三维电磁阵列剖面法的基本原理及应用

本文论述了三维电磁阵列剖面法的基本原理，并从理论上论述了大地电磁测深中的静态效应是由电磁响应中与频率无关的静态项引起的，基于这一原理，本文提出了三维ＥＭＡＰ野外采集方式和数据处理方程。三维ＥＭＡＰ法不仅能消除ＭＴ中的静态效应，而且由于采集信息量大大增加，较常规ＭＴ有更好的地质效果，文中给出的实例证明了这一点。     

钎焊金刚石钻头模具尺寸设计

勘探用金刚石钻头在钎焊烧结过程中,钻头芯模、外模和钢体的尺寸直接决定金刚石钻头的尺寸,对金刚石钻头的使用性能影响很大,而现有的文献中对于模具尺寸设计的研究稍显不全面。对钻头钎焊烧结过程的热涨与冷缩过程进行深入分析研究,提出了更直观的模具计算公式和防止涨模的措施。     

PC机在控制金刚石合成工艺方面的应用

通过开发压机ＰＣ机的内在功能，编制合理的控制程序，改进了设备的工况，提高了金刚石合成工艺的控制精度。     

航空流网络解构与空域资源动态配置研究——以京-成空中廊道为例

空中廊道作为一种新型航空流组织与空域资源分配方式,是一种复杂的航空流网络,解析其结构特征并评估其结构性能是实现空域资源动态配置的前提。该文通过构建网格时空图方法,以京—成空中廊道为例进行航空流网络解构研究,包括基于航迹簇的网络构型、流量时空波动与航空流聚合分化三方面,据此提出空域资源动态配置方案。研究结论如下:1)以多种邻近阈值指示航迹交叉角度持续增大,检测出航空流网络存在平行流、交叉流、全覆盖流和半覆盖流4种构型,基于其占比和特征的显著差异性提出并行扩容调整方案;2)以高频数网格点状或短线状集中分布指示流量时空波动,检测出航空流网络存在两个不同内涵的时间高峰、以距离中值区为近似对称轴的空间高峰以及在区段间漂移的时空交互高峰,进而提出时间错峰调整方案;3)以网格属性指示聚合分化点的分布,检测出航空流网络阶梯递减、高值集聚和叠合特征,相应提出动态快速分化分流调整方案。     

地理格网模型研究进展

地理格网系统起源于早期的制图研究,并发展成为表达复杂地理现象、综合分析自然与人文数据、模拟地理系统功能与行为的基本方法。地理格网系统的组成包括格元、格边和格点,格元代表了区域面状特征,格点确定了格元的基本位置和点状特征,格边用于度量格元间的通量关系。在现代地球测量技术驱动下,地理格网系统的功能从传统的地图定位框架与地理现象表达,进一步拓展出多源地理空间数据融合、地理综合分析等新功能。研究椭球空间下的地理格网系统构建模型、误差分布、地学计算等是地理格网系统研究的前沿和基础性科学问题。     

世界金刚石矿产资源形势及其保证程度

从世界金刚石矿产资源概况、资源特点出发,分析了资源供需前景,提出了对世界金刚石矿产资源勘查与开发的建议。     

基于Web的金刚石钻头模具钢体设计

介绍了应用网页技术进行金刚石钻头模具钢体设计计算的方法。该方法丰富了模具钢体设计的远程教育,免去了传统人工求解的繁杂过程,界面友好,精度高,结果可靠,具有实际使用价值。      

海洋GIS数据模型与结构

探讨了海洋 GIS中的数据模型和数据结构问题。根据物理海洋学的研究方法 ,提出了海洋 GIS的数据表达模型。针对海洋 GIS中水体的特点 ,提出了适合海洋 GIS水体的多级化格网型数据结构 ,给出了两种大尺度海洋常用的格网化方案 :全球等角格网化方案和全球等面积格网化方案。这种格网型数据结构是普通 GRID的扩展 ,具有鲜明的海洋数据应用特色。     

Overview of the geology, petrology and tectonic framework of the high-pressure–ultrahigh-pressure metamorphic belt of the Kokchetav Massif, Kazakhstan

Abstract High‐ to ultrahigh‐pressure metamorphic (HP–UHPM) rocks crop out over 150 km along an east–west axis in the Kokchetav Massif of northern Kazakhstan. They are disposed within the Massif as a 2 km thick, subhorizontal pile of sheet‐like nappes, predominantly composed of interlayered pelitic and psammitic schists and gneisses, amphibolite and orthogneiss, with discontinuous boudins and lenses of eclogite, dolomitic marble, whiteschist and garnet pyroxenite. On the basis of predominating lithologies, we subdivided the nappe group into four north‐dipping, fault‐bounded orogen‐parallel units (I–IV, from base to top). Constituent metabasic rocks exhibit a systematic progression of metamorphic grades, from high‐pressure amphibolite through quartz–eclogite and coesite–eclogite to diamond–eclogite facies. Coesite, diamond and other mineral inclusions within zircon offer the best means by which to clarify the regional extent of UHPM, as they are effectively sequestered from the effects of fluids during retrogression. Inclusion distribution and conventional geothermobarometric determinations demonstrate that the highest grade metamorphic rocks (Unit II: T = 780–1000°C, P = 37–60 kbar) are restricted to a medial position within the nappe group, and metamorphic grade decreases towards both the top (Unit III: T = 730–750°C, P = 11–14 kbar; Unit IV: T = 530°C, P = 7.5–9 kbar) and bottom (Unit I: T = 570–680°C; P = 7–13.5 kbar). Metamorphic zonal boundaries and internal structural fabrics are subhorizontal, and the latter exhibit opposing senses of shear at the bottom (top‐to‐the‐north) and top (top‐to‐the‐south) of the pile. The orogen‐scale architecture of the massif is sandwich‐like, with the HP–UHPM nappe group juxtaposed across large‐scale subhorizontal faults, against underlying low P–T metapelites (Daulet Suite) at the base, and overlying feebly metamorphosed clastic and carbonate rocks (Unit V). The available structural and petrologic data strongly suggest that the HP–UHPM rocks were extruded as a sequence of thin sheets, from a root zone in the south toward the foreland in the north, and juxtaposed into the adjacent lower‐grade units at shallow crustal levels of around 10 km. The nappe pile suffered considerable differential internal displacements, as the 2 km thick sequence contains rocks exhumed from depths of up to 200 km in the core, and around 30–40 km at the margins. Consequently, wedge extrusion, perhaps triggered by slab‐breakoff, is the most likely tectonic mechanism to exhume the Kokchetav HP–UHPM rocks.     

Grid dispersion in generating finite-differences synthetic seismograms

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