甘孜－理塘结合带甘孜地区混杂岩类型及成因分析   总被引：1，自引：0，他引：1  

江元生 《四川地质学报》1996,(3)

对甘孜－理塘结合带甘孜地区的沉积混杂、火山混杂、构造混杂岩作了系统分析研究。重点论述了甘孜地区三条构造混杂岩带的物质组成、变形特征和形成机制。结合带是由大小不等，形态各异的岩块（片）拼贴、堆叠而成的构造混杂岩带。较合理地解释了结合带内，大洋拉斑玄武岩、洋岛玄武岩、大陆碱性玄武岩共存的地质特征。提出了一种新的构造岩石单位——构造混杂岩。并对甘孜地区蛇绿岩的成因作了探讨。  相似文献   

Affordance-based categorization of road network data using a grounded theory of channel networks     

Simon Scheider  Werner Kuhn 《International journal of geographical information science》2013,27(8):1249-1267

We propose a grounded ontological theory of channel networks to categorize features, such as junctions, in road network databases. The theory is grounded, because its primitives can be given an unambiguous interpretation into directly observable qualities of physical road networks, such as supported movements and their medium, connectedness of such media, and turnoff restrictions. The theory provides a very general approach to automatically annotate and integrate road network data from heterogeneous sources, because it rests on application-independent observation principles. We suggest that road network categories such as junctions and roads are based on locomotion affordances. Road network databases can be mapped into our channel network theory, so that instances of roads and junctions can be automatically categorized or checked for consistency by what they afford. In this paper, we introduce affordance-based definitions of a road network and a junction, and show that the definition of latter is satisfied by some of the most common junction types.  相似文献   

Cenozoic tectonic evolution of the central Wassuk Range,western Nevada,USA     

《International Geology Review》2012,54(5):547-571

The central Wassuk Range is ideally located to investigate the interplay of Basin and Range extension and Walker Lane dextral deformation along the western Nevada margin of the Basin and Range province. To elucidate the Cenozoic evolution of the range, the author conducted geologic mapping, structural data collection and analysis, geochemical analysis of igneous lithologies, and geochronology. This research delineates a three-stage deformational history for the range. A pulse of ENE–WSW-directed extension at high strain rates (～8.7 mm/yr) was initiated immediately after the eruption of ～15 Ma andesite flows; strain was accommodated by high-angle, closely spaced (1–2 km), east-dipping normal faults which rotated and remained active to low angles as extension continued. A post-12 Ma period of extension at low strain rates produced a second generation of normal faults and two prominent dextral strike–slip faults which strike NW, subparallel to the dextral faults of the Walker Lane at this latitude. A new pulse of ongoing extension began at ～4 Ma and has been accomodated primarily by the east-dipping range-bounding normal fault system. The increase in the rate of fault displacement has resulted in impressive topographic relief on the east flank of the range, and kinematic indicators support a shift in extension direction from ENE–WSW during the highest rates of Miocene extension to WNW–ESE today. The total extension accommodated across the central Wassuk Range since the middle Miocene is >200%, with only a brief period of dextral fault activity during the late Miocene. Data presented here suggest a local geologic evolution intimately connected to regional tectonics, from intra-arc extension in the middle Miocene, to late Miocene dextral deformation associated with the northward growth of the San Andreas Fault, to a Pliocene pulse of extension and magmatism likely influenced by both the northward passage of the Mendocino triple junction and possible delamination of the southern Sierra Nevada crustal root.  相似文献   

秦昆结合部塔秀地区隆务河组碎屑锆石LA-ICP-MSU-Pb年代学及其地质意义     

路宗悦  余心起  刘满年  张振  魏立勇  赵常存  郑鑫  寇少磊  许安民  王照翻 《现代地质》2019,33(4):691-702

秦昆结合部独特的地质组成与复杂的造山带结构受到广泛关注。前人对该地区沉积物质来源进行了初步分析,但存在较大争议。选取隆务河组碎屑岩为研究对象,运用碎屑锆石LA-ICP-MS U-Pb同位素年代学方法,探讨隆务河组物源特征。U-Pb测年结果表明,隆务河组碎屑锆石年龄谱明显分为4组:2 746~2 084 Ma,1 094~775 Ma,492~411 Ma,372~237 Ma。其中,372~237 Ma年龄组约占总体的56.79%,所占比例最大,年龄相对集中,且呈现出强烈的峰值,代表了阿尼玛卿洋向北俯冲碰撞产生的一系列构造岩浆事件,其余年龄段所占比例则较少。综合分析显示,隆务河组碎屑沉积物质来源较为复杂,具有明显的多元性,存在祁连造山带、柴北缘构造带和东昆仑造山带3个物源区,其中东昆仑造山带提供了大部分物源,为隆务河组贡献最大的物源区。  相似文献   

