MTW European Type Trapezium Mill

Input size:30-50mm

Capacity: 3-50t/h

LM Vertical Roller Mill

Input size:38-65mm

Capacity: 13-70t/h

Raymond Mill

Input size:20-30mm

Capacity: 0.8-9.5t/h

Sand powder vertical mill

Input size:30-55mm

Capacity: 30-900t/h

LUM series superfine vertical roller grinding mill

Input size:10-20mm

Capacity: 5-18t/h

MW Micro Powder Mill

Input size:≤20mm

Capacity: 0.5-12t/h

LM Vertical Slag Mill

Input size:38-65mm

Capacity: 7-100t/h

LM Vertical Coal Mill

Input size:≤50mm

Capacity: 5-100t/h

TGM Trapezium Mill

Input size:25-40mm

Capacity: 3-36t/h

MB5X Pendulum Roller Grinding Mill

Input size:25-55mm

Capacity: 4-100t/h

Straight-Through Centrifugal Mill

Input size:30-40mm

Capacity: 15-45t/h

Large vertical mill production line for deepseated rocks

  • An operational approach to ground control in deep mines

    2022年2月1日  Though mining at depth is not new, for example deep gold mining in South Africa and nickel mining in Canada, the new caving operations are not only deep but impact large 2024年3月1日  Methodologies to prevent deterioration for safer deep mining are discussed This paper presents details of the early to midstage deterioration in the form of notch growth of two Notch formation in vertical excavations in a deep hard rock mine 2019年4月13日  Increasing demand for metals caused by global economic growth and exploitation of shallow mineral deposits forces mineral extraction to go deeper A direct Deep Mining: A Rock Engineering Challenge2021年12月9日  The North China Craton is one of China’s major goldproducing areas Breakthroughs have been continually made in deep prospecting at depths of 500–2000 m in the Jiaodong Peninsula, and geophysical methods have A GeologicalGeophysical Prospecting Model for

  • Mitigating a DeepSeated Landslide Hazard, Leyte

    2010年4月9日  Mitigating a DeepSeated Lands lide Hazard the Case of 105 Mahiao Slide Area, Leyte Geothermal Produc tion Field, Philippines Winston Philip C Pioquinto 1 , Joe ffrey A Cara nto 1 , Lauro F 2023年4月25日  Toppling deformation is a unique geological form in rock slopes, with complex geomechanical behavior and engineering properties A large number of deepseated toppling deformation slopes are developed in the deep incised valleys in Southwest China By summarizing these typical slope cases, it is found that there are certain differences in the rock Evolutionary mechanisms of deepseated toppling deformation of 2010年1月1日  A near exponential decrease of permeability with depth d (m) according to log 10 (k) = −14 − 32 × log 10 (d) was also suggested in general for nonsedimentary crustal rocks by Manning (PDF) Structure and permeability of deepseated rocks in the 2016年12月30日  Deepseated largescale toppling failure presents unique challenges in the study of natural slope deformation process in mountainous regions An active deepseated toppling process was identified in the Erguxi slope located in southwest China, which affected a large area and damaged critical transportation infrastructure with the volume of the deforming Deepseated largescale toppling failure in metamorphic rocks

  • Analyses on drainage capacity and sliding resistance of large

    2019年10月11日  Analyses on drainage capacity and sliding resistance of large diameter vertical wells for deepseated landslide stabilization Ba Thao Vu 14,16, Van Minh Pham 14, Quoc Dung Nguyen 14,15, Huy Vuong Nguyen 14 Our results 2016年12月14日  Ductile flexural toppling is commonly recognized to result in the formation of large and deepseated topples (Nichol et al 2002;Hungr et al 2014); however, when certain discontinuities exist Deepseated largescale toppling failure in metamorphic rocks: a 2024年10月8日  INTRODUCTION The reflection seismic method is a powerful geophysical technique that uses the reflection of seismic waves to obtain an image of the earth's subsurface (Yilmaz, 2001)Reflected seismic waves bring information about the rocks and geological structures in the subsurface (Ahmadi, 2015)Active seismic methods are widely employed by Seismic imaging of deep‐seated gold deposit and host rocks 2021年9月22日  1 Introduction Deepseated gravitational slope deformations (DGSDs) are large and slow rockmass movements (slip rate of a few mm/year) commonly affecting the entire relief slope and involving ∼200–300 m thick rock volumes, with relatively small displacements compared to the slope dimensions (Agliardi et al, 2001, 2012; Dramis SorrisoValvo, 1994; Active Faulting and Deep‐Seated Gravitational Slope Deformation

