广西南部钦州地区早—中三叠世火山事件——台马碎斑熔岩   总被引：1，自引：0，他引：1  

杨丽贞  刘融涛  白艳萍 《地质通报》2011,30(1):95-100

通过对前人划分的十万大山岩带的主要岩体——台马岩体的野外地质特征、岩石学特征的研究,认为原台马岩体主要由碎斑熔岩组成,是火山侵出相的产物而不是侵入相的花岗斑岩。结合台马碎斑熔岩与周边火山岩、侵入岩、地层的关系,认为它是早—中三叠世中心裂隙式火山构造中央部位侵出的穹状岩脊。因此,十万大山岩带是火山-侵入杂岩带,台马碎斑熔岩是该火山-侵入杂岩带的一个相。  相似文献   

极化大地复电阻率正反演   总被引：3，自引：0，他引：3  

李勇  林品荣  郑采君  李桐林  王有学  孟庆奎 《吉林大学学报(地球科学版)》2011,(Z1):355-361,373

论述了层状极化大地复电阻率正、反演算法。给出了层状极化大地条件下三极和对称四极装置视复电阻率的解析表达式,并引入线性滤波方法实现表达式的求解。正演算例计算结果表明;随着频率的降低,复电阻率相位峰值增大;随着极化层层厚增加,复电阻率虚部平缓变化后连续递增。介绍了递推反演算法的实现过程,从理论模型试算结果看,测深曲线较好地反映了极化层Cole-Cole参数随深度的变化规律,其曲线的首支和尾支趋近于极化层的真Cole-Cole参数,表明了反演计算的可行性。  相似文献   

Stratigraphic evolution of a submarine channel-lobe complex system in a narrow fairway within the Magallanes foreland basin, Cerro Toro Formation, southern Chile     

Anne Bernhardt  Zane R. JobeDonald R. Lowe 《Marine and Petroleum Geology》2011,28(3):785-806

This study integrates newly acquired stratigraphic data, geologic mapping, and paleocurrent data to constrain the stratigraphic evolution of the oldest channel-lobe complex in the Upper Cretaceous Cerro Toro Formation in the Silla Syncline area of the Magallanes Basin, termed the Pehoe member. The Pehoe member ranges in thickness from 60 m in the north to at least 410 m farther down system and comprises three separate divisions (A, B, and C). A lower conglomerate unit and an upper one, termed Pehoe A and C divisions respectively, represent the fill of major incised submarine channels or channel complexes. These are separated by stratified sandstone of the Pehoe B division, representing a weakly confined lobe complex, either transient or terminal.The integration of new data with observations from previous studies reveal that the three main coarse-grained conglomerate and sandstone members in the Cerro Toro Formation in the Silla Syncline include at least seven distinct submarine channels or channel complexes and two major lobe complexes. The thinning and disappearance of these units along the eastern limb of the syncline reflect confinement of the flows to a narrow trough or mini-basin bounded to the east by a topographic high. This confinement resulted in unidirectional paleocurrents to the south and southeast in all deposits. Changes in depositional geometries are interpreted as reflecting changes in sediment supply and relative confinement. Submarine channels were from 700 m to 3.5 km wide and occupied a fairway that was 4-5 km wide. Flows moving south and southeast in this mini-basin probably crossed the eastern topographic high south of the present exposures and joined those moving southward along the axis of the foreland basin at least 16 km to the east.  相似文献   

Modeling regional sediment transport and shoreline response in the vicinity of tidal inlets on the Long Island coast,United States     

Le Xuan Hoan  Hans Hanson  Magnus Larson  Pham Thanh Nam 《Coastal Engineering》2011

