Identifying the origin of the magnetic directional anomalies recorded in the Datong loess profile, northeastern Chinese loess plateau   总被引：3，自引：0，他引：3  

Rixiang Zhu  Qingsong Liu  Yongxin Pan  Chenglong Deng  Jimin Sun 《Geophysical Journal International》2006,164(2):312-318

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Retrograde evolution of quartz segregations from the Dos Picos shear zone in the Nevado-Filabride Complex (Betic chains,Spain). Evidence from fluid inclusions and quartz c-axis fabrics     

J. M. González-Casado  C. Casquet  J. M. Martínez-Martinez  V. Garcia-Dueñas 《International Journal of Earth Sciences》1995,84(1):175-186

Synkinematic quartz veins are ubiquitous in the shear zone separating the Veleta unit from the Calar Alto unit in the internal part of the Betic Cordilleras. They have been studied with respect to quartz c-axis fabrics, microstructures and fluid inclusions. Veins were probably generated during syn-metamorphic stacking of the units at P = 500 – 600 MPa and T = 400 – 500°C. Quartz displays two groups of microstructures in the shear zone: (1) older coarse-grained mosaics (CGM) resulting from exaggerated grain growth; and (2) younger fine-grained mosaics (FGM) developed at the expense of the former. The fine-grained mosaics show polygonal granoblastic and elongate mosaic microstructures in general, with ribbon microstructures often found near the boundary of the units. Fluids contained in secondary inclusions vary from high salinity brines to different types of CO₂—brine mixtures and low density CO₂ fluids. Differences in composition and P-T trapping conditions are indicated for the different types of inclusions. Some fluid inclusions are older than the FGM, whereas others are younger, thus constraining the P- T conditions at which the two microstructural events took place. Fluid inclusion evidence suggests conditions of P_fluid > 170 MPa and T 370–430°C for the CGM and P_fluid 20–80 MPa and T > 340°C for the FGM.The quartz c-axis fabrics dealt with here correspond to the second recrystallization event, as little evidence of older fabrics is preserved in the shear zone. C-axis patterns vary across the shear zone from slightly asymmetrical type I crossed girdles in the hanging wall and footwall to more asymmetrical crossed girdles at the boundary of the units. This indicates a correlative increase in the magnitude of the heterogeneous shear strain in the same direction. Most of the deformation is concentrated at the top of the Veleta unit. The sense of movement is top to the west, in agreement with other kinematic markers.The quartz c-axis fabrics resulted from dynamic recrystallization during simple shear. The retrograde P-T path inferred from fluid inclusion analysis, along with other geological and geochronological evidence, indicates that this deformation is coeval with a reduction in the crustal overburden.Geochronological and stratigraphic data show that the proposed Dos Picos extensional detachment, separating the Calar Alto and Veleta units, took place during the early Miocene, synchronous with the intense thinning of the Nevado-Filábride Complex and of the whole continental crust underlying the Alborán Basin.  相似文献   

石英c轴组构影响因素探讨:以郯庐断裂带糜棱岩为例   总被引：1，自引：1，他引：0  

王勇生  杨秉飞  王海峰  余顶杰 《岩石学报》2016,32(4):965-975

石英是自然界中最主要的造岩矿物之一,也是地壳流变过程的主要变形矿物,其c轴组构特征与变形温度、剪切指向具有密切的关系,因而常被用来获取剪切指向、估计变形温度、计算运动学涡度等。但由于受到变形分解、先存构造、流体等因素的影响,同一岩石中常会得到多个不同的石英c轴组构结果。如果天然变形岩石同时受到多种因素的影响,其石英c轴组构会表现为何种特征?与岩石变形温度、剪切旋向是否仍具有很好的对应性?基于以上问题,本次工作以大别山东缘郯庐断裂带内经历了多期变形、富含流体活动的超糜棱岩为研究对象,在同一岩石薄片中选择不同区域,利用EBSD开展石英c轴组构分析。分析结果表明,选择的超糜棱岩的石英c轴组构点极密分布形态指示岩石变形发生于非共轴变形条件下;剪切指向方面,6个分析区域中区域1表现为左旋剪切指向特征,与薄片中优势剪切指向一致,而除区域4外的其他4个区域显示出与优势剪切指向相反的右旋剪切指向特征;变形温度方面,区域4以柱面滑移为主,显示了高温变形特征,而其余5个区域均以底面滑移为主,指示了低温变形环境。根据本次石英c轴组构特征分析结果,可以得出一些认识:岩石中石英表现为完全的GBM动态重结晶,所指示的温度明显高于大量沿糜棱面理分布的绿泥石所指示的绿片岩相环境,显示流体活动促进了岩石变形;而石英c轴组构指示的变形温度为绿片岩相环境,与绿泥石存在的现象一致,表明糜棱岩化过程中流体活动对石英c轴组构的影响并不明显。在发生过多期变形事件的岩石中,岩石中早期高温变形信息有可能保留下来并记录在石英c轴组构特征中,因而通过石英c轴组构分析有可能获得早期事件的信息;虽然石英c轴组构影响因素众多,但首先开展详细的显微镜下观察,然后有选择地对剪切指向清晰区域开展石英c轴组构分析,仍然能够得到与岩石中优势剪切指向一致的石英c轴组构结果。  相似文献   

