Showing 41 - 60 results of 65 for search 'different surface uplift', query time: 0.12s Refine Results
  1. 41

    Characteristics and Causes of Extreme Heavy Rainfall in Heilongjiang Province During August 2023 by Qi Duo, Wang Chengwei, Bai Xuemei, Gong Yanduo, Sun Qi, Luan Chen, Tang Kai, Zhao Yujie

    Published 2024-05-01
    “…Convection is developed and strengthened by the combined action of systematic uplift by a trough at 500 hPa, warm shear at 850 hPa, topographic convergence, and uplift. …”
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    Article
  2. 42

    Dynamic Response of Pile-Net Composite Subgrade under Coupled Seismic-Train Load Effect by DENG Yousheng, ZHANG Keqin, LI Hui, LI Wenjie, ZHAO Huiling, MA Erli

    Published 2025-05-01
    “…Therefore, it is necessary to study the dynamic response of pile-net composite subgrades at different train running speeds and peak accelerations. …”
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  3. 43

    Comparative Study on REE Occurrence Mode in Ion- adsorption Type REE Deposits from Changting, Fujian, and Northern Myanmar by Xiaoyu LI, Wenliang XIONG, Lijun ZHANG, Da CHEN, Zhimin ZHU

    Published 2025-08-01
    “…The weathering degree in Changting mining area is higher, and the CIA index is as high as 92.07%, which may be the main reason for more clay minerals in Changting mining area, it is also easier to develop colloidal rare earths closely embedded with clay minerals such as psilomelane and kaolinite than in northern Myanmar; Although the weathering degree of northern Myanmar mining area is low, the preservation thickness of iREE ore body in northern Myanmar is larger, which may be that its geomorphic conditions are more conducive to the preservation of iREE - crustal uplift and surface denudation in northern Myanmar may be closer to the threshold, or there may be a more reasonable alternating interval of strong and weak erosion; iREE tailings formed after leaching of iLREE deposit is generally a clay material with low REE and stable chemical properties. …”
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  4. 44

    Insights Into Spatiotemporal Evolution of Induced Earthquakes in the Southern Delaware Basin Using Calibrated Relocations From the TexNet Catalog (2017–2022) by Asiye Aziz Zanjani, Heather R. DeShon, Vamshi Karanam, Alexandros Savvaidis

    Published 2025-06-01
    “…Abstract This study presents a comprehensive analysis of induced seismicity (2017–2022) and InSAR‐derived surface deformation in the southern Delaware basin. …”
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  5. 45

    RIEDEL MEGASHEARS R' AND THE TREND TO GRAVITATIONAL EQUILIBRIUM AS MAIN FACTORS OF TSUNAMIGENIC EARTHQUAKES by M. A. Goncharov, E. A. Rogozhin, N. S. Frolova, P. N. Rozhin, V. S. Zakharov

    Published 2015-09-01
    “…And it is the boundary between these regions of the Earth surface subsidence and uplifting, to which tsunamigenic earthquake are confined at reverse faults of the seabed surface with the raised wall facing the trough (Fig. 42). …”
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  6. 46

    Key technology research and development and prospects for outdoor large- and medium-sized snow groomers by Jiawei SHENG, Zhehan CHEN, Yanli YANG, Chun JIN, Lifang ZHENG, Xixia LIU, Weidong LUO

    Published 2025-06-01
    “…We analyzed challenges such as adapting to different environments, reducing track weight, and ensuring quality control of the body surface. …”
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  7. 47

    Crustal thickness and lithospheric properties of Mercury constrained by gravity data by Qingyun Deng, Mao Ye, Weifeng Hao, Chi Xiao, Zhen Zhong, Denggao Qiu, Wensong Zhang, Chong Zheng, Yichen Wang, Jianguo Yan, Jean-Pierre Barriot, Zhiyong Xiao, Fei Li

    Published 2025-06-01
    “…The global crustal thickness variations are obtained by inverting the Bouguer gravity anomaly, which is suggested to be correlated with the mantle uplift of large impact basins, partial melt of mantle materials, or/and intra-lithosphere contractional strain. …”
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  8. 48

    METHODOLOGY FOR CALCULATION OF RIGIDITY IN EARTH DAM SLOPE PROTECTION UNDER CONDITIONS OF WAVE IMPACT by E. I. Mikhnevich

    Published 2018-04-01
    “…While calculating diameter of dumped rip-rap material the following shearing forces have been taken into account: uplift wave pres- sure depending on wave height; drag force which is formed on the slope due to back sweep of wave; shearing component of protection material gravity force which is dependent on preselected slope ratio. …”
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  9. 49

    Fluvial terrace formation in a mountainous area (2): influence of eustatism, tectonics and altitudinal distribution of watersheds based on an allostratigraphic study (Albania) by Mugnier, Jean-Louis, Guzmán, Oswaldo, Vassallo, Riccardo,  Matraku, Kristina, Jouanne, François

    Published 2024-12-01
    “…This variety is controlled by the respective amount of the three parameters: lateral erosion, aggradation and difference between incision and aggradation.Active faults offset the paleoriver profiles at throw rates locally greater than 1 mm·yr-1 and the tectonic uplift influences the long term incision: Nested strath terraces or nested filled terraces with substratum risers occur in zones of high uplift rate (greater than 0.4 mm·yr-1), superposed units and nested fill terraces with hidden substratum risers occur in the weakly uplifted zones of the intra-mountainous graben-like structures.Most of the Albanian terraces are located above straths (nearly flat erosional surfaces) linked to phases of lateral beveling. …”
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  10. 50