A new numerical model was developed to simulate regional sediment transport and shoreline response in the vicinity of tidal inlets based on the one-line theory combined with the reservoir analogy approach for volumetric evolution of inlet shoals. Sand bypassing onshore and sheltering effects on wave action from the inlet bar and shoals were taken into account. The model was applied to unique field data from the south coast of Long Island, United States, including inlet opening and closure. The simulation area extended from Montauk Point to Fire Island Inlet, including Shinnecock and Moriches Inlets. A 20-year long time series of hindcast wave data at three stations along the coast were used as input data to the model. The capacity of the inlet shoals and bars to store sand was estimated based on measured cross-sectional areas of the inlets as well as on comprehensive bathymetric surveys of the areas around the inlet. Several types of sediment sources and sinks were represented, including beach fills, groin systems, jetty blocking, inlet bypassing, and flood shoal and ebb shoal feeding. The model simulations were validated against annual net longshore transport rates reported in the literature, measured shorelines, and recorded sediment volumes in the flood and ebb shoal complexes. Overall, the model simulations were in good agreement with the measured data.  相似文献   

复指数方法降噪技术及其试验研究     

包兴先  刘福顺  李华军  高志强 《中国海洋大学学报(自然科学版)》2011,(Z1):155-160,164

实测信号中的噪声,以及模型阶次的不确定性给模态参数的准确识别带来困难。以提高模态参数识别精度为目标,提出基于模型定阶和信噪分离的复指数模态参数识别方法。该方法借助奇异值分解技术确定模型阶次,采用结构低秩逼近方法进行信噪分离。在此基础上,利用复指数法进行模态参数识别。分别选取一维的悬臂梁模型和二维的悬挂板模型进行物理模型实验,结果表明:该方法提高模态参数的识别精度,尤其是阻尼比的识别精度,具有较好的工程应用前景。  相似文献   

The ultrastructure of the spermatozoon of Octopus ocellatus Gray, 1849 (Cephalopoda: Octopoda)     

杨建敏  王卫军  郑小东  周全利  张宇  孙国华  刘相全 《中国海洋湖沼学报》2011,29(1):199-205

Morphology of the spermatozoon of Octopus ocellatus was studied by light, scanning electron, and transmission electron microscopes. Sperm are 600–700 μm long, with a large number of granules in diameter about 130 nm. Each spermatozoon is composed of a head, neck, and tail. The head is made up of an acrosomal complex anterior to the nucleus. The spiral acrosomal complex consists of an electron-lucent vesicle, lacuna, and an electron-dense acrosomal vesicle. Additionally, the spiral acrosomal vesicle has numerous equidistant striations, and is surrounded by many small granules (20 nm diameter). A long straight nucleus, which is electron-densed, has a deep posterior concavity, the nuclear vacuole. At the terminal end of the nucleus is a sleeve-like structure with a concave posterior nuclear fossa (PNF). The neck is short connecting the PNF. The basal body is located in the PNF and gives rise to the axoneme. This structure connects the head, neck, and tail. The tail is divided into a middle piece and a principal piece. The middle piece, having a 9+9+2 arrangement, is surrounded by a mitochondrial sheath and terminates by an electron-dense fibrous sheath. The principal piece is the longest part of the sperm with coarse fibers tapering posteriorly. The results of this study shall provide some useful information for artificial breeding of this species.  相似文献   

Knowledge co-production for Indigenous adaptation pathways: Transform post-colonial articulation complexes to empower local decision-making     

