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1

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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2

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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3

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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4

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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5

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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7

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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8

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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9

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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10

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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11

WANG, Youzhi, and Shihui WANG. "Porosity Characteristics of Tectonic Coal and Its Controlling Factors." Acta Geologica Sinica - English Edition 89, s1 (2015): 460–62. http://dx.doi.org/10.1111/1755-6724.12307_23.

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12

Gong, Lei, Shu Jun Guo, Shuai Gao, Xian Xian Tao, and Jian Guo Huang. "Distribution Characteristics of Fractures in the Ultra-Low Permeability Reservoirs of Anpeng Oilfield, China." Advanced Materials Research 909 (March 2014): 463–66. http://dx.doi.org/10.4028/www.scientific.net/amr.909.463.

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Using the data of cores, outcrops, thin sections and image logs, we analyzed the fracture distribution characteristics in the ultra-low permeability reservoirs of Anpeng oilfield. Then, we analyzed the main factors controlling the development of fractures. There are tectonic fractures and diagenetic fractures in the ultra-low permeability reservoirs. Tectonic fractures with high dip-angle are the main fracture type. Under the stresses resulting from horizontal tectonic compressions in the Early and Late Himalayan movements, three sets of tectonic fractures formed in the study area, i.e. E-W, N
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Ang, Marcus, Jodhbir S. Mehta, Chelvin C. A. Sng, Hla Myint Htoon, and Donald T. H. Tan. "Indications, Outcomes, and Risk Factors for Failure in Tectonic Keratoplasty." Ophthalmology 119, no. 7 (2012): 1311–19. http://dx.doi.org/10.1016/j.ophtha.2012.01.021.

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14

YUAN, Yu-Song, Shu-Chun YANG, Sheng-Biao HU, and Li-Juan HE. "Tectonic Subsidence of Qiongdongnan Basin and Its Main Control Factors." Chinese Journal of Geophysics 51, no. 2 (2008): 248–55. http://dx.doi.org/10.1002/cjg2.1216.

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15

Alekseev, Viktor. "Tectonic and magmatic factors of Li-F granites localization of the East of Russia." Journal of Mining Institute 248 (May 25, 2021): 173–79. http://dx.doi.org/10.31897/pmi.2021.2.1.

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We have investigated tectonic and magmatic factors of Li-F granites localization of the East of Russia. The study is based on the ideas of Far Eastern geologists about the deep structures of intraplate activity. A model of a source structure with mantle heat sources and ore-forming magmatic complexes was used. We carried out a special metallogenic analysis of the East of Russia as applied to the rare metal-tin-bearing formation of subalkaline leucogranites, including Li-F ones.
 Source structures are the main factor in the tectonic and magmatic development of the East of Russia, localizat
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16

Hu, Yang, Zhi Ping Wu, and Guang Zeng Wang. "Hydrocarbon Accumulation Dominant Factors and Modes of Minghuazhen Formation in Chengdao Area." Applied Mechanics and Materials 628 (September 2014): 372–75. http://dx.doi.org/10.4028/www.scientific.net/amm.628.372.

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Chengdao area is a multiple hydrocarbon accumulation belt with the typical tectonic background, and its main target stratum is Neogene. However, the exploration and recognition level of Minghuazhen Formation is still at the primary stage. Based on the comprehensive analysis of seismic, well-logging, logging and geochemical data, and combined with its structural characteristics, intensity of fault activity and reservoir-caprock assemblage, this paper systematically analyzed the dominant factors of hydrocarbon accumulation in Minghuazhen Formation, and clarified that the tectonic setting control
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17

Lemenkova, Polina. "STATISTICAL ANALYSIS OF THE MARIANA TRENCH GEOMORPHOLOGY USING R PROGRAMMING LANGUAGE." Geodesy and cartography 45, no. 2 (2019): 57–84. http://dx.doi.org/10.3846/gac.2019.3785.

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This paper introduces an application of R programming language for geostatistical data processing with a case study of the Mariana Trench, Pacific Ocean. The formation of the Mariana Trench, the deepest among all hadal oceanic depth trenches, is caused by complex and diverse geomorphic factors affecting its development. Mariana Trench crosses four tectonic plates: Mariana, Caroline, Pacific and Philippine. The impact of the geographic location and geological factors on its geomorphology has been studied by methods of statistical analysis and data visualization using R libraries. The methodolog
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18

Wang, Guang Zeng, Zhi Ping Wu, Chao Liu, and Yang Hu. "Fault Activity’s Controlling Effect on Source Rock an Example from Bohai Sea Area." Applied Mechanics and Materials 628 (September 2014): 366–71. http://dx.doi.org/10.4028/www.scientific.net/amm.628.366.

