考虑纵向帽梁作用的支护结构有限单元法     

马穗斌  杨浚炜 《江苏地质》1998,22(4):238-241

根据纵向帽梁与支护桩及支撑的约束和变形协调,提出了考虑纵向帽梁作用的支护结构的有限元解法,用于模拟基坑开挖各施工工况。采用能够替代空间结构分析的平面分析方法,既简化了计算,同时又较好地满足了工程需要。给出了计算模式,并讨论了土压力的计算、支撑弹簧系数的取值问题。  相似文献   

胜利海上埕岛油田下古生界潜山高产因素分析   总被引：1，自引：0，他引：1  

高喜龙  杨鹏飞 《海相油气地质》1998,3(4):51-56

埕岛油田是我国浅海－极海海域发现的第一个大型整流油气田,四周环凹,油源条件十分优越,全区可划分为西排山,中排山,东排山三个潜山带构造单元,油气运移通道主要是断裂和风化壳不整合面,区域盖层发育良好,储集条件是油气富集高产控制因素,纵向上潜山带储层主要集中在潜山的风化壳;平面上主要沿断层分布,沿断层发育的奥陶系在潜山是本区古生办潜山勘探的最有利目标。  相似文献   

乌石凹陷含油气远景     

苏厚熙 《海洋地质与第四纪地质》1993,13(1):65-72

乌石凹陷是北部湾盆地的一个以下第三系沉积为主的生油凹陷。主要生油层流沙港组泥页岩生油指标高、厚度大、分布面积广,具有丰富的油气源;在早第三纪已形成的四个局部构造带为有利的油气聚集场所。凹陷东部流沙港组存在高压异常,而凹陷西部存在流沙港组与涠洲组两套烃源岩。  相似文献   

Local Joint Flexibility Multibrace Tubular Joints     

Chen Tieyun Zhang Huiyuan Professor  Shanghai Jiao Tong University  Shanghai Engineer  China State Shipbuilding Corp.  Shenzhen Shipbuilding Trading Co. Ltd. 《中国海洋工程》1993,(2)

The local joint flexibility matrix of multibrace tubular joints (uniplanar and multiplanar joints) is defined. The formulation for computing the elements of local flexibility factor matrix of multibrace tubular joints by semi- analytic method is presented in this paper. The stiffening effect of unloaded braces and cross-flexibility between braces are discussed. Using the local flexibility of unibrace joints instead of that of multibrace joints in conventional structural analysis will lead the result to an unsafe side.  相似文献   

The Stress Concentration of Multiplanar Tubular Joints of Offshore Structure     

Chen Tieyun  Zhang Huiyuan Proefessor  Shanghai Jiao Tong University  Shanghai Engineer  Shenzhen Shipbuilding Trading Co. LTD  Shenzhen 《中国海洋工程》1993,(4)

- The formulation for the stress concentration matrix of multiplanar tubular joint with braces subjected to combined load is established in this paper. The formulations for SCF values of multiplanar tubular joints are compared with those by Wordsworth and Efthymiou. The stiffening effect and load-interaction effect are discussed. A spatial offshore jacket with braces subjected to combined load is computed as a numerical example. The maximum stress of each multiplanar tubular joint and its location are found through SCF matrix. Finally, the difference between the maximum stresses of multiplanar tubular joints and their corresponding uniplanar tubular joints are discussed.  相似文献   

广西昆仑关A型花岗岩地球化学特征及构造意义   总被引：12，自引：2，他引：10  

谭俊  魏俊浩  李水如  王忠铭  付乐兵  张可清 《地球科学》2008,33(6):743-754

昆仑关岩体位于广西南丹-昆仑关燕山期花岗岩带西南端, 岩石类型为黑云母花岗岩.岩相学及化学成分显示其属高钾钙碱性岩系, 具高硅、富碱和铝、低磷和钛的特点, SiO₂含量为68.13~72.61, K₂O/Na₂O比值介于1.28~1.69之间, 铝指数A/CNK=0.72~1.28, 属准铝质一强过铝质岩石.富集Ga、Rb、Th、U、Pb等元素, 而强烈亏损13a、Nb、Sr、P和Ti.稀土元素具明显负Eu异常, 总体呈现轻稀土富集的右倾"V"形配分模式.昆仑关古民单元锆石LA-ICP-MSU-Pb定年结果为93±1Ma, 形成于晚白垩世.矿物组成及地球化学特征确定了南丹-昆仑关花岗岩带是华南西南端一条重要的铝质A型花岗岩带, 控岩断裂构造为NW向南丹一昆仑关深大断裂.岩石学及主量和微量元素(含稀土)特征表明岩体侵位于后碰撞阶段的张性构造环境.结合研究范围在晚白垩世的构造背景及区域应力场匹配组合关系, 认为其与印度板块在该时期北移所引起的古太平洋板块高角度俯冲所导致的弧后拉张有关, 与浙闽沿海A型花岗岩或碱性岩分别代表了匹配构造体制下的两条A型花岗岩带.   相似文献   