  • Structure, Mineralogy and Geomechanical Properties of Shear

    2016年10月25日  Deepseated rockslides, which are characterised by slow to extremely slow rates of movement, frequently occur in foliated metamorphic rock masses (schists, phyllites, paragneiss series) Many case studies indicate that slope displacement is predominantly localised at basal and internal shear zones Thus, the deformation and stability behaviour of rockslides 2022年3月17日  Shidaguan slope (hereinafter short for SDG slope) is an unstable rock slope with an area of 3078 × 104 m2 and a deformation depth of 30–70 m in Maoxian County, Sichuan Province, China Three seismometers (P2–P4) with high sensitivity were installed at different locations on the unstable part of the slope P2 and P3 were almost at the same elevation Geology amplification of the seismic response of a large deepseated 2016年4月12日  The largescale deformation of high mountain slopes finds its origin in many phenomena (inherent parameters, external stresses) with very different time constants (instantaneous to geological scale) Gravitational effect, tectonic forces and water infiltration are generally the principal causes of slope instability However, it can be very difficult to distinguish Longterm monitoring of a large deepseated landslide (La 2014年1月1日  Rocks from the sea floor differ from those encountered on land due to their shape and their chemical composition The effect of seawater and the pressure it exercises on hot, outpouring lava will fashion the shape of deepsea volcanic rocks giving the sea floor a different appearance than what we see in subaerial environmentsSea Floor Rocks SpringerLink

  • Active Faulting and Deep‐Seated Gravitational Slope Deformation

    2021年9月22日  1 Introduction Deepseated gravitational slope deformations (DGSDs) are large and slow rockmass movements (slip rate of a few mm/year) commonly affecting the entire relief slope and involving ∼200–300 m thick rock volumes, with relatively small displacements compared to the slope dimensions (Agliardi et al, 2001, 2012; Dramis SorrisoValvo, 1994; 2020年11月14日  Identifying deepseated toppling failure presents unique challenges for the study of natural slope deformation in mountainous regions In the absence of an effective quantitative approach, this study aims to provide a comprehensive grading system in order to establish a slope engineering geological model that can evaluate the deformation of a deep Identification and zonation of deepseated toppling deformation in 2020年4月22日  An old largescale landslide with a volume of 46 × 106 m3 located on the right bank of the Lancang River, Southwest China, was formed by the deepseated toppling failure of a rock mass The rock mass located downstream of the landslide toppled intensely with a maximum toppling depth exceeding 200 m and a volume over 15 × 108 m3 We studied the formation DeepSeated LargeScale Toppling Failure: A Case Study of the 2021年9月17日  PDF Shidaguan Slope (hereinafter short for SDG Slope) is an unstable rock slope with an area of 3078×10 ⁴ m ² and a deformation depth of 3070 m in Find, read and cite all the research (PDF) Seismic Site Response of A Large Deepseated Rock

  • Deformation characteristics and multislab formation of a deepseated

    2019年5月1日  This study presents the results of a more than 10yearlong field investigation and remote sensing monitoring campaign of a highly active deepseated rock slide located in a glacial to periglacial environment (Bliggspitze, Tyrol, Austria) Data concerning (i) the terrain surface displacements based on imagery (webcam timelapse, orthoimages) and both terrestrial and 2006年3月14日  [17] Spatial density of large landslides in the WSA is 12 × 10 −2 km −2, ie, 3 times that of rock avalanches in the central Southern Alps (42 × 10 −3 km −2 [Whitehouse, 1983]), and that of large deepseated failures in the stronger crystalline basement rocks of the adjacent Fiordland Mountains (4 × 10 −3 km −2 [Korup, 2005b])Effects of large deep‐seated landslides on hillslope morphology 2012年4月25日  Major element, trace element and Nd–Sr isotopic data are presented for 82 plutonic rocks from the southern Coast Mountains Batholith (CMB) in British Columbia, Canada, ranging in emplacement age from 210 to 50 Ma The rocks are part of a large composite magmatic arc batholith, which the major element data show to be of calcalkaline affinityElemental and Isotopic Evidence for Granitoid Genesis From DeepSeated 2017年7月1日  New versions of the universal JdDi exchange clinopyroxene barometer for peridotites, pyroxenites and eclogites, and also garnet barometer for eclogites and peridotites were developedDeep seated magmas and their mantle roots:

  • Deformational Features of DeepSeated Gravitational Slope

    2020年12月22日  Deepseated gravitational slope deformation, referred to as DGSD by Dramis and SorrisoValvo (), is a largescale, voluminous, and longlasting slope movementDGSD has various types such as buckling, toppling, sliding, and dragging depending on the morphological relationship between bedding planes (foliation) and the slope (Chigira 2000)2019年9月1日  Local settings of the Obir Fault site: (A) hillshaded digital terrain model illuminated from NW with depicted Obir and Periadriatic Line (PAL) fault systems, deepseated gravitational slope Gravitational and tectonic stress states within a deepseated 2020年6月15日  1 Introduction Large, deepseated landslide failure can be accompanied by a catastrophic impact on societies and infrastructures This kind of landslide is often preceded by large periods (on the order of several years) of creep until On the Stability of Deep‐Seated Landslides The Cases of Vaiont 2016年6月6日  Hydromechanical Rock Mass Fatigue in DeepSeated Landslides Accompanying Seasonal Variations 2349 123 fractures), such as the rock slope behaviour observed inProgressive failure in deepseated rockslides due to seasonal