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Based on the fault activity, geochemical data and predecessor research results on tectonic subsidence and source rock of Bohai Sea Area, this paper took Bohai Sea Area as an example to compare its structural activity factors with its source rock indexes, and then to explore fault activity’s controlling effect on source rock. And the results shows: source rock thickness is mainly controlled by fault throw of boundary fault, but it is also be influenced by others factors in different stages; Fault activity rate, climatic conditions etc. factors are all key factors influencing organic matter perc
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19

Guo, Yu, Jing Zhou Zhao, and Qian Wang. "The Influence of Tectonic Characteristics on the Accumulation of CBM in H Area." Advanced Materials Research 868 (December 2013): 56–61. http://dx.doi.org/10.4028/www.scientific.net/amr.868.56.

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There are several geological factors affecting the accumulation of CBM, including tectonic condition, burial depth, coal thickness, coal rank, gas content, permeability, reservoir pressure, desorption pressure and hydrological condition, etc. This article analyzes the influence of tectonic characteristics on the accumulation of CBM in H area, combining the tectonic characteristics and the actual production data, finally conclusions can be drawn that the uplifting movement of crust after coal-forming period could break the original adsorption equilibrium, then CBM would escape under unfavorable
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20

Pankov, I. L. "THEORETICAL ESTIMATION OF IN-SITU STRESSED STATE OF ROCK MASSIFES UNDER CONDITIONS OF." News of the Tula state university. Sciences of Earth 4, no. 1 (2019): 292–304. http://dx.doi.org/10.46689/2218-5194-2019-4-1-292-304.

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System of physical equations was obtained, which determines the relationship between main stresses and corresponding strains for the conditions of the all-round compression tectonic stress field in a virgin compacted intact massif of rocks. Estimated formulas for determining the maximum and minimum horizontal stresses of an intact massif, which is under conditions of plane-directional tectonic influence depending on the factors of vertical pressure, porosity and deformation modulus of rocks, are obtained. The behavior of the horizontal stress distribution from the vertical pressure is consider
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21

Filatov, Vladimir V., and Liubov A. Bolotnova. "On the seismic activity of the Upper Kama potassium salt deposit." Izvestiya vysshikh uchebnykh zavedenii Gornyi zhurnal, no. 1 (February 17, 2020): 60–67. http://dx.doi.org/10.21440/0536-1028-2020-1-60-67.

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Introduction. The exploitation of the earth's subsoil on an industrial scale leads to a disturbance of equilibrium state of the geological environment and, as a consequence, to the manifestation of various dynamic events in it: sinkholes, rockbursts, induced earthquakes of various magnitudes, etc. Therefore, the problem of predicting such events or phenomena becomes urgent. About two dozen factors determining the state of geological environment and its dynamic regime have been identified in the course of solving this problem for the territory of Upper Kama (Verkhnekamskoe) potassium salt depos
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22

Hnidets, V. P., K. H. Hryhorchuk та L. V. Balandyuk. "PECULIARITIES OF FORMATION OF THE LOWER CRETACEOUS TEСTONO-SEDIMENTATION SYSTEM OF THE BLACK SEA MEGADEPRESSION". Geological Journal, № 2 (15 липня 2021): 67–78. http://dx.doi.org/10.30836/igs.1025-6814.2021.2.224399.

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Based on the analysis of the distribution of structural-material complexes, facial-genetic types and modeling of the history of immersion of the Lower Cretaceous sediments, the spatial-temporal differentiation of the tectonic regime of the Black Sea megadepression in the Early Cretaceous was established. It is shown that the structural and lithologicalfacial features of the Lower Cretaceous tectonic-sedimentation system were determined by the interaction of tectonic and geological-paleooceanographic factors. Thus, the low sea level and the initial phases of activation of sublatitudinal faults
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Repina, K. V. "Natural factors forming the quality of carbonate raw materials." Journal of Geology, Geography and Geoecology 27, no. 3 (2019): 495–503. http://dx.doi.org/10.15421/111873.