《Global Environmental Change》2020

Co-production between scientific and Indigenous knowledge has been identified as useful to generating adaptation pathways with Indigenous peoples, who are attached to their traditional lands and thus highly exposed to the impacts of climate change. However, ignoring the complex and contested histories of nation-state colonisation can result in naïve adaptation plans that increase vulnerability. Here, through a case study in central Australia, we investigate the conditions under which co-production between scientific and Indigenous knowledge can support climate change adaptation pathways among place-attached Indigenous communities. A research team including scientists, Ltyentye Apurte Rangers and other staff from the Central Land Council first undertook activities to co-produce climate change presentations in the local Arrernte language; enable community members to identify potential adaptation actions; and implement one action, erosion control. Second, we reflected on the outcomes of these activities in order to unpack deeper influences. Applying the theory of articulation complexes, we show how ideologies, institutions and economies have linked Indigenous societies and the establishing Australian nation-state since colonisation. The sequence of complexes characterised as frontier, mission, pastoral, land-rights, community-development and re-centralisation, which is current, have both enabled and constrained adaptation options. We found knowledge co-production generates adaptation pathways when: (1) effective methods for knowledge co-production are used, based on deeply respectful partnerships, cultural governance and working together through five co-production tasks—prepare, communicate, discuss, bring together and apply; (2) Indigenous people have ongoing connection to their traditional territories to maintain their Indigenous knowledge; (3) the relationship between the Indigenous people and the nation-state empowers local decision-making and learning, which requires and creates consent, trust, accountability, reciprocity, and resurgence of Indigenous culture, knowledge and practices. These conditions foster the emergence of articulation complexes that enable the necessary transformative change from the colonial legacies. Both these conditions and our approach are likely to be relevant for place-attached Indigenous peoples across the globe in generating climate adaptation pathways.  相似文献   

青藏高原零度层亮带的识别订正方法及在雷达估测降水中的应用   总被引：7，自引：2，他引：5  

庄薇  刘黎平  胡志群 《气象》2013,39(8):1004-1013

零度层亮带是指雪花或冰晶降落到零度层附近,表面发生融化而使雷达反射率突然增大的现象.它是影响雷达资料质量的重要因素,常会导致雷达估测降水的高估.青藏高原海拔高、零度层低,零度层以下的降水范围非常有限,亮带对青藏高原地区的雷达估测降水的影响更加显著.因此,对亮带进行自动识别订正,对提高青藏高原雷达降水估测的精度有重要意义.本文在考虑青藏高原遮挡严重的情况下,通过计算反射率垂直廓线来识别零度层亮带,对亮带区域进行订正,并将亮带订正前后的混合扫描反射率分别估测降水,分析亮带订正对降水估测误差的影响.结果表明:雷达识别的亮带高度在探空资料零度层以下几百米内;亮带订正前,反射率垂直廓线在零度层附近有显著弯曲,雷达对降水的估测明显偏高;亮带订正后,反射率垂直廓线在零度层附近的显著弯曲消失,雷达估测的降水量与雨量计的观测值较一致,降水估测误差比订正前明显减小.  相似文献   

闽东北木拱廊桥建筑群地理空间响应研究     

张光英 《亚热带资源与环境学报》2011,6(2):83-88

闽东北木拱廊桥建筑群是一个独特的地理建筑,很好的诠释了建筑与自然环境的关系,体现了建筑与周围的自然和人文环境同存共息关系.闽东北木拱廊桥建筑在技术应用上,结合人文的、生态的、经济的、地区的等进行不同程度的革新,推动新的桥梁建筑艺术的创造,是特殊自然条件的建筑拓展空间、延伸空间的典型.闽东北木拱廊桥建筑群在闽东北得以出现...  相似文献   

基于CPLD的高精度可调脉冲信号发生器研制   总被引：1，自引：0，他引：1  

樊多盛  施韶华  李孝辉 《时间频率学报》2014,(1):25-33

为满足精密时间间隔测量设备的测试需要,研制了一种时间间隔可调的高精度脉冲信号发生器。利用计算机串口控制的方式,结合复杂可编程逻辑器件（CPLD）集成度高、可靠性好及工作速度快的优点,采用A1tera公司的设计软件QuartusII进行设计仿真及实现。仿真与实测实验表明,该脉冲信号发生器不仅可以产生单路可调脉冲信号,而且能产生多路可调脉冲信号,产生的单路秒脉冲信号的1s取样Allan方差为1．84×10^-11;产生的时间间隔为100ns的多路脉冲信号的1s取样Allan方差为2．36×10^-11,2路信号之间的时间间隔数据系列的峰一峰值为101ps,可以满足多通道时间间隔测量设备测试要求的稳定度与准确度。  相似文献