The geological characteristics of oceanic-type UHP metamorphic belts and their tectonic implications: Case studies from Southwest Tianshan and North Qaidam in NW China

The geological characteristics of ultrahigh-pressure （UHP） metamorphic belts formed by deep subduction of oceanic crust are summarized in this paper. Oceanic-type UHP metamorphic belt is characterized by its protolithlc assemblage of typical oceanic crust, the peak metamorphic temperature 〈600℃, P-T path undergoing blueschist facies during prograde and retrograde metamorphic evolution, reepectively, with low geothermal gradient of cold subduction. The further study of oceanic-type UHP metamorphic belt is very significant for constructing metamorphic reaction series of cold subduction zone, for understanding how aqueous fluids were transported into deep mantle and for classifying the types of UHP metamorphism in cold subduction zone. The uplift and exhumation mechanism of oceanic UHP metamorphic rocks is one of the most challenging problems in the study of UHP metamorphism, which is very important for understanding the geodynamic mechanism of solid Earth. As a traveler eubducted into the mantle depth end then uplifted to the surface, oceanic-type UHP metamorphic belts witness the bulk process from the subduction to exhumation and is an ideal target to study the geochemical behavior end cycling of elements in subduction zones. The tectonic evolution of one convergent orogenic belt can be usually divided into two stages of oceanic subduction and followed continental subduction and collision, and the two best-established examples of orogenic belts are Alpa and Himalaya. Therefore, the study of oceanic-type UHP metamorphic belt is the frontier of the current plate tectonic theory. As two case studies, the current status and existing problems of oceanic-type UHP metamorphic belts in Southwest Tianshan and North Qaidam, NW China, are reviewed in this paper.     

苏丹国穆格莱德盆地构造特征及演化

用盆地分析的方法确定了穆格莱德盆地的原型为伸展断陷盆地.由于改造状况不同,出现3种类型:第一类是未受改造的伸展断陷盆地,第二类是挤压反转的伸展断陷盆地,第三类是走滑改造的伸展断陷盆地.盆地内半地堑、半地垒不对称地交替变化是通过调节带调节其变形或位移,该盆地调节带有6种类型,其构造样式为地垒状凸起、鼻状构造和走向斜坡,具有纵向、横向和斜向3种走向.盆地构造演化有3期:(1)早白垩世早期,随着非洲-南美泛大陆裂开,产生了第一期伸展断陷盆地;(2)早白垩世晚期到晚白垩世,随着原始大西洋的扩张,形成了第二期伸展断陷盆地;(3)新生代,随着区域沉降,演化为伸展坳陷盆地.油气储量主要分布在第二期伸展断陷盆地,油气具有跨时代聚集、高产富集的特点.     

潮间带菌株CZⅣ-1068的鉴定及抑菌活性研究

CZⅣ-1068是从舟山长峙岛潮间带海泥中分离到的一株细菌,最适NaCl浓度范围为1%～3.5%,经琼脂扩散法抗菌模型筛选表明对大肠杆菌、副溶血性弧菌、枯草芽孢杆菌、金黄色葡萄球菌、藤黄微球菌和白假丝酵母有拮抗作用。利用形态学观察、生理生化反应对菌株进行了初步研究,并利用PCR的方法扩增了CZⅣ-1068的16S rDNA,然后进行核苷酸序列测定分析,结果表明CZⅣ-1068与Bacillus sp.82344(AF227848)相似性高达100%,初步确定为腊状芽孢杆菌的一种。     

毛细管电泳法测定胺类手性药物结合常数

采用毛细管区带电泳法,在20℃温度下,选择含不同浓度高磺化-β环糊精（HS-β—CD）磷酸盐缓冲溶液（磷酸盐浓度50mmol／L,pH2．50）,分别试验了HS-β-CD与伯胺、仲胺和叔胺三种胺类手性药物萘乙胺、盐酸异丙肾上腺素和扑尔敏的分离情况,采用双倒数法求解结合常数,结果表明HS-β—CD与叔胺类药物扑尔敏的结合常数最大,并对实验结果进行了讨论．     

Evolution of the Xiaotian-Mozitan fault and its implications for exhumation of Dabie HP-UHP rocks