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The article is devoted to the study of natural factors that influence the regularities in the distribution of the quality of carbonate raw materials in the deposits of the Articulation Zone of the Donbass Basin with the Priazovskiy block of the Ukrainian Shield. Paleogeographic conditions of sedimentation and the processes of secondary quality change were established by comparing the lithologic-stratigraphic sections of deposits in different parts of the Articulation Zone: from the west (Novotroitskoe deposit) through the center (Elenovskoe deposit) and to the east (Karakubskoe deposit). The v
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Makarova, N. V., A. S. Gusel’tsev, T. V. Sukhanova, and V. M. Makeev. "Geological conditions of suffosion processes development and their acitivity at Sal-Don neotectonic upland (Rostov NPP area)." Геоэкология. Инженерная геология. Гидрогеология. Геокриология, no. 6 (December 21, 2019): 19–29. http://dx.doi.org/10.31857/s0869-78092019619-29.

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Suffusion processes and their influence on the stability of the Rostov NPP site are investigated. Geological, tectonic, geomorphological, hydrogeological conditions, as well as anthropogenic factors affect the development and intensification of suffusion. These conditions and factors include the following: predominance of Pliocene and Quaternary sands in the geological cross-section; the presence of clay aquiclude underlying sandy deposits; natural seasonal and human-induced fluctuations of the water level in the Tsimlyansk reservoir; as well as pumping of groundwater. The buried relief in the
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Chotchaev, Khyisa, Vladislav Zaalishvili, and Boris Dzeranov. "Natural endogenous factors of geoecological transformation of the mountain part of North Ossetia." E3S Web of Conferences 164 (2020): 07025. http://dx.doi.org/10.1051/e3sconf/202016407025.

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Geoecological transformation of the biocenosis habitat is an evolutionary process, predetermined by the interaction of the lithosphere with the hydrosphere, atmosphere and the solar system as a whole, under the condition of anthropogenic impact absence. Geoecological transformation occurs under the influence of many natural factors of an endogenous and exogenous nature, the effects of which in the mountainous areas are especially intensive and damageable, due to the sharp and intense exposure forms of exogenous factors of the erosive destruction, the presence of a large gravitational potential
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Weihaupt, John G., Frans G. Van Der Hoeven, Claude Lorius, and Frederick B. Chambers. "Origin(s) of Antarctica's Wilkes Subglacial Basin." Antarctic Science 26, no. 4 (2013): 377–83. http://dx.doi.org/10.1017/s0954102013000746.

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AbstractThe Wilkes Subglacial Basin (WSB), the largest subglacial basin in East Antarctica, is a topographic depression of continental proportions that lies beneath the East Antarctic continental ice sheet. Discovered by the US Victoria Land Traverse 1959–60, the origin of the WSB and the influence of palaeoclimate on its overlying continental ice sheet have remained uncertain since the time of its discovery. Most explanations of origin favour lithospheric structural control as a function of tectonic activity. Lithospheric flexure due to thermally or isostatically induced uplift of the Transan
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Liu, Jianhao, Caijin Xie, and Junying Rao. "Calculation Model and Influencing Factors of Surrounding Rock Loosening Pressure for Tunnel in Fold Zone." Advances in Civil Engineering 2021 (February 6, 2021): 1–15. http://dx.doi.org/10.1155/2021/6678511.

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This research aims to study the surrounding rock loosening pressure variation law of tunnel in the fold area. Based on the calculation method of surrounding rock loosening pressure for shallow tunnel, a new calculation model of the surrounding rock pressure was proposed for tunnel in the fold area; through this calculation model, the effects of tectonic stress (F), the angle ( φ 1 ) between tectonic stress and horizontal plane, tunnel buried depth (h), friction angle ( θ ), the multiple (k) between tectonic stress and rock mass gravity in the upper part of the tunnel, lateral pressure coeffici
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Sobolev, S. V., and A. Y. Babeyko. "What drives orogeny in the Andes?" Geology 33, no. 8 (2005): 617–20. http://dx.doi.org/10.1130/g21557ar.1.

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Abstract The Andes, the world's second highest orogenic belt, were generated by the Cenozoic tectonic shortening of the South American plate margin overriding the subducting Nazca plate. We use a coupled thermomechanical numerical modeling technique to identify factors controlling the intensity of the tectonic shortening. From the modeling, we infer that the most important factor was accelerated westward drift of the South American plate; changes in the subduction rate were less important. Other important factors are crustal structure of the overriding plate and shear coupling at the plates' i
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Fan, Zhen Feng, Jin Liang Zhang, Xiao Lin Liu, and Jin Kai Wang. "Structural Style in Gentle Slope and its Control Action for Sedimentary and Reservoir Formation of Chenjiazhuang Area in Jiyang Depression for Case." Advanced Materials Research 187 (February 2011): 84–91. http://dx.doi.org/10.4028/www.scientific.net/amr.187.84.

