Anisotropy of isothermal remanent magnetism is a recently developed technique for rock fabric study.
等温剩磁各向异性是一种新的磁组构研究方法。
In the area without magma mingling or with weak magma mingling, the host rock is dominated by porphyaceous adamellite showing normal granite fabric.
无岩浆混合作用或岩浆混合作用较弱区段，寄主岩石以似斑状二长花岗岩为主，显示正常的花岗岩结构构造岩浆混合作用强烈区段。
Shaoxing County Chuangjia fabric Qizhou China Textile Factory is located in the South-rock weir Ko Nishimura.
绍兴县创佳织物起绉厂位于中国轻纺城南面柯岩堰西村。
Based on the analysis of geologic background and rock fabric, the authors study the fluid inclusions in the barite of the lacustrine hydrothermal sedimentary rock from the Lower Cretaceous Xiagou Formation in the Qingxi sag of Jiuquan basin.
以地质背景和岩石组构分析为基础，对酒泉盆地青西凹陷下沟组湖相热水沉积岩中的重晶石矿物进行了流体包裹体研究。
A quantitative description technique for orientation analysis of argillaceous rock fabric by X ray diffraction
泥页岩组构X射线衍射定量分析方法
The magnetic lineation and magnetic foliation study of the ore area show that the magnetic fabric study can proclaim the stress field of rock deformation as the petrofabric analysis.
矿区的磁线理、磁面理等磁组构研究表明，磁组构能与岩组研究一样，解决岩石变形的应力场问题。
According to geologic structural location, features of occurrence, rock fabric and geochemical index of basalt in Ruqi clough of Helan Mountain, it can be regarded as continental rift basalt.
根据贺兰山汝箕沟玄武岩的地质构造位置、产状特征、岩石组构和地球化学指标等，将其划归为大陆裂谷玄武岩系列，它代表了典型的陆内拉张环境。
Tectonic-lithological Assemblages of Southern Qinling Accretionary Complex and Their Formation Process; Distribution and structural fabric features of mudstone interlayer of rock salt in underground gas storage
南秦岭增生杂岩带构造岩石组合及其形成过程盐岩地下储气库泥岩夹层分布与组构特性研究
The spheric stress affects the rock and mineral formation and metamorphism, and the differential stress controls the deformation and the fabric variation of rocks.
前者影响成岩成矿和变质作用，后者控制岩石变形和组构的变化。
· that with the variations of country rock pressure and axial differential stress, the above four rock samples all show the variations of velocity, attenuation and permeability, which indicates the variation of fabric, particularly the variation of microcrack.
随着围压和轴向差异应力的变化，四种样品中的波速、衰减和渗透率均发生不同形式的变化，反映了岩样组构特别是微裂隙的变化情况。
Fabric analysis studys vectorial quality of natural rock and unit in space by statistical method and illustrates or probes the produced condition and metastatic history during tectonic movement.
岩组分析是利用统计的方法研究天然岩石及其组成单元在空间向量性质，以阐明或探讨岩石形成时的条件及其在构造运动中的变形历史。
This paper deals with characteristics of the Devonian depositional system in south Guizhou-central Guangxi in terms of rock association, depositional fabric, profile series, biocoenoses, sedimentary mechanism and on the basis of detailed field study and previous data.
以详细的野外调查和前人资料为基础，对岩石组合、沉积组构、剖面序列、生物组合、沉积机理等进行分析，研究了黔南&桂中地区泥盆系沉积体系特征。
The Characteristics of the Surface Movement of the Lobate-shape Rock Glacier From the Debris Fabric, Tianshan, China
从砾石组构看天山叶状石冰川的表面运动特征
Under the structure of deposit, wall-rock alteration, the fabric of ore, the symbiotic composition and relationship of minerals, and so on, mineralization can be divided into two periods: period of sediment diagenesis and construction-hydrothermal period.
根据矿床构造、围岩蚀变、矿石结构构造和矿物共生组合及其相互关系等，可将水银洞金矿成矿作用划分为两个成矿期：沉积成岩期和构造-热液期。
The fabric characteristics formed by oscillation and multidirectional currents in basal clastic rock section;
底部粗碎屑段表现出振荡和多向水流形成的组构特征，无明显的粒序；
Coal is a special kind of rock that is sensitive to stress and strainUnder different stressstrain environment and tectonic stress effect, the physical structure, chemical structure, characteristic of optical property, etcof coal will greatly be changed, and tectonic coal with different structural characteristics and types will be formedVitrinite reflectance changes regularly during the process of tectonic coal deformation, which is extensively applied to the quantitative analysis of coalfield structureThis is also confirmed by deformation experiments under high temperature and confining pressureIn order to further investigate the microscopic mechanism of the change of vitrinite optical fabric, Xray diffraction, paramagnetic resonance and nuclear magnetic resonance were used to study the chemical structure of different types of tectonic coal and experimentally deformed coals under high temperature and confining pressureResearch shows that there is a close internal relation between the evolution of tectonic coal chemical structure and the vitrinite reflectanceThe optical property anomaly of vitrinite reflectance is a concrete manifestation of chemical structure evolution of tectonic coal in physical optical propertyDifferent physical and chemical structure in different types of tectonic coal resulted in a great difference in the characteristics such as gas content, permeability, etcMylonitic coal developed area is a dangerous belt for gas outburst in coal mine because of its high gas content and low permeability which are determined by special physical and chemical structuresTherefore, we can evaluate and predict the enrichment of mine gas and outburst hazard through studying distribution laws of tectonic coalIt provides a new thought and method for research on mine gas disaster.
煤是对应力和应变非常敏感的一种特殊岩石，在不同的应力应变环境和构造应力作用下，煤的物理结构、化学结构及其光性特征等都将发生显著变化，从而形成具有不同结构特征的、不同类型的构造煤。构造煤在变形的过程中，镜质组反射率将发生规律性变化，并被较为广泛地应用于煤田构造的定量研究，高温高压变形实验也证实了这一现象。为了深入探讨煤镜质组光性组构变化的微观机理，将X射线衍射、顺磁共振和核磁共振等技术应用于不同类型构造煤以及高温高压实验变形煤的化学结构研究。研究表明，构造煤化学结构演化与镜质组反射率的演化具有密切的内在联系，镜质组反射率的光性异常是构造煤化学结构演化在物理光学性质上的具体体现。不同类型的构造煤由于物理和化学结构上的不同，导致瓦斯含量和透气性等瓦斯特性上的重大差异，糜棱煤特殊的物理和化学结构决定了其高含气量和低透气性的特征，是矿井瓦斯突出的危险地带，因此，可以通过构造煤分布规律的研究，进行矿井瓦斯富集与突出危险性的评价与预测，为矿井瓦斯灾害的研究提供新的思路和方法。