苏丹哈佳吉金矿区地质特征及控矿因素浅析     

鲍中义  杨立新  谭建刚  李山  李瑞翔 《山东地质》2011,(10):16-19

哈佳吉金矿区位于尼罗河大型韧性剪切带次级构造带上,属岩浆热液破碎带蚀变岩型金矿床。该文通过论述矿区地质特征,总结控矿因素,证实该区矿体严格受构造蚀变带控制,近EW向韧性剪切构造,尤其是构造转弯部位、构造膨大部位、不同级别构造复合部位,以及多期成矿作用叠加部位是矿床形成的有利空间。并与岩性和蚀变矿化关系密切,赋存于黄铁矿化碎裂岩、黄铁矿化硅化变粒岩质碎裂岩带中,产状与蚀变矿化带一致。  相似文献   

Upper mantle P-wave tomography across the Longmenshan fault belt from passive-source seismic observations along Aba-Longquanshan profile     

Zhiming Bai  Xiaobo Tian  You Tian 《Journal of Asian Earth Sciences》2011,40(4):873-882

A passive seismic experiment across the Longmenshan (LMS) fault belt had been conducted between August 2006 and July 2007 for the understanding of geodynamic process between the Eastern Tibet and Sichuan basin. We herein collected 3677 first P arrival times with high precision from seismograms of 288 teleseismic events so as to reconstruct the upper mantle velocity structure. Our results show that the depth of the Lithosphere–asthenosphere boundary (LAB