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Haft-graben fault basin often have large-scale gentle slope, and the zone of structural style, sedimentary types and forming factor has its unique characteristics. This paper takes Chenjiazhuang area in Jiyang depression for example. By constructing, deposition and accumulation of combining methods Chenjiazhuang area can be divided into three major tectonic units, witch are upliftt zone, slope zone and structural slope-break zone. Different tectonic units develop different sedimentary and reservoir types, and the accumulation controlling factors are also larger differences.
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Tran, Duc-Huy, and Shih-Jung Wang. "Land subsidence due to groundwater extraction and tectonic activity in Pingtung Plain, Taiwan." Proceedings of the International Association of Hydrological Sciences 382 (April 22, 2020): 361–65. http://dx.doi.org/10.5194/piahs-382-361-2020.

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Abstract. Pingtung coastal plain, located at the active convergent boundary between Philippine Sea Plate and Eurasian Plate, is one of the most active areas regarding tectonic deformation in Taiwan. Groundwater over-pumping for aquaculture along the coast area of Pingtung plain induced a serious land subsidence problem for decades. How much land subsidence contributed by tectonic activity and groundwater pumping is a crucial issue for tectonic study and groundwater management in this area. This study collected the data in different fields and proposed a conceptual model to calculate the quanti
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Nevstruyev, Viktor, and Olga Kozlova. "Geodynamic and structural factors of porphyritic objects localization in Sikhote-Alin." E3S Web of Conferences 56 (2018): 04020. http://dx.doi.org/10.1051/e3sconf/20185604020.

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Ore bearing porphyritic systems of Sikhote-Alin form linear zones in Cretaceous volcanic belt. They are limited to zones of tectonic disturbances at Moho depths of 19-25 mi (30-40 km). Pacific slab lies at around 340 miles (548 km) below the volcanic belt, which matches the slab depth of porphyritic deposits formation belts in the Andes and Indonesia-Tonga region. Formation of porphyry copper systems is linked to the processes of metalliferous fluids intrusion at slab destruction areas near asthenosphere.
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Dalatkazin, T. S., Y. P. Konovalova, V. I. Ruchkin, and P. I. Zuev. "RESEARCH FOR MODERNIZA TION OF RADON EMANA TIONAS THE EXPRESS METHOD AT GEODYNAMIC DIAGNOSTICS." News of the Tula state university. Sciences of Earth 4, no. 1 (2019): 206–20. http://dx.doi.org/10.46689/2218-5194-2019-4-1-206-220.

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Research for application of radon emanation measurementsat geodynamic diagnostics of the rock massif arepresented. The geodynamic activity participates in formation of radon emanations. For elimination of not tectonic factors on formation of radon emanation the rationing of radon volume activity in soil air is used. The received changes of radon volume activity are confirmed by geodetic survey. The rationing of radon volume activity in soil air allows to use radon measurements for ranging of the revealed abnormal deformation sites - tectonic spheres- onge-odynamic activity degree.
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Gong, Lei, Shuai Gao, Xiaofei Fu, Shumin Chen, Bingyang Lyu, and Jiaqi Yao. "Fracture characteristics and their effects on hydrocarbon migration and accumulation in tight volcanic reservoirs: A case study of the Xujiaweizi fault depression, Songliao Basin, China." Interpretation 5, no. 4 (2017): SP57—SP70. http://dx.doi.org/10.1190/int-2016-0227.1.

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The Xujiaweizi fault depression is located in the northern part of the Songliao Basin, China. The Yingcheng Formation of the Xujiaweizi fault depression is a fractured tight volcanic reservoir. Many primary pores exist in the tight volcanic reservoirs of the Yingcheng Formation, but their connectivity is very poor. The degree of development of tectonic fractures determines the reservoir quality and the probability of hydrocarbon accumulation. To elucidate the fracture characteristics and their effects on hydrocarbon migration and accumulation, we analyze the fracture genetic types, characteris
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Stamenković, Vlada, and Doris Breuer. "The tectonic mode of rocky planets: Part 1 – Driving factors, models & parameters." Icarus 234 (May 2014): 174–93. http://dx.doi.org/10.1016/j.icarus.2014.01.042.