The Xiaotian-Mozitan fault （XMF） located north of the Dabie orogenic belt separates the North Dabie complex to the south from the Beihuaiyang low-grade metamorphic rocks to the north. It comprises several NW-striking ductile shear zones and brittle faults. The brittle faults obviously overprinted on the ductile shear zones and promoted the development of the volcanic basins in early Cretaceous to the north, which suggests that the brittle faults were normal faults formed in early Cretaceous during doming of the Dabie orogenic belt. The ductile shear zone superposed on the north Dabie gray gneiss, and it is an important channel where the Dabie HP-UHP rocks exhumed. For obtaining new structural constraint on exhumation of the HP-UHP rocks, we present here experimental results on the microstructure, quartz C-axis fabrics and the microprobe analyses of phengite. The ductile shear zone was determined to be formed at a temperature of 600-650 ℃ and pressure of 1.1 GPa by the mineral deformation, microprobe analyses and geobarometry of Si-in-phengite of the mylonite, the results suggest that the mylonite now exposed on the surface experienced an upper amphibolite-facies metamorphism in the lower crust. The mineral stretching lineation varies from horizontal in the east segment to sub-dip in the west. Shear sense indicators from outcrop and thin sections of orientated specimen and quartz C-axis fabrics suggest that the XMF is a sinistral normal fault. The kinematics analysis of the ductile shear zone indicates that the exhumation of Dabie HP-UHP rocks is the results of a SE-directed extrusion and an anticlockwise rotation around its eastern pivot simultaneously.     

体外预应力桥钢索转向区力学性能仿真分析

结合某高速公路体外预应力试验桥的设计,利用桥梁分析专业软件MIDAS/Civil对该桥的转向块区域力学性能进行了空间仿真分析,研究了该关键区域的应力分布、受力特点以及传力路径;根据混凝土材料本构关系和屈服准则提出了利用应力差值分析屈服区域特性的研究手段.得出转向块结构竖向压应力主要分布在肋部的转向管道以上部分;竖向拉应力主要分布在转向肋与底板交界外缘处以及转向管道之间区域,建议加宽转向管道间距,以减小该区域的应力集中现象.根据仿真分析结果,对实际工程的设计和施工提出了一些切实可行的建议,研究结论可供类似工程参考.     

脆性材料斜裂纹断裂与损伤耦合分析

对单向拉伸的斜裂纹,应用西多霍夫损伤模型和断裂力学耦合分析方法,推导出脆性材料斜裂纹损伤区与断裂区的边界方程,确定了脆性材料斜裂纹初始损伤区和断裂区的径向尺寸.提出了裂尖断裂区内径向应变能的概念,并建立了基于此概念上的裂纹扩展准则,即裂尖断裂区内径向最小应变能(RMSE)判据,从而确定了脆性材料斜裂纹在断裂区边界上的开裂角.最后确定了不同裂纹倾角起裂点的坐标.     

软土地基浅层处理及施工方法

阐述了公路软土路基处理的必要性,介绍了公路软土路基的主要处理方法以及作用机理。     

松辽盆地西斜坡古沟谷-坡折带特征及其对储层分布的控制

利用井-震结合、地层对比、沉积相及古地貌分析等方式识别沟谷-坡折带,重点分析了沟谷-坡折带特征及对储层分布的控制作用.研究表明:松辽盆地西斜坡早白垩世发育的两极挠曲坡折带在平面上呈北东向展布;沟谷顺物源分布,垂直于坡折带走向;在基准面旋回变化过程中,沟谷-坡折带对沉积物的体积分配和相分异有特定的控制作用,进而与储层的分布有着密不可分的关系;沟谷是控制水系和沉积物搬运的通道,坡折带是沉积物卸载的场所,沟谷-坡折带体系控制了沉积物的类型和平面分布.     

综放工作面过风氧化带围岩控制技术

平朔井工三矿39017工作面局部区域为风氧化带,综放工作面过风氧化带期间存在安全隐患问题,为使综放工作面安全高效通过风氧化带,采取如下措施:一是在39107辅运巷超前注浆加固;二是使用U型棚支架加强支护39107辅运巷;三是加强工作面条件管理,如提高初撑力、顶梁铺网、架前注浆等方法。目前工作面已顺利通过风氧化带,确保了安全生产,提高了煤炭回收率,提升了生产效益。