  • A health management system for large vertical mill ResearchGate

    2020年3月1日  As large vertical mill always works in severe conditions, the online monitoring, timely fault diagnosis, and trend prediction are very important guarantees for the safe service and saving 2012年2月1日  This paper deals with three large DeepSeated Landslides (DSLs) at a front of a subalpine meridional chain, on the “La Marbrière” slope near the town of Grasse (AlpesMaritimes, France) The geological framework controlling the stability and morphology of the DSLs is associated with thick and tamped Triassic layers of mudstone with gypsum overlain by Evolution stages of large deepseated landslides at the front of a 2012年12月12日  During the last decade, several rainfallinduced deepseated large landslides with volumes of the order of 1 million m3 were triggered in various locations in Slovenia (central Europe), each representing a serious threat to the nearby villages and traffic infrastructure and urging to be mitigated The Macesnik landslide, triggered in 1989, and the Slano blato Reinforced concrete shafts for the structural mitigation of large deep 2021年11月4日  In addition, this interaction may be of concern even for deep tunnels in areas such as deepseated landslides (DSL) (Yong et al 2013; Bandini et al 2015; Salmi et al 2017; Zhou et al 2020) DSLs are large mass movements with a recognized failure surface and a large rock volume detaching from that surface, and the depth of the sliding surface can reach Twin tunneling–induced deepseated landslide in layered sedimentary rocks

  • Tectonic constraints on a deepseated rock slide in weathered

    2017年8月1日  Deepseated rock slides (DSRSs), which are often related to deepseated gravitational slope deformation (DSGSD) (Dramis and SorrisoValvo, 1994, Ambrosi and Crosta, 2006, Hradecký and Pánek, 2008), have been recognised as one of the most important mass wasting processes worldwide over the past several decades (Hutchinson, 1968, Saunders and 2021年12月24日  512 Formation of DeepSeated Faults and Folds and Their Relationship with the FoldandThrust Belts The formation periods of these deepseated faults and folds are hotly debated, and two theories have been advanced: early formation during the Indosinian and late formation during the CenozoicControls of Deep‐Seated Faults and Folds on Hydrocarbon Fluid 2022年3月17日  PDF Shidaguan slope (hereinafter short for SDG slope) is an unstable rock slope with an area of 3078 × 10⁴ m² and a deformation depth of 30–70 m in Find, read and cite all the Geology amplification of the seismic response of a 2019年3月8日  To understand the magnetic signal from deepseated rocks, we need to explore the sources and nature of the magnetic mineralogy This paper reviews the magnetic properties of rocks that formed deep in the Earth's crust Magnetic Mineralogy and Petrophysical Properties

  • (PDF) The Beauregard dam (Italy) and the deepseated

    2006年10月23日  Large storage dam projects may modify geoenvironmental conditions in many ways The reservoir impoundment of the 2855 m high Xiluodu arch dam located on the Jinsha River (China) caused large 2022年12月5日  The movement of large, slowmoving, deepseated landslides is regulated East–west and vertical cumulative displacements measured by Thick lines represent mean 2D velocity time Acceleration of a large deepseated tropical landslide due to 2014年10月28日  Landslides with A s > 10,000 m 2 are expected to be predominantly bedrock, relatively deepseated (>10m deep), and in the Kii Peninsula, they often display complex geotechnical and hydrological Large deepseated landslides controlled by geologic structures 2020年5月26日  Large (deepseated) landslides present complex geometries, rock/soil properties, and kinematical behavior Complex geometries are due to the presence of several sliding zones, while complex properties typically result from the dilation, compression, or fatigue of geologic materials Kinematical behavior is often episodic, with periods of stability followed by Forecasting the longterm activity of deepseated landslides via

  • A 3D Predictive Method for DeepSeated Gold Deposits in the

    2022年7月25日  With the rapid depletion of mineral resources, deep prospecting is becoming a frontier field in international geological exploration The prediction of deep mineral resources is the premise and foundation of deep prospecting However, conventional metallogenic predictive methods, which are mainly based on surface geophysical, geochemical, and remote sensing 2018年7月19日  It represents a keyinterpretive map for identifying the deepseated structural features The stripped gravity map allowed the identification of two low topographic areas to the south of RBoil field They outline location of two deep basins, where the preMiocene rocks were preserved in the down thrown blocks of the major faultsAn integrated analysis of gravity and well data for deepseated 2024年11月1日  Highprecision aeromagnetic survey data revealed a vast expanse of deepseated granitoids within the Gonghe basin, a finding substantiated by geothermal well findings (Zhang et al, 2020b) Triassic intrusive igneous basement rocks with a thickness of approximately 10 km were identified through gravimetric measurements (Zhang et al, 2018b)Deepseated radiogenic heat production characteristics in the

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