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Kuznetsov, V. G., and L. M. Zhuravleva. "Lithological, Biological, and Tectonic Factors Determining the Structure of Oil-and-Gas Reservoirs." Lithology and Mineral Resources 56, no. 4 (2021): 343–55. http://dx.doi.org/10.1134/s0024490221040040.

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36

Bai, Ying, Hong Liang Wang, Qian Ru Li, and Peng Wu. "Cenozoic Tectonic Evolution and Controlling Factor on Hydrocarbon Accumulation in the Southern East China Sea Shelf Basin." Applied Mechanics and Materials 416-417 (September 2013): 1908–13. http://dx.doi.org/10.4028/www.scientific.net/amm.416-417.1908.

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The East China Sea shelf basin, which is a fault subsidence during the Cenozoic Era, locates in the East China Sea continental shelf. In this paper, balanced section technique has been applied to analyzing the differential evolution in the East China Sea shelf basin south of Cenozoic tectonic and summarizing the control factors of tectonic activities on the petroleum accumulation. Our study results will provide essential data and basis for the distribution of the Cenozoic oil and gas and promote the development of the petroleum exploration in the East China Sea shelf basin.
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ΒΟΥΒΑΛΙΔΗΣ, Κ., Α. ΣΦΕΙΚΟΣ, Θ. ΠΑΡΑΣΧΟΥ, Χ. ΚΕΧΑΓΙΑ та Δ. ΨΩΜΙΑΔΗΣ. "Η επίδραση της γεωλογίας και της τεκτονικής στην εξέλιξη του υδρογραφικού δικτύου και της υδρολογικής λεκάνης του ποταμού Πάμισου της Θεσσαλίας." Bulletin of the Geological Society of Greece 38 (10 вересня 2005): 86. http://dx.doi.org/10.12681/bgsg.18428.

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River Pamisos is a main tributary of Pinios River, draining the SW part of the Thessaly catchment area. The river's drainage basin comprises part of the plain as well as of the mountainous terrain that bounds the broader Thessaly Plain. In this paper we present the results of both qualitative and quantitative analyses of the drainage network and morphology through processing of digitized data with GIS software. Quantitative measurements allowed objectively to compare different landforms and to calculate less straightforward parameters (geomorphic indices) that may be useful for the identifying
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38

Balázs, Attila, Liviu Matenco, and Didier Granjeon. "Thermo-mechanical and stratigraphic numerical forward modelling: recent advances and their joint application in the Pannonian Basin." Földtani Közlöny 149, no. 3 (2019): 183. http://dx.doi.org/10.23928/foldt.kozl.2019.149.3.183.

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Basin analysis and subsidence history provide key insights into sedimentary basin forming mechanisms. Direct observations have long been the only source of information on their thermal and lithological architecture. State of the art modelling techniques today enable the prediction and computation of their formation and evolution constrained by geological field observations, geophysical and deep borehole data. Understanding the inherent connections between large-scale tectonic and local basin-scale surface processes requires the joint application of thermo-mechanical and stratigraphic modelling
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39

Fan, Chunyan, Xianglu Tang, Yuanyin Zhang, et al. "Characteristics and origin of the pore structure of the lacustrine tight oil reservoir in the northwestern Jiuquan Basin, China." Interpretation 7, no. 3 (2019): T625—T636. http://dx.doi.org/10.1190/int-2018-0108.1.

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The pore structure controls the formation processes of tight oil reservoirs. It is meaningful to study the characteristics and origin of the pore structure of the tight oil reservoir. We have analyzed the pore structure of the tight oil reservoir by thin sections, scanning electron microscopy, and mercury intrusion porosimetry. We analyze the origin of the pore structure based on sedimentological, diagenetic, and tectonism processes. The porosity of the tight oil reservoirs is mainly approximately 2%–10%, and the permeability is mainly from 0.01 to 0.3 mD. The pores of the lacustrine tight oil
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40

Bruno, Luigi, Bruno Campo, Bianca Costagli, et al. "Factors controlling natural subsidence in the Po Plain." Proceedings of the International Association of Hydrological Sciences 382 (April 22, 2020): 285–90. http://dx.doi.org/10.5194/piahs-382-285-2020.

