宝鸡石油机械厂34#高层住宅楼工程降水方案设计     

高清苗  侯利军  梁秀娟  王建勋 《陕西地质》2007,35(1):51-58

根据拟建场地的地层结构及地下水条件,结合周边环境和基坑支护、降水要求,确定合理的降水模型及基本设计计算参数,进行降水井设计计算。本设计采用管井方案,设计中最重要的是确定管井数量,先预设一个滤水管进水部分长度,计算出管井数量,然后进行反算、验算,遵循技术可行、节约费用的原则,最终确定出合理的井点数量。降水井投入使用后,基坑内侧的少量渗水,运用集水明排的方法排泄,取得了良好的效果。管井与集水明排相结合进行降水的方法在宝鸡市区得到了广泛应用。  相似文献   

Orogenic Gold Mineralization in the Qolqoleh Deposit, Northwestern Iran   总被引：1，自引：1，他引：1  

Farhang Aliyari    Ebrahim Rastad  Hou Zengqian 《Resource Geology》2007,57(3):269-282

The Qolqoleh gold deposit is located in the northwestern part of the Sanandai‐Sirjan Zone, northwest of Iran. Gold mineralization in the Qolqoleh deposit is almost entirely confined to a series of steeply dipping ductile–brittle shear zones generated during Late Cretaceous–Tertiary continental collision between the Afro‐Arabian and the Iranian microcontinent. The host rocks are Mesozoic volcano‐sedimentary sequences consisting of felsic to mafic metavolcanics, which are metamorphosed to greenschist facies, sericite and chlorite schists. The gold orebodies were found within strong ductile deformation to late brittle deformation. Ore‐controlling structure is NE–SW‐trending oblique thrust with vergence toward south ductile–brittle shear zone. The highly strained host rocks show a combination of mylonitic and cataclastic microstructures, including crystal–plastic deformation and grain size reduction by recrystalization of quartz and mica. The gold orebodies are composed of Au‐bearing highly deformed and altered mylonitic host rocks and cross‐cutting Au‐ and sulfide‐bearing quartz veins. Approximately half of the mineralization is in the form of dissemination in the mylonite and the remainder was clearly emplaced as a result of brittle deformation in quartz–sulfide microfractures, microveins and veins. Only low volumes of gold concentration was introduced during ductile deformation, whereas, during the evident brittle deformation phase, competence contrasts allowed fracturing to focus on the quartz–sericite domain boundaries of the mylonitic foliation, thus permitting the introduction of auriferous fluid to create disseminated and cross‐cutting Au‐quartz veins. According to mineral assemblages and alteration intensity, hydrothermal alteration could be divided into three zones: silicification and sulfidation zone (major ore body); sericite and carbonate alteration zone; and sericite–chlorite alteration zone that may be taken to imply wall‐rock interaction with near neutral fluids (pH 5–6). Silicified and sulfide alteration zone is observed in the inner parts of alteration zones. High gold grades belong to silicified highly deformed mylonitic and ultramylonitic domains and silicified sulfide‐bearing microveins. Based on paragenetic relationships, three main stages of mineralization are recognized in the Qolqoleh gold deposit. Stage I encompasses deposition of large volumes of milky quartz and pyrite. Stage II includes gray and buck quartz, pyrite and minor calcite, sphalerite, subordinate chalcopyrite and gold ores. Stage III consists of comb quartz and calcite, magnetite, sphalerite, chalcopyrite, arsenopyrite, pyrrhotite and gold ores. Studies on regional geology, ore geology and ore‐forming stages have proved that the Qolqoleh deposit was formed in the compression–extension stage during the Late Cretaceous–Tertiary continental collision in a ductile–brittle shear zone, and is characterized by orogenic gold deposits.  相似文献   

渤海小高压的形成机制分析     

侯淑梅  孙忠欣  张承旺 《山东气象》2007,27(4):10-13

对2006年7月3日一次典型的渤海小高压与切变线相互作用的天气过程进行了分析，初步探讨了渤海小高压的形成机制。渤海小高压是由于渤海特殊的地理位置造成的，它与南北支系统的相互作用、中低纬切变线的位置、日本海低涡中横槽的位置密切相关。渤海小高压的形成与其高低空的动力、热力条件关系密切，当华北到渤海地区没有明显的低空辐合和高空辐散，并受明显的干区、正的沙氏指数区、能量低值区控制时，容易形成渤海小高压。  相似文献   

东营市秋冬季大雾天气分析     

张承旺  侯淑梅  孙忠欣 《山东气象》2007,27(4):24-26

利用1971-2000年东营市及所辖3个县站的资料分析了地处黄河入海口的东营市大雾天气气候特征，结果表明：每年11月到次年的1月，是一年中大雾出现最岁的月份，广饶县大雾出现得最多，平均每年大雾日有22．7天。针对2006年9月20-23日连续大雾天气，分析了其高、低空环流形势，在此基础上总结了东营秋冬季大雾的预报着眼点。对于连续性大雾的第一天预报，需要湿度条件、辐射降温条件、风力条件均有利时才易出现大雾，而对于连续性的大雾，对辐射降温条件要求不高。  相似文献   