    Structural Deformation Style and Seismic Potential of the Maoyaba Fault, Southeastern Margin of the Tibet Plateau by Xianbing Zhang, Ning Zhong, Xiao Yu, Guifang Yang, Haibing Li

    Published 2025-04-01
    “…The southeastern margin of the Tibet Plateau represents one of the most seismically active zones in China and serves as a natural laboratory for investigating the uplift dynamics and lateral expansion mechanisms of the plateau. …”
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  11. 51

    Tectonic deformation and seismic mechanism of the 2021 Aksai MS 5.5 earthquake by ZOU Xiaobo, LI Xingjian, SHAO Yanxiu, YUAN Daoyang, QIU Jiangtao, YIN Xinxin, KOU Junyang

    Published 2024-11-01
    “…Both the ascending and descending orbit surface deformation fields showed uplift near the epicenter with similar magnitudes and signs in the line-of-sight direction, indicating that the earthquake rupture was mainly thrusting. …”
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  12. 52

    Holographic generalised Gukov-Witten defects by Pieter Bomans, Lorenzo Tranchedone

    Published 2025-03-01
    “…We give compelling evidence for this claim by uplifting the solutions to type IIB supergravity and showing that the five-dimensional 1 2 $$ \frac{1}{2} $$ -BPS solutions uplifts to the bubbling surface operators solutions. …”
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  13. 53
  14. 54

    Ground ice and hydrothermal ground motions on aufeis plots of river valleys by V. R. Alekseev

    Published 2015-03-01
    “…Combination of these processes may cause a rapid (often unexpected) reconfiguration of channels of both surface and subsurface runoff, abrupt uplifts and subsidences of the surface, and decompaction and «shaking-up» of seasonally thawing and seasonally freezing rocks, which may create exceptionally unfavorable conditions for construction and operation of engineering structures. …”
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  15. 55

    Temperature variability and its governing mechanisms within the Jailolo Strait, Indonesia

    Published 2025-04-01
    “…In the upper thermocline (40–100 m), two temperature minima occur: one in April due to outflow to the Pacific Ocean, and another in August due to uplifted water. Different cooling processes mark the dominant annual variation in the mid thermocline (100–150 m depth) and the lower thermocline (150–200 m). …”
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  16. 56

    Causes of the Outer Spiral Rainbands in Typhoon Yagi ( 2018) in Shandong Province of China by Chunyan SHENG, Sudan FAN, Qiaona QU, Shijun LIU, Wengang ZHU

    Published 2025-06-01
    “…What are the differences between outer spiral rainbands? These issues deserve further studies.…”
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  17. 57

    Radiative and MHD Effects on Time-Dependent Thermal-Material Transfer by Micropolar Binary Mixture by Md. Mosharrof Hossain, R. Nasrin, Md. Hasanuzzaman

    Published 2022-01-01
    “…An analysis of unsteady magneto-convective heat-mass transport by micropolar binary mixture of fluid passing a continuous permeable surface with thermal radiation effect has been introduced in this paper. …”
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  18. 58

    INTERBLOCK ZONES IN THE CRUST OF THE SOUTHERN REGIONS OF EAST SIBERIA: TECTONOPHYSICAL INTERPRETATION OF GEOLOGICAL AND GEOPHYSICAL DATA by K. Zh. Seminsky, N. O. Kozhevnikov, A. V. Cheremnykh, E. V. Pospeeva, A. A. Bobrov, V. V. Olenchenko, M. A. Tugarina, V. V. Potapov, R. M. Zaripov, A.S. Cheremnykh

    Published 2015-09-01
    “…The methods and techniques used in studies along the transect complement each other and make it possible to investigate different properties of interblock zones. In general, in comparison with blocks, the zones are distinguished by the relief lowering, anomalous water exchange conditions, gas anomalies that are positive and complex in shape, and low resistivity values both near the surface and at depth (Fig. 3–6, 8, and 11–16). …”
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  19. 59

    Geodetic Evidence of the Interannual Fluctuations and Long-Term Trends Over the Antarctic Ice Sheet Mass Change by Yuanjin Pan, Xiaohong Zhang, Jiashuang Jiao, Hao Ding, C. K. Shum

    Published 2025-01-01
    “…In addition, the glacial isostatic adjustment (GIA) effect is found to play a key role in the large-scale VLM uplifting of the West AIS. After evaluating five different GIA models with GPS vertical velocity, we suggest that the ICE-6G_D model can more effectively correct GIA signals in GPS observations over Antarctica.…”
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  20. 60

    CRYOGENESIS AND GEODYNAMICS OF ICING VALLEYS by V. R. Alekseyev

    Published 2015-09-01
    “…Combined, these processes lead to rapid and often incidental reconfigurations of the surface and subsurface runoff channels, abrupt uplifting and subsiding of the ground surface, decompaction and 'shaking-up' of seasonally freezing/thawing rocks, thereby producing exceptionally unfavourable conditions for construction and operation of engineering structures.Formation and development of river networks are heavily influenced by aufeis deposits and processes taking place at the aufeis surfaces, especially in areas of discontinuous and continuous permafrost where an average thickness of the ice cover on rivers ranges from 1.0 to 2.5 m, and the major part of the ice cover is accumulated layer by layer due to freezing of discharged groundwater. …”
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    Article