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Abstract. Understanding the causes and mechanisms of land subsidence is crucial, especially in densely populated coastal plains. In this work, we calculated subsidence rates (SR) in the Po coastal plain, averaged over the last 5.6 and 120 kyr, providing information about land movements on intermediate (103–105 years) time scales. The calculation of SR relied upon core-based correlation of two lagoon horizons over tens of km. Subsidence in the last 120 kyr appears to be controlled mainly by the location of buried tectonic structures, which in turn controlled sedimentation rates and location of
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41

Liu, Guoping, Lianbo Zeng, Chunyuan Han, et al. "Natural Fractures in Carbonate Basement Reservoirs of the Jizhong Sub-Basin, Bohai Bay Basin, China: Key Aspects Favoring Oil Production." Energies 13, no. 18 (2020): 4635. http://dx.doi.org/10.3390/en13184635.

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Analysis of natural fractures is essential for understanding the heterogeneity of basement reservoirs with carbonate rocks since natural fractures significantly control key attributes such as porosity and permeability. Based on the observations and analyses of outcrops, cores, borehole image logs, and thin sections from the Mesoproterozoic to Lower Paleozoic in the Jizhong Sub-Basin, natural fractures are found to be abundant in genetic types (tectonic, pressure-solution, and dissolution) in these reservoirs. Tectonic fractures are dominant in such reservoirs, and lithology, mechanical stratig
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42

Паламарчук (Palamarchuk), Ирина (Irina) Анатольевна (Anatol'yevna), Ольга (Ol'ga) Степановна (Stepanovna) Бровко (Brovko), Владимир (Vladimir) Васильевич (Vasil'yevich) Беляев (Belyaev), et al. "INFLUENCE OF THE ENVIRONMENTAL GEOECOLOGICAL FACTORS ON THE BIOCHEMICAL INDICATORS OF LICHENS IN THE TERRITORY OF THE VELSK-USTYANSK TECTONIC NODE (ARKHANGELSK REGION)." chemistry of plant raw material, no. 4 (December 11, 2018): 215–24. http://dx.doi.org/10.14258/jcprm.2018043803.

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The influence of geoecological factors formed in Velsk-Ustyansk tectonic node of the Arkhangelsk region on the state of lichenobiotics was studied. Two of the most common species of bushy lichens are selected as the test systems. The objects of research are two species of bushy lichens, which were used as a test system. From the soil lichens, the species Cladonia stellaris was studied. From the epiphytic lichens, the species Usnea subfloridana was studied. The material was collected in the vegetation period (spring-autumn) from the three test plots (in the center, at the periphery and outside
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43

Surikova, Ekaterina. "GEOLOGY AND PETROLEUM POTENTIAL OF NOVY PORT FIELD ON THE RESULTS OF THE INTERPRETATION OF 2D SEISMIC AND DEEP DRILLING." Interexpo GEO-Siberia 2, no. 1 (2019): 206–16. http://dx.doi.org/10.33764/2618-981x-2019-2-1-206-216.

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The objective of this study was to build a set of structural and isopach maps of seismic sequences, seismic-geological sections, paleo-sections and correlation schemes; structural-tectonic and paleotectonic analysis of Novy Port shaft; to study the influence of tectonic processes and lithological factors on the oil and gas content of Jurassic and Cretaceous sedimentary sequences. It was concluded that the formation of the structural trap of Novy Port field began in Berrias-Aptian, the most intensive growth of the structure occurs in the post-Turonian time due to the upward movement of the base
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REZAEE, M. R., N. M. LEMON, and R. J. SEGGIE. "Tectonic fingerprints in siderite cement, Tirrawarra Sandstone, southern Cooper Basin, Australia." Geological Magazine 134, no. 1 (1997): 99–112. http://dx.doi.org/10.1017/s0016756897006407.

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Compositional zoning and dissolution in cement is a direct response to the fluctuation of pore water chemistry, the variation of which during burial can be controlled by many factors, including the interaction between pore water and rock-forming minerals and the mixing of fluids from different origins. This paper suggests that tectonic activity can, by altering the hydraulic gradient, also influence pore water chemistry and lead to dissolution of cement, made clear by zoning within siderite crystals. Three different stages of siderite cement have been described from the Tirrawarra Sandstone in
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45

Koral, H., J. Kronfeld, N. Avsar, V. Yanko, and J. C. Vogel. "Major Recent Tectonic Uplift in Iskenderun Bay, Turkey." Radiocarbon 43, no. 2B (2001): 957–63. http://dx.doi.org/10.1017/s003382220004162x.

