初论龙门山推覆构造带的基本结构样式

龙门山推覆构造带在构造类型上具有褶皱推覆体和冲断推覆体之分，在形成方式上具有推覆和滑覆两大类型，在形成序次上具有前展式和后叠式的扩张方式，在组合形态或结构上具有推覆滑覆叠加样式，是青藏高原东北边缘推覆构造的普遍特征之一。在形成机制上与扬子地台、特提斯构造带的演化密切相关，是我国陆内造山带的典型推覆构造带。     

节理裂隙岩体的离散元计算方法

岩体通常被弱面所切割、分离，岩体结构的稳定性与弱面性质密切相关，离散元方法是对岩体进行形变分析计算的方法之一。作者介绍了该方法的基本计算步骤并以预应力锚杆为例进行了应力、应变计算推导，为边坡加固、围岩支护提供了一种可靠的计算方法。     

沂沭断裂带构造地貌格局及其形成与演化

沂沭断裂带表现为东西分带、南北分段的棋盘格式构造地貌格局.这种构造地貌格局是由于受到北北东一南南西向挤压作用,断裂带两端受到近南一北向挤压作用而形成的;其形成及发展经历了四个主要阶段.     

求解构造地质应力场的方法─PC-1500袖珍计算机的应用

本文阐明利用多种小构造资料求主应力轴的方法原理，并建立计算机编图计算的数学模 式，对比了手工与计算机编图计算的结果．     

北京地区新构造运动特征与地震的关系

北京地区是新构造运动表现明显地区之一.新第三纪以来受地应力作用,发生各种地壳形变,它直接表现在构造演化和地貌形态上.这种活动与本区地震有着密切的关系.     

武当山推覆构造的几何结构──鳞片叠覆模式

武当山推覆构造由主滑脱面、前缘叠瓦褶断带、中央推覆体带和后缘挤压－伸展带４种构造成分组成。中央推覆体带划分为７个推覆体。各推覆体在平面上呈鳞片状越覆，在剖面上呈送冲叠覆，构成鳞片叠覆的几何模式。     

β＇－Sialon陶瓷的抗热震性

测定了无压和热压烧结两种β’－Ｓｉａｌｏｎ陶瓷的抗热震性能，计算了两者的抗热震参数，发现热压烧结β’－Ｓｉａｌｏｎ的抗热震断裂能力优于元压烧结β’－Ｓｉａｌｏｎ，而抗热震损伤能力却劣于后者。ＳＥＭ分析和理论推导认为，除了力学性能的影响之外，显微结构中微裂纹数量及尺寸直接影响了材料的抗热震性。无压烧结β＇－Ｓｉａｌｏｎ显微结构中微裂纹数量及尺寸均大于热压烧结β＇－Ｓｉａｌｏｎ，这有利于无压烧结材料抗热震损伤能力的提高，但不利于其抗热震断裂能力的提高。     

黄河龙羊峡电站坝区F_7断层新活动性问题的工程地质研究

本文根据断裂动力学、古地震及现代应力积累问题等方面的分析结果,对龙羊峡电站坝区F7断层新活动性特征进行了深入的研究。查明该断层是一条第四纪以来多次活动的古粘滑型发震断层,其最新活动休止时间为晚更新世中晚期,现今应力积累程度只达37.9％,在工程年代内该断层处于相对稳定状态。研究中,现代测试技术的应用有效地解决了分析中的一些重要问题。综合运用热发光绝对年龄测定和石英颗粒表面结构扫描电镜研究,为鉴定断层的最新活动年代提供了新的有效方法;热释光温度测定方法则开拓了研究断层粘滑活动性的新途径。     

Interaction of fluid dynamic factors in the migration and accumulation of natural gas

The migration of fluid petroleum gas, described as fluid potential, depends only on gravity, fluid pressure controlled by depression and capillary force during tectonically stable period; but on tectonic stress during the tectonically active period with severe compression. This method is applied in the Junggar Basin, showing that the migration of Jurassic gas during Cretaceous and Eocene and the migration of Permian gas from Jurassic till the present are determined by capillary force and fluid pressure (including overpressure) which is controlled by depression; the migration of Jurassic gas from Eocene till the present and the migration of Permian gas during Triassic are controlled by tectonic stress.     

Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim basin, China

The petrological characteristics and heavy mineral assembly of the Jurassic System in Kuqa Basin are consistent with the tectonic evolution, which is the major factor controlling the filling process of Kuqa Basin. Controlled by the source areas at the both sides of the Basin, the matrixes are dominated by sedimentary rock, high-grade metamorphic rock, acid magmatic rock, and the highest heavy mineral assemblage of zircon-garnet-magnetite in the content. According to heavy mineral indexes, the Jurassic strata can be classified into three rhythmic units of heavy mineral. The lower sequence contains abundant heavy minerals and relatively high content of detritus and its matrixes primarily came form the recycling orogen. The assemblage of “zircon-garnet-magnetite” indicates that the sedimentary area in the early evolution period of the basin is relatively near the provenance. The middle sequence is different from the lower sequence in the heavy mineral assemblage and has the different characteristics from that of source rock. The heavy mineral assemblage is “garnet-zircon” with the highest content of garnet and its main matrices are the high-grade metamorphic rock, acid magmatic rock and hydrothermal vein at the northeastern edge of the basin. The middle and upper sequences are characterized by the clast provenance, which is primarily from the recycling orogen at the northern edge of the basin and secondarily from the southern uplift. As a result of the two provenances, the strata with apparent changes of heavy mineral assemblage and index better coincides with the interfaces of the secondary strata sequences, which reflects the denudation history and the filling process of the orogen at the northern edge of the basin.