工程场地条件评定中的地脉动研究   总被引：13，自引：2，他引：13  

陶夏新  刘曾武等 《地震工程与工程振动》2001,21(4):18-23

为了研究开发更经济，更简便的场地动务特性探测方法，本文简要地回顾了工程场地条件评定中地脉动研究的演进，概述了地脉动观测技术的发展，循着地脉动分析方法的演进历程，叙述了谱和谱比分析方法，利用地脉动频散曲线反演场地速度构造的研究，讨论了各种分析方法的依据和适用条件，指出了目前存在的问题，并探讨了可能的改进途径。  相似文献   

合肥盆地周缘石炭—二叠系碎屑岩储层特征及盆内储集性预测     

王鑫 《海相油气地质》1997,2(2):39-44

合肥盆地周缘中石炭系－二叠系碎屑岩的成分成熟度和结构２成熟度较高，成岩后生作用强烈，特别是强的机械压实作用和成岩自生矿物的多期胶结作用，使其孔隙结构和储集物性变差。盆地南缘石炭系碎屑岩成岩强度更强，孔隙结构更差。碎屑岩的孔隙类型多样，以构造裂隙和次生孔隙为主，且裂隙和次生孔隙的形成呈多期性，先期形成的次生孔隙不同程度地被后期的自生矿物充填。  相似文献   

Phytogenic lacustrine sedimentation - oil shales in Neogene from Serbia, Yugoslavia     

Jelena Obradović  Jelena Djurdjević - Colson  Nebojša Vasić 《Journal of Paleolimnology》1997,18(4):351-364

Lacustrine basins of Neogene age in Serbia were formed either in intramountain valleys-graben and half-graben structures or in the marginal part of the Pannonian sea during Oligocene or at the beginning of Miocene, lasted and ended at the end of Miocene or Pliocene. The formation of the numerous depressions of the Balkan Peninsula, due to tectonic activity, gave lake basins with alluvial, swamp and lacustrine facies. The cycle with these facies was repeated several times. The lakes are mostly meromictic, often permanently stratified (oil-shale). A high rate of sedimentation with thickness up to 2000 m is characteristic for many of these basins. In many lakes phytogenic sedimentation occurs, giving facies with coal and with oil-shales. In this paper only some basins with oil-shales will be discussed, e.g. Valjevo-Mionica, Jadar and Pranjani basin. The characteristics of Vranje and Aleksinac basin will be discussed only in general. The organic rich sequences (oil shales) are characterized by the thin lamination, preservations of fish remains and plant leaves and absence of bioturbation, which needed permanent stratification of water body and anoxic conditions. Paleoclimatic regimes at the time of deposition and diagenesis were warm, subtropic with the changes of humid and dry periods.  相似文献   

Thermal stability of extended clusters in dravite: a combined EMP,SREF and FTIR study     

Ferdinando Bosi  Henrik Skogby  Tonči Balić-Žunić 《Physics and Chemistry of Minerals》2016,43(6):395-407

A dravite from Yemen of near end-member composition was treated in air and hydrogen atmospheres at 600–900 °C to reveal changes in Mg and Al order over the octahedrally coordinated Y and Z sites, and to explore related changes in the characteristic vibrational bands in the principal (OH)-stretching frequency. Relevant information was obtained using electron microprobe analysis (EMPA), structural refinement (SREF) and polarized infrared (IR) single-crystal spectroscopy. Overall, the EMPA, SREF and IR data show that only minor changes occur during thermal treatment up to at least 800 °C, including variations in structural parameters, Mg–Al order–disorder and (OH)-stretching bands, indicating limited hydrogen loss. Untreated and treated dravite samples have very similar long-range and short-range atomic structures, which may be related to the occurrence of stable Al–Mg extended clusters around the O1 (=W) and O3 (=V) sites: ^W(F)–^Y(MgMgMg)–^V(OH)₃–^Z[AlAlAlAlAl(Al,Mg)]; ^W(OH)–^Y(MgMgAl)–^V(OH)₃–^Z[AlAlAlAlAl(Al,Mg)]; ^W(O^2–)–^Y(AlAlAl)–^V(OH)₃–^Z[AlAlAlAlAl(Al,Mg)]. These extended clusters remain stable to temperatures close to the observed start of decomposition (~900 °C).  相似文献   

Micropaleontological,mineralogical, and geochemical record in late quaternary cores from abyssal Grenada Basin     

Barun K. Sen Gupta  Michel Pujos  J.- C. Pons  James J. Galluzzo  Paul Aharon  M. Parra 《Geo-Marine Letters》1991,11(1):2-8

