下运带式输送机液压制动系统的试验研究

针对下运带式输送机液压制动系统的不同运行工况和动态特性,设计了实验室试验系统,介绍了试验的原理和步骤,分别模拟试验了液压制动系统的空载发热、最大制动力矩、正常制动、超速调速制动等不同的运行工况,并对制动系统的压力、转矩以及油液温度进行实时检测。试验结果表明:该液压制动系统有很好的制动效果,且具有控制智能化、发热小、响应迅速、冲击较小等优点,能够满足下运带式输送机各工况制动性能的要求。     

“一带一路”愿景下民族地区与海洋文化的现实机缘

分析了中国草原丝路、沙漠丝路、西南丝路和海上丝路所途径的民族地区与海洋文化割裂不断的历史联系和现实机缘,指出了在当今的海洋时代,借助“一带一路”的开发和建设,建构中国海洋文化全球传播民族路径的重大意义。     

卧式椭圆轨迹振动筛的自定中心问题研究

当振动筛筛箱各点作长轴平行于筛面的椭圆轨迹运动时,这种振动筛的胶带轮不可能只作定轴转动(即自定中心)。如果恰当地选择胶带轮几何中心的偏心值,胶带轮的摆动幅度将减小,因此,胶带的工作情况仍将得到改善。     

中新生代天山板内造山带隆升证据：锆石、磷灰石裂变径迹年龄测定

取自天山南侧库车盆地北缘欧西达坂花岗岩体的锆石、磷灰石裂变径迹年龄给出了初步结果：中 新生代天山板内造山带在早白垩世（134Ma～109Ma）发生了明显快速隆升,平均隆升速率为0.13mm/a（130m/Ma）;而从晚白垩世到现在,天山板内造山带的平均隆升速率为0.03mm/a（31.9m/Ma）。在晚新生代天山板内造山带再次发生了快速隆升。现有的同位素研究成果表明中新生代天山造山带至少发生了两次幕式快速隆升。     

梯形齿与双圆弧齿同步带传动精度分析

分析了同步带齿与轮齿齿形参数在传动中产生的多边形效应基础上,建立了同步带传动精度计算模型,由此分析了紧迫长度、带与轮齿形参数对传动精度的影响,并对梯形齿、双圆弧齿同步带传动精度进行了计算和比较,为同步带在精密设备上的应用提供了计算依据。     

太阳散射辐射测量装置的设计

为实现太阳散射辐射的自动测量,设计一种简单方便的测量装置。该装置可与全自动太阳跟踪器连接在一起,代替现有的遮光环装置。太阳散射辐射测量装置通过利用直接辐射表赤纬轴的转动来实现遮光装置赤纬轴的转动,整个遮光装置放置在全自动太阳跟踪器外壳上,实现遮装置时角轴的转动。整个装置采用齿形带传动,在利用平行四边形结构的同时也更好地保证了精度。     

秦岭佛坪穹隆盖层岩系的地质和地球化学特征

地质和地球化学研究表明,佛坪穹隆盖层岩系主要由晚震旦—晚古生代地层组成,呈变质程度不等的变质岩产出,构成以佛坪基底杂岩为核心的中心式递增变质带。认为该岩系经历了多期构造变形,与穹隆核部基底杂岩以剪切带或断层接触,其原岩为陆源碎屑岩－碳酸盐岩组合,形成于扬子板块北缘的被动大陆边缘（Ｚ２－Ｐｚ１）和秦岭微板块内的陆表海（Ｐｚ２）沉积环境。     

Characteristics and geological significance of the eclogites from the Tongbai Mountains, Henan Province

Some eclogites and the related high-P metamorphic belt have been found for the first time from the Tongbai Mountains, Henan Province, where the eclogites and their probable retrogressive products ——garnet amphibolites——occur as lenses in mica-schists. The fresh eclogites comprise garnet, omphacite, quartz, rutile, phengite, barroisite, etc. The compositional features of garnet and available geothermobarometers indicated that the eclogites belong to the low-T type. The mica-schists contain phengite, quartz, garnet and rutile that are also attributed to high-P assemblage. The eclogites and related high-P belt probably belong to the Early Paleozoic in age, which is distinct from the Indosinian Dabie high- and ultrahigh-P metamorphic belt.     

The age of Xiannü Mountain fracture belt in Three-Gorge region——A fission track study

Apatite was separated from fault-clay, fracture-cliff rock and fracture wall rock, which were collected from Huangkou fracture north to Xiannu Mountain lying 20 km southwest to Three Gorges Dam Project-Sandouping dam. The fission tract characters and their length variations of apatite show that Xiannu Mountain fracture belt was formed at (0.7 ± 0.04)Ma, but its wall rock at (25.31 ±2.8) Ma. This result and previous studies show that no activity has happened since the Holocene, and the Three Gorges Dam Project is not affected by activity of the Xiannu Mountain fracture belt.     

Discovery of the highly depleted N-MORB-type volcanic rocks: new evidence for the Mianlue paleo-ocean

The highly depleted N-MORB-type volcanic rocks have been discovered in Mianlue mélange of Qinling orogenic belt, central China. These mafic rocks are associated with the meta-peridotites, showing LREE-depleted pattern, similar to N-MORB and typical ophiolites. It is indicated that an ancient ocean existed in the Mianlue area of Qinling orogenic belt during the late Paleozoic.