectively, while regional accounts of South American coastal landforms were made by specialists in books edited by Bird and Schwartz (1985) and Schwartz (2005). Clapperton (1993) reviewed Quaternary coastal morphogenesis. Coastal sites of scientific importance and historical coastline changes were discussed by Bird and Koike (1981) and Bird (1985). This chapter focuses on the principal factors involved in coastal evolution and morphogenesis, describes key regional landforms, and proposes a new analytical perspective for South America’s coasts by introducing a hierarchical system within coastal groups. The main coastline of South America is approximately 31,100 km long, of which 10,400 km face the Pacific Ocean, 16,700 the open Atlantic Ocean, and the remaining 4,000 km the more sheltered Caribbean Sea. Of the total length, approximately two-thirds lie within the tropics, ensuring that physical and ecological responses to ocean-atmosphere circulation systems involving the Intertropical Convergence Zone dominate these coasts. The remaining one third of the coast beyond the tropics is dominated during part or all of the year by temperate westerly conditions, which become increasingly cool and stormy toward the continent’s southern tip. The origins of the present coast reflect the tectonic forces that have affected the South American plate over the past 200 million years, augmented by relative sea-level changes associated with changing global (eustatic) ocean volume and regional (isostatic) crustal adjustments. The Atlantic coast of South America owes its broad outline to the separation of the continent from neighboring parts of Gondwana that began more than 200 Ma (million years ago). The Pacific and Caribbean coasts have a more complex history, related to the progressive interaction of the westwardmoving South American plate with four oceanic plates with which it has come into contact).
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Conference papers on the topic "Tectonic factors"

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Mikhaylov, Sergey Petrovich, and Anastasia Andreevna Shtyrlyaeva. "Consideration of the Influence of Carbonate Cement on the Accuracy of Prediction of Well Start-Up Flow Rates in Deep Reservoirs of the West Siberian Oil and Gas Basin on the Example of Reservoir U1 Formation." In SPE Symposium: Petrophysics XXI. Core, Well Logging, and Well Testing. SPE, 2021. http://dx.doi.org/10.2118/208422-ms.

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Abstract Oil reservoirs are often affected by tectonic processes throughout their lifetime. Tectonic processes contribute to the impact on the formation of a number of mechanical and chemical factors. These factors change the composition and structure of the reservoir and this affects the reservoir properties of the reservoir. Deep-seated reservoirs experience a longer and more intense impact of tectonic processes. A more detailed study of the composition and properties of reservoirs for an accurate forecast of reservoir properties and their productivity potential is due to this. Standard log
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Bertello, F., A. Fattorini, and C. Visentin. "Tectonic and Sedimentary Factors Controlling the Petroleum System of the Murzuk Basin, Libya." In 1st EAGE North African/Mediterranean Petroleum & Geosciences Conference & Exhibition. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.8.s037.

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Liping, Xiong, Liu Yanli, and Shi Danni. "Research on the Tectonic Evolution of the North Africa from Morocco to Libya as the Controlling Factor on the petroleum basins’ Hydrocarbon Accumulation." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2566974-ms.

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ABSTRACT This paper focuses on the tectonic evolution of the North African petroleum basins as the controlling factors on the major basins’ formation, evolution and the hydrocarbon accumulation, analyzing the petroleum enrichment conditions and proposing hydrocarbon accumulation mode. The analysis concludes that the distribution of North Africa Basins is in regular east-west direction, clear depression associates with highland structure. The basins becomes gradually older from the west to the east, corresponding to the Western Paleozoic basin, the Middle part Paleozoic and Mesozoic superimpose
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Melinte-Dobrinescu, Mihaela. "FACTORS CONTROLLING THE OCCURRENCE OF THE GOSAU-TYPE BASINS IN THE SOUTHERN CARPATHIANS: TECTONIC VERSUS SEA-LEVEL FLUCTUATION." In 16th International Multidisciplinary Scientific GeoConference SGEM2016. Stef92 Technology, 2016. http://dx.doi.org/10.5593/sgem2016/b11/s01.024.