Clay mineralogy and trace-element geochemistry of two abyssal cores indicate that the primary source of surface-current-transported detrital material in the southern Grenada Basin changed from a continental, South American terrane to a volcanic, Lesser Antillean terrane at the end of the Pleistocene. The record of benthic foraminiferal assemblages demonstrates that the Caribbean Bottom Water (CBW) was relatively oxygen poor and less corrosive in late Pleistocene glacial times than in interglacial times. The change in the properties of CBW in the Holocene was related to a renewed influx of North Atlantic Deep Water in the Caribbean.  相似文献   

胶州湾红岛码头疏浚物质输移扩散数值预测   总被引：4，自引：1，他引：4  

娄安刚  李凤歧  吴德星  袁道伟  王学昌 《海洋科学》2003,27(12):45-49

利用有限元分步杂交法，首先对胶州湾海域潮流场进行了数值模拟，进而建立了胶州湾疏浚物悬浮泥沙的二维输运——扩散模型，并应用于胶州湾红岛拟建码头疏浚区的疏浚物输运扩散数值模拟预测，根据预测结果分析了红岛码头疏浚区施工期间悬浮泥沙对附近水环境的影响。  相似文献   

Sequences Characterization of Microsatellite DNA Sequences in Pacific Abalone(Haliotis discus hannai)   总被引：1，自引：0，他引：1  

Kijima Akihiro 《中国海洋大学学报(英文版)》2007,(1)

1 Introduction Microsatellites or simple sequence repeats (SSRs) are tandemly repeated motifs of one to six bases found in all prokaryotic and eukaryotic genomes analysed to date (Zane et al., 2002). Due to their hyper-variable and co-dominant nature, relatively high abundance and random distribution in the genome, microsatellites are among the most efficient class of molecular markers. Such repeats display high polymorphism because of variation in repeat length and can be rapidly analysed t…  相似文献   

无居民海岛功能定位初探     

麻德明  丰爱平  石洪华  麻德波  刘锴 《东北测绘》2012,(3):27-29

根据无居民海岛的自然属性和社会属性,考虑到海岛环境的特殊性、资源承载的有限性、空间开发功能的衍生性,以及与国家主体功能区规划和全国海洋功能区划的衔接性,从海岛开发适宜性和海岛可持续保护的角度,研究无居民海岛功能分类方法,构建海岛功能分类评价指标体系,确定海岛功能分类的适宜性评价因子及评价标准,并引入综合评判理论,量化指标因子,构建综合评判模型,在此模型的基础上,借助GIS技术实现无居民海岛功能定位。  相似文献   

城市内部居住环境评价的空间分析——以佳木斯市为例   总被引：1，自引：0，他引：1  

顾成林  李雪铭  周健 《云南地理环境研究》2012,24(4):55-61

对城市内部居住环境质量进行定量研究是目前城市研究的热点之一。运用GIS、网格计算和空间数据自相关模型结合的方法对佳木斯市进行实证研究。利用ArcMap平台将研究区域划分成若干相同大小元胞(cell),以元胞为单位进行各种统计运算。以居住环境满意度调查问卷数据为基础建立属性数据库,并与元胞建立拓扑关系生成空间—属性一体化数据库,作为评价的基础,分别对居住环境的主要构成因子:利便环境、周边环境、文化环境进行了评价。通过空间自相关模型对评价单元之间的内在联系进行了探索性分析,发现居住环境是在空间分布形态上相应地表现出整体上的趋同性和局部的差异性。并从空间相关联的角度出发,对研究区域提出了空间布局和规划的方案。  相似文献   

山东郗山-龙宝山地区与碱性岩有关的稀土矿床地质特征及成因   总被引：1，自引：0，他引：1  

于学峰  唐好生  韩作振  李长有 《地质学报》2010,84(3):407-417

郗山和龙宝山稀土矿具有相似的成矿地质背景、控矿岩体特征及矿床地质特征。燕山早期碱性侵入岩与稀土矿关系密切,稀土矿体主要赋存于杂岩体内及其附近围岩中;稀土元素和同位素研究表明,含矿质的富碱岩浆可能属壳幔混源型,碱性岩浆及成矿物质最初可能都来源于上地幔同一部位,而在岩浆上侵过程中同化混染了地壳物质。郗山稀土矿为单一富轻稀土矿床,矿脉类型以含稀土石英重晶石碳酸盐脉为主,含稀土矿物以氟碳铈矿和氟碳钙铈矿为主,碳酸铈钠矿和菱钙锶铈矿属国内首次发现。龙宝山稀土矿为稀土、金共生矿,矿脉类型主要为石英脉和硅化角砾岩;含稀土矿物主要有氟碳铈矿、氟碳铈镧矿、氟碳钙铈矿;金矿物有自然金、银金矿等。成矿时代稍晚于岩浆岩形成时代,属中生代燕山晚期;矿床成因类型为碱性岩浆期后中-低温热液稀土矿床。  相似文献