2014年云南景谷6.6级地震序列震源参数研究          下载免费PDF全文

周少辉  蒋海昆  曲均浩  郑旭  郭宗斌  李亚军  张志慧 《地震工程学报》2020,42(6):1565-1572

利用290个M_L ≥ 2.5的景谷6.6级地震序列事件的数字波形资料，计算得到其震源参数。结果显示，地震矩M₀数值范围为10¹²~10¹⁶ N·m；拐角频率f_c为3~16 Hz；视应力数值范围为0~15 MPa，平均值是2.14 MPa，中位数为1.39 MPa。同时，各个震源参数之间均存在一定的相关关系；景谷地震序列余震空间分布可分为北段、中段与南段，其视应力高低分布依次为：南段 > 中段 > 北段；表明主震发生后，震源区南段区域的应力水平最高，这可能是后续5.8级\，5.9级强余震均发生在南段的根本原因。在视应力时间变化特征方面，5.8级、5.9级强余震的发生前，震中所在的南段视应力数值存在"逐渐变大-维持稳定"的特点。而后续未发生强余震的北段和中段，其视应力时间变化为早期快速调整，后续逐渐变化到各自区域的视应力均值水平；这类变化表明对于震源区南段，在强余震发生前的短时间内，南段区域首先出现局部应力不断挤压增强，并随后维持相对高值应力水平的"闭锁"状态，直到强余震的发生。因而，震后震源区余震视应力的空间分布对强余震可能产生地点判定有指示作用，其时间变化特征与地震序列中较强地震的发生存在一定的相关性。余震视应力的时空变化对序列后续地震活动的判定有重要指示作用，可为强余震的时空判定提供相应参考。  相似文献   

Impedance characteristics of carbon steel under cathodic protection   总被引：1，自引：0，他引：1  

李言涛  侯保荣 《中国海洋湖沼学报》1998,16(1):60-63

INTRODUCTIONInpraCticalengineeringapplicati0ns,thecormsionofstalundercathodicprotalioncanbecontr0llediftheproodi0np0tenhalisset2O()t03(X)mVnegativewithaspeCttothenatamlcormsi0np0tenial(MasatSugi,l976,Takehiko,l972).Theprotalnp0tentia1edinpraedcalapplicationisbedonexperienceandtheory.Tooru(l985,l986)foundthattheopbocathodicproodionpotentialcoinddedwiththepotentialwhenpolarhati0nresistancemaxndnd,s0thiscoinedencecanbeedt00btainoptbore-sultforcarbonstalundercathodicpronaion.Inthiswork,the…  相似文献   

Identification and sequence of a cDNA clone corresponding to a gene involved in development ofUndaria pinnatifida     

He-shen  Hou  Ning  Li  Chao-yuan  Wu 《中国海洋湖沼学报》1998,16(1):25-29

During the induction of gamete-producing gametangia, induced gametophytes were collected at 4 days intervals (0,4,8,12 d) and total RNAs were isolated by CsCl gradient ultracentrifugation. Some stage-specific expressed mRNAs were identified by differential display of mRNAs from different developing stages of the gametophytes. The cDNA of one specific mRNA was verified, cloned and sequenced. This gene was specifically expressed during 4 days of induction, and had partial homologous sequence with tobacco IAA-binding protein gene. It suggests that this cDNA may represent a gene which is related to the IAA regulating function during the development of the gametophytes.

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教师在数字化测图教学实践中的主导作用     

侯建国  李金平 《测绘工程》1998,7(4):70-74

介绍在数字化测图实践中,各关键技术环节上教师的主导作用,总结了实践教学的经验和体会。  相似文献   

西昆仑库地西北依沙克群中首次发现放射虫化石   总被引：1，自引：1，他引：0       下载免费PDF全文

方爱民  李继壳 《地质科学》1998,33(3):384-384

新藏公路137km处一些克沟中自下而上发育一套由基性火山岩、火山碎屑岩及深海复理石组成的库地蛇绿岩系。  相似文献   

右江盆地三叠纪岩层极低级变质作用及地球动力学意义   总被引：16，自引：1，他引：15       下载免费PDF全文

索书田  毕先梅  赵文霞  侯光久 《地质科学》1998,(4):395

 右江盆地三叠纪槽盆相浊流沉积岩系遭受过区域极低级变质作用。依据地质观察和伊利石结晶度、绿泥石-云母堆垛集合体、标志性粘土矿物及白云母(伊利石)b0参数测定资料,阐述了泥质岩石的成岩变质作用经浅层(近)变质作用到浅变质作用的转换特征。变质温度区间为150-350℃,低压类型,具高地温梯度(40-43℃/km).变质级及亚带总体与地层时代及岩层在地层柱中的位置有耦合关系,而与区域变形强度无关。最后指出区域极低级变质作用是印支-燕山构造旋回早期及区域变形前的地质事件,属于地壳伸展构造背景下右江边缘型盆地内部的埋藏型变质作用。  相似文献