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Radiocarbon dating was carried out in the sediment profiles of four marine sediment cores taken from Iskenderun Bay, Turkey. The bay is quite shallow in the present day, and a previous tectonic study had considered that the bay floor might have been subsiding. However, this cannot be so, for the 14C ages would thereby lead to the apparent paradox of normal marine sedimentation having taken place during times when glacio-eustatic sea level lowering would have exposed the bay floor. Rather, we conclude that the floor of Iskenderun Bay on the whole has been experiencing rapid uplift since the end
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46

Heidebrecht, A. C., and N. Naumoski. "Evaluation of site-specific seismic design requirements for three Canadian cities." Canadian Journal of Civil Engineering 15, no. 3 (1988): 409–23. http://dx.doi.org/10.1139/l88-056.

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Siesmic design requirements as specified in building codes normally use a generic approach in which the seismic response is independent of the site location, except for a single intensity-related parameter used to define the severity of the expected ground motion. In reality, the characteristics of earthquakes that influence structural response depend on both the level of seismic motion and the seismo-tectonic environment at the specific location. This paper describes a methodology for determining seismic design requirements that uses both magnitude (M) and epicentral distance (R) to define th
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Shang, Fu-Hua, Yan-Ming Zhu, Hai-Tao Gao, Yang Wang, Rui-Yin Liu, and Xian-Wei Meng. "Analysis of Developmental Characteristics and Dominant Factors of Pore-Fracture Systems in Lower Cambrian Marine Shale Reservoirs: A Case Study of the Niutitang Formation, Fenggang Block, Southern China." Journal of Nanoscience and Nanotechnology 21, no. 1 (2021): 57–71. http://dx.doi.org/10.1166/jnn.2021.18461.

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Due to breakthroughs in the Lower Silurian Longmaxi Formation in the Sichuan Basin and multiple strata around the basin, the northern part of Guizhou adjacent to the Sichuan Basin has become a key area for shale gas exploration. Compared with the Longmaxi Formation, the Niutitang Formation displays greater TOC (total organic carbon) content, depositional thickness and distribution area, but the details remain undetermined. In the study area, the Lower Cambrian Niutitang Formation typically has high TOC content, maturity and brittle mineral content. The study area has experienced multiple perio
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48

Cui, Y. J., Y. Li, X. Y. Si, et al. "Tectonic Controls on Near-Surface Variations in CH4 and CO2 Concentrations along the Northwestern Margin of the Ordos Block, China." Geofluids 2019 (August 5, 2019): 1–10. http://dx.doi.org/10.1155/2019/7909483.

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Tectonic controls on near-surface CH4 and CO2 concentrations were investigated by measuring CH4 and CO2 concentrations at the surface and a height of 1.5 m, in the different tectonic units that comprise the northwestern margin of Ordos Block, China, which has a complex tectonic structure and a history of strong earthquakes. CH4 and CO2 concentrations varied from 1905 to 2472 ppb and 397.5 to 458.5 ppm, respectively. Surface CH4 and CO2 concentrations were generally higher than those measured at 1.5 m, but showed similar trends, indicating that the measured CH4 and CO2 predominantly originated
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Wu, Shiguo, Xinyuan Zhang, Zhen Yang, Tuoyu Wu, Jinwei Gao, and Dawei Wang. "Spatial and temporal evolution of Cenozoic carbonate platforms on the continental margins of the South China Sea: Response to opening of the ocean basin." Interpretation 4, no. 3 (2016): SP1—SP19. http://dx.doi.org/10.1190/int-2015-0162.1.

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Widespread and tremendously thick Cenozoic carbonate sequences are present along the margins of the South China Sea (SCS). However, most of the sequences have been drowned since the Late Miocene. The stratigraphic architecture of the carbonate platforms in the SCS can provide information on the tectonic evolution of the ocean basin. Based on 2D/3D seismic, well and regional geologic data, we have interpreted the Cenozoic SCS carbonate platforms along the continental margins. The carbonate platforms developed during rifting and initiated on the fault block of the conjugate rifted margins. Most
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Krystal, A. "STRUCTURAL AND TECTONIC FACTORS FORMING GAS CONTENT OF COAL-MEASURES UNITS IN WESTERN DONBAS." Tectonics and Stratigraphy, no. 41 (December 18, 2014): 49–55. http://dx.doi.org/10.30836/igs.0375-7773.2014.94602.

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