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Schuller, Volker, Andras Zamolyi, Eirik Stueland, István Dunkl, Michael Kettermann, and Zsolt Schleder. "Fault Rock Property Prediction On Jurassic Clastics Of The Barents Sea/Norway." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/206290-ms.

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Abstract We analysed the fault rocks of a compartmentalized field in the Barents Sea, in an area with several tectonic elements, which formed at different tectonic events. Standard Fault Seal Analysis (FSA) was conducted to predict the shale content of the fault rock (SGR). A static cellular model based on well data, seismic data and geological concepts served as input. The fault rock calibration workflow required various data acquired by different methods. We analysed the Mid-Triassic to Upper Jurassic clastic deposits to reconstruct the tectonic history. Apatite fission track and (U-Th)/He t
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Mukanov, Adil, Chenkai Zhang, Almat Sagynbayev, Amir Kuvanyshev, Dana Shaikhina, and Yernur Akashev. "Characterization of Key Quality Factors of Highly Argillaceous and Naturally Fractured Paleozoic Carbonate Deposits with Complex Tectonic Setting South Turgai Basin, Kazakhstan." In SPE Annual Caspian Technical Conference and Exhibition. Society of Petroleum Engineers, 2018. http://dx.doi.org/10.2118/192584-ms.

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Mukanov, Adil, Chenkai Zhang, Almat Sagynbayev, Amir Kuvanyshev, Dana Shaikhina, and Yernur Akashev. "Characterization of Key Quality Factors of Highly Argillaceous and Naturally Fractured Paleozoic Carbonate Deposits with Complex Tectonic Setting South Turgai Basin, Kazakhstan (Russian)." In SPE Annual Caspian Technical Conference and Exhibition. Society of Petroleum Engineers, 2018. http://dx.doi.org/10.2118/192584-ru.

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Khanbikova, Regina, Venera Bazarevskaya, Oleg Sotnikov, and Albert Bachkov. "Oil Saturation Index in Hydrophobic Carbonate Reservoir: Evaluation Aspects." In SPE Symposium: Petrophysics XXI. Core, Well Logging, and Well Testing. SPE, 2021. http://dx.doi.org/10.2118/208416-ms.

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Abstract Hydrocarbon reserves in carbonate reservoirs account for 38% - 60% of total world reserves, according to different estimates. In Tatarstan, carbonate reservoirs are found, mostly, in the eastern slope of the Melekess Depression and the South-Tatarian Arch. The carbonate reservoirs are confined to the Middle and Lower Carboniferous sediments, the Upper Devonian (including the domanik sediments), and the Upper Permian (the Kazanian heavy oil accumulations). Considering an extensive geographic and stratigraphic range and differing tectonic and sedimentation environments, the carbonate ro
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Есина, Л., L. Esina, А. Хворощ, et al. "THE ROLE OF THE SUBMARINE LANDSLIDE PROCESSES IN EVOLUTION OF THE BLACK SEA CONTINENTAL SLOPE AND SHELF. THE INFLUENCE OF LANDSLIDES ON MODERN COASTAL PROCESSES." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3a0b6c337.05323429.

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Abstract:
Detailed studies of landslide formation on the continental slope of Near Caucasus part of Black Sea, we have made in the area between the Pshada– Olginka settlements allowed to explore the distribution of landslide formations on the continental slope and to establish their influence on the retreat of the shelf edge. The intensive destruction of shelf edge leads to a reduction in its width, the intense movement of sediments from the shelf and transporting them to the continental slope and deep-sea part in large quantities. The evolution and distribution of landslides are influenced by the geolo
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10

Salguero, Gualberto Chiriboga. "Geotechnical Management in OCP Pipeline." In 2012 9th International Pipeline Conference. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/ipc2012-90154.

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Abstract:
Landslides are one of the main threats in maintaining pipeline integrity and depend directly on natural geological and geotechnical conditions. External factors such as weather, rainfall, and others, can trigger land movements and displace the pipeline. The Ecuadorian OCP (Heavy Crude Oil Pipeline) is a buried pipeline going in an East to West direction, crossing 485 kilometers of the Ecuadorian territory. It starts in the Amazon Region (approximately 300 meters above sea level), and then climbs the Andes Mountains (4060 meters above sea level in its tallest portion), to then descend to the sh
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