岩石磁组构可以揭示应变吗？——以华南地块早三叠世灰岩为例   总被引：1，自引：1，他引：0       下载免费PDF全文

韩玉林  谈晓冬 《地球物理学报》2009,52(10):2588-2594

一般认为磁组构能有效地反映岩石所经历的应变特征.为了研究不同类型的磁组构和不同期次应变之间的关系,对来自华南地块两个地区的早三叠世灰岩样品进行了岩石磁学、磁组构以及应变特征的对比分析.来自湖北通山县的样品经历了三期构造变形,这为解析磁组构和多期次应变提供了理想的机会.岩石磁学结果显示携磁矿物主要为磁铁矿.磁化率各向异性（AMS）和非磁滞剩磁各向异性（AAR）结果显示其最小轴与层面垂直,最大轴和中间轴分布于层面内,反映了沉积和压实作用产生的应变,而后期构造应变在磁组构中没有体现.来自广东连县的样品发育有渗透性压溶缝面理和方解石脉,说明经历了构造应变.AMS结果没有显示占优势的组构方向.AAR结果显示三轴组构,其最大轴分布于最大应力方位,与构造应变特征吻合,最初的压实组构被构造应变组构所代替.上述结果表明：（1）AAR可以很好地反映渗透性应变的特征,而AMS有时会失效;（2）应变的尺度要小于样品的尺度,磁组构才能有效地反映应变.  相似文献   

Correlation between rock fabrics and physical properties of carbonate reservoir rocks   总被引：5，自引：0，他引：5  

H. Dürrast  S. Siegesmund 《International Journal of Earth Sciences》1999,88(3):392-408

 Three carbonate core samples from an oil and gas reservoir of the NW German basin were chosen to study the correlation between rock fabrics and physical properties of reservoir rocks. Detailed fabric analyses and texture investigations were carried out as well as laboratory measurements of different physical properties, e.g. density, porosity, permeability, electrical conductivity, seismic compressional and shear wave velocities. Although the three core samples come from a similar depositional facies, they show great differences in the occurrence and three-dimensional distribution of the rock fabric elements. These heterogeneities are the result of various diagenetic and tectonic processes. For the correlation between the rock fabrics and the physical properties four main rock fabric types have to be considered: (a) major constituents, e.g. fossils, ooides, peloides and crystals; (b) pore space with different pore types; (c) fractures; and (d) stylolites. The results of the correlation clearly show that the values and anisotropies of the petrophysical properties are fairly related to the observed fabric elements, with their different arrangements, spatial distributions and preferred orientations. These results also provide a fundamental understanding of the petrophysical responses, such as seismics, to the different geological features (e.g. fractures) and their dynamic changes with pressure, which can be converted to different depths. The knowledge gained from such correlations may lead to an improved interpretation of geophysical data for hydrocarbon exploration and production and therefore to an advanced reservoir characterization. Received: 28 January 1999 / Accepted: 21 June 1999  相似文献   

Physical weathering of marbles caused by anisotropic thermal expansion   总被引：6，自引：0，他引：6  

S. Siegesmund  K. Ullemeyer  T. Weiss  E. K. Tschegg 《International Journal of Earth Sciences》2000,89(1):170-182

 Marbles as building stones as well as in their natural environments show complex weathering phenomena. The most important damage scenario is based on the highly anisotropic thermal expansion coefficient α of calcite, i.e. extreme expansion parallel and contraction normal to the crystallographic c-axis. Therefore, the rock fabric and especially the lattice-preferred orientation (texture) of calcite and/or dolomite as the predominant mineral phases in marbles have a significant influence on the mechanical weathering. The textures of marbles from five different locations vary from a more or less perfect prolate to moderate oblate shape of the [006] pole figure tensor. Accordingly, the texture-derived bulk thermal dilatation anisotropy covers a broad range from –0.048 to 0.680. The modelled thermal dilatations correlate with those obtained from experimental measurements. The difference in magnitude is basically explained by the microcrack fabrics which was not considered in the computations. All samples show a deterioration due to thermal treatment regardless of the strength of texture. The directional dependence of (a) the total magnitude of the thermal dilatation coefficient and (b) of the residual strain is highest in marbles with a strong texture, whereas the Carrara marble with a weak texture exhibits a uniform crack formation. The progressive loss of cohesion along grain boundaries due to dilatancy may serve as an example for the initial stage of physical weathering. Received: 10 February 1999 / Accepted: 16 October 1999  相似文献   