交叉点结构特征约束的机载LiDAR点云与多视角航空影像配准     

王广帅  万一  张永军 《地球信息科学学报》2020,22(9):1868-1877

针对机载点云与航空影像配准精度受点云密度影响较大的问题,本文提出一种交叉点结构特征约束下的机载点云影像配准方法。该方法充分利用激光测距精度较高这一优势,采用点云中的平面结构对影像区域网进行绝对定向约束。首先,利用POS辅助平差后的影像内外方位元素和影像交叉点结构匹配结果,以反投影距离为测度,按照最小二乘准则交会得到交叉点物方结构;然后,在LiDAR点云中自动探测交叉点结构的同名LiDAR平面点;最后,进行交叉点结构特征约束下的航空影像联合区域网平差,得到精确的相机内参数和影像外方位元素。实验结果表明,本文方法在平面和高程方向上均可达到1~2个像素的配准精度。与基于建筑物角特征的配准方法相比,有效克服了点云密度对配准精度的影响,当点云密度较低时,本文方法依然可以取得较高的配准精度。  相似文献   

豫鲁冀交界区S波分裂变化特征     

何重阳  邢康  郑培玲  郭少峰  卞龙  韩贞辉 《地震地磁观测与研究》2019,40(2):21-27

选取豫鲁冀交界区17个数字化测震台站S波记录,对该区地震进行限定筛选,并对台站记录的地震波形进行严格仔细的参数测量与提取,分析地震波传播过程中S波分裂变化及与地震的关系,提取中等地震前S波分裂所表现的地球物理异常特征。  相似文献   

西构造结—帕米尔及周边深部结构与构造探榷          下载免费PDF全文

王谦身  滕吉文  陈石  文武  张永谦  徐伟民 《地球物理学报》2020,63(8):2970-2977

帕米尔高原是五大山脉汇结之中心,被称为"西构造结".在此山高耸谷陡深是人迹罕至的无人区.应用稀少的地面重力和人工地震数据和卫星重力资料,以NNW和NEE向两条长达1620 km的十字交叉剖面,对帕米尔高原地区地壳深部结构与区域地质构造进行了研讨.帕米尔高原中心地区地壳厚度(莫霍界面深度)接近70 km,并在总体上呈向四周逐渐延展减薄(变浅)的总趋势,到帕米尔的周边地区减薄为50余km左右.这里是一个壳幔结构变异的构造强烈活动地域.  相似文献   

潮汐汊口水流结构和动力特性研究     

吴尧  张蔚  何用  卢陈  吴门伍 《海洋通报》2019,38(2):186-193

潮汐汊口作为河网的重要单元,关系到水沙以及可溶污染物、营养物质的输运和分配,对河口三角洲的水文过程、地貌沉积和生态环境,都有至关重要的影响。本文选取国内最大的珠江河网的分汊顶点-马口、三水分汊,基于一个大潮潮周期内走航ADCP测量,分析潮汐汊口各个支汊的流速过程及三维流速的时空分布特征;结合非稳态的调和分析算法和小波连续变换确定汊口处主要的潮汐组分,利用潮流分离技术,剥离出占主导作用的潮波信号并探讨潮波动力在潮汐汊口处的空间分布形态。研究发现,由于潮波在西江马口和北江三水汊道内传播的不对称性,两汊间的流速过程存在1.5 h左右的相位差。而连接西北江的岗根汊道,由于存在频繁的水体交换和弯道水流的特性,岗根断面的动力作用较为复杂,其最大垂向平均流速在涨落急时刻分别向左、右岸偏移,横向断面均出现了显著的顺时针二次流。  相似文献   

皖西白大山群的发现及其地质意义   总被引：7，自引：0，他引：7  

毕治国  李玉发  汤加富  侯明金 《安徽地质》1994,(Z1)

皖、豫交界的白大山－茶庵一带，出露一套碎屑岩夹碳酸盐岩地层，以往被置于青白口系八公山群。近期笔者等赴该地再次进行了调查和研究，结果发现该群地层组合内含有大量球藻类和植物碎片化石，这些微古植物分子在国内外多见于下古生代。并从岩石组合特征对比分析，认为该套地层属志留－泥盆系的可能性最大。对这套地层及微古植物的发现，具有两方面重要的地质意义：１．过去对华北地台南缘从未见有这个时代地层的报导，这就为该区地层填补了一个空白；２．从已采获的微古植物组合及岩性组合特征等分析，这有可能对华北地台南缘的岩相古地理图及地史发展等问题，进行一些必要的改写与补充。  相似文献   

硅的间接跃迁双光子吸收系数谱     

崔昊杨  李志锋  马法君  陈效双  陆卫 《海洋学报》2010,32(10):7055-7059

利用皮秒Nd:YAG脉冲激光器作为激发光源,测量出光子能量介于1.36 μm (0.912 eV)—1.80 μm (0.689 eV)之间的硅间接跃迁双光子吸收系数谱.尽管此波段范围内的激光光子能量小于硅间接带隙,但当激光辐照在硅基光电二极管受光面时,在二极管两电极端仍然探测到了显著的脉冲光伏信号.光伏信号峰值强度与入射光强呈二次幂函数关系,表明其是双光子吸收过程.采用pn结等效结电容充放电模型,将光伏响应信号峰值与入射光强相关联,从中提取出硅的间接跃迁双光子吸收系数,改变入射波长得到系数谱.研究表明:  相似文献