Experimental Researches on Reflective and Transmitting Performances of Quarter Circular Breakwater Under Regular and Irregular Waves     

史艳娇  吴米玲  蒋学炼  李炎保 《中国海洋工程》2011,(3)

A series of regular and irregular wave experiments are conducted to study the reflective and transmitting performances of quarter circular breakwater (QCB) in comparison with those of semi-circular breakwater (SCB). Based on regular wave tests, the reflection and transmission characteristics of QCB are analyzed and a few influencing factors are investigated. Then, the wave energy dissipation as wave passing over the breakwater is discussed based on the hydraulic coefficients of QCB and SCB. In irregular wav...  相似文献   

基于熵值-理想点法的泥石流危险度研究     

刘朝安  高文龙  阙金声  陈剑平 《吉林大学学报(地球科学版)》2011,(Z1):201-206,226

泥石流危险度的划分是泥石流研究中的重点与难点,泥石流危险度的确定对于泥石流整体特征的把握具有十分重要的作用。采用熵值-理想点法建立了泥石流危险度划分模型,选取流域面积、主沟长度与泥石流沟相对最大高差等10个评价指标。利用现场3条泥石流沟作为工程评价对象,通过熵值法确定各评价指标的权重系数,并采用理想点法进行泥石流危险度的划分研究。根据模型分析结果,泥石流沟2与3属于高危险度(贴近度为0.79与0.83),泥石流沟1属于中危险度(贴近度为0.82)。泥石流危险度与现场情况及已有研究资料基本一致,证明了该法在泥石流危险度划分中的合理性与有效性。  相似文献   

宁东鸳鸯湖矿区梅花井煤矿112201工作面探放水实践     

李喆 《中国煤炭地质》2011,(11):41-43

112201工作面是梅花井煤矿首采工作面,位于矿井南端浅部,切眼靠近鸳鸯湖背斜轴部。工作面涌水量从2009年4月份开始回采时的15m3/h,增至2010年3月份的230m3/h。工作面的突然涌水导致大量淋水,从而使采区底板严重泥化,给矿井安全生产带来巨大威胁。分析认为,工作面的主要充水水源为2-1煤的顶板含水层（七里镇砂岩）,主要通道为顶板的采动裂隙带。通过实施探放水和疏放水工程,工作面下隅角的涌水量由180m3/h降至30m3/h以内,极大的减少了含水层突然涌水对工作面的危害,为梅花井乃至鸳鸯湖矿区防治水工作起到了积极作用。  相似文献   

Acoustic evidence of shallow gas accumulations and active pockmarks in the ?zmir Gulf, Aegean sea     

Derman Dondurur  Günay ÇifçiMahmut Göktu? Drahor  Süleyman Co?kun 《Marine and Petroleum Geology》2011,28(8):1505-1516

Based on high-resolution Chirp seismic, multibeam bathymetry and side scan sonar data collected in the ?zmir Gulf, Aegean Sea in 2008 and 2010, gas-related structures have been identified, which can be classified into three categories: (1) shallow gas accumulations and gas chimneys, (2) mud diapirs, and (3) active and inactive pockmarks. On the Chirp profiles, shallow gas accumulations were observed along the northern coastline of the outer ?zmir Gulf at 3-20 m below the seabed. They appear as acoustic turbidity zones and are interpreted as biogenic gas accumulations produced in organic-rich highstand fan sediments from the Gediz River. The diapiric structures are interpreted as shale or mud diapirs formed under lateral compression due to regional counter-clockwise rotation of Anatolian microplate. Furthermore, the sedimentary structure at the flanks suggests a continuous upward movement of the diapirs. Several pockmarks exist close to fault traces to the east of Hekim Island; most of them were associated with acoustic plumes indicating active degassing during the survey period in 2008. Another Chirp survey was carried out just over these plumes in 2010 to demonstrate if the gas seeps were still active. The surveys indicate that the gas seep is an ongoing process in the gulf. Based on the Chirp data, we proposed that the pockmark formation in the area can be explained by protracted seep model, whereby sediment erosion and re-distribution along pockmark walls result from ongoing (or long lasting) seepage of fluids over long periods of time. The existence of inactive pockmarks in the vicinity, however, implies that gas seepage may eventually cease or that it is periodic. Most of the active pockmarks are located over the fault planes, likely indicating that the gas seepage is controlled by active faulting.  相似文献