Microbial signatures in peritidal siliciclastic sediments: a catalogue   总被引：12，自引：0，他引：12  

Gisela Gerdes  Thomas Klenke  & Nora Noffke 《Sedimentology》2000,47(2):279-308

A catalogue of microbial structural signatures is presented, based upon the coupling of fundamental biogeochemical–microbial processes and local morphogenetic determinants. It summarizes a collection of sedimentary structures obtained from two modern siliciclastic peritidal environments in different climatic zones (temperate humid: Mellum Island, southern North Sea; subtropical arid: coast of southern Tunisia). Textural geometries reveal a high structural diversity, but their determinants are primarily based upon six major parameters: (1) intrinsic biofactors: structural diversification of sedimentary microbial films and mats inherent in the organisms, i.e. their construction morphology, growth, taxis and behaviour, and local abundance of specific morphotypes. Most prominent are the ensheathed filamentous cyanobacteria Microcoleus chthonoplastes and Lyngbya aestuarii, and the sheathless filamentous cyanobacterium Oscillatoria limosa. (2) Biological response to physical disturbances: sediment supply, erosion and fracturing of surface layers resulting from desiccation cause growth responses of biofilms and microbial mats. (3) Trapping/binding effects: physicobiological processes give rise to grain orientations and wavy to lenticular lamina, lamina‐specific grain arrangements and ‘sucrose’ calcium carbonate accumulations. (4) Secondary physical deformation of biogenic build‐ups: mechanical stresses acting upon sediments overgrown and biostabilized by biofilms and mats produce erosional and overthrust structures. (5) Post‐burial processes: textural fabrics that evolve from mechanical effects of gas formation from decaying mats, and features related to the formation of authigenic minerals (calcium carbonates, calcium sulphates, pyrite). (6) Bioturbation and grazing: post‐depositional structures, such as Skolithos‐type dwellings, traces of burrowing insects, gastropod grazing traces and faecal pellets. In synopsis, the catalogue firstly comprises a sound set of ubiquitous signatures. This uniformity in architectural characteristics is attributed to the presence and local dominance of certain microbes throughout the different settings. The catalogue secondly documents signatures that are extremely sensitive to tidal position, hydrodynamic regime and overall climatic conditions. These kinds of signature indicate narrow facies zones, which often coincide with the activity or dominance zones of certain organisms. An overview of structures of microbial origin from the fossil record underlines the potential of many of the signatures included in this catalogue to become fossilized and provide strong indicators of former siliciclastic tidal settings.  相似文献   

Bacteria Elimination and SO2 Filtration Using Spacer Fabric Loaded With Natural Zeolite‐Nanosilver Composites          下载免费PDF全文

Mohammad Mehdi Shirmohammadi‐Bahadoran  Majid Montazer  Mehdi Kamali Dolatabadi  Abbas Bahador 《洁净——土壤、空气、水》2018,46(9)

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鄂尔多斯盆地陇东地区延长组纵向储层质量差异及主控因素分析     

付晶  吴胜和  罗安湘  张立安  李桢  李继宏 《地学前缘》2013,20(2):98-107

综合应用多种岩心分析资料对陇东地区上三叠统延长组主力勘探目的层长8和长6油层组的岩石组构、岩石组分与储层质量差异进行了对比分析,探讨了岩石组构与岩石组分对储层质量差异的控制作用。长8末期一次显著的构造事件导致长8与长6油层组储层岩石组分和组构特征发生了明显的变化。相较于长8油层组,长6油层组粒度较细、杂基含量较高,使得原始渗透率较低,并导致更强的压实作用,使得其最终储层质量较差;塑性组分含量高,经历了较强的压实作用,原生粒间孔保存较少,并不利于后期溶蚀作用对储层进行改造;喷发岩岩屑含量低使储层早期绿泥石膜胶结相对不发育;富含白云岩岩屑为晚期含铁碳酸盐胶结物的形成提供了物质基础,使得长6油层组储层进一步致密化;长石含量高使得自生伊利石含量高,其形成的大量微孔隙导致了渗透率的大幅度降低。  相似文献   

South Australian seismicity 1967–1971     

Ian C. F. Stewart  Angela Slade  D. J. Sutton 《Australian Journal of Earth Sciences》2013,60(4):441-452

The South Australian seismograph network has been extended since 1968 so that most earthquakes of Richter magnitude ML ≥ 1.9 within the state are located accurately. Recurrence relations have been derived which define the seismicity of the known active areas. The seismic energy release has also been used to indicate the spatial variation in earthquake activity. Epicentre trends have been noted, and may be related to hypothesized movements on intracontinental plate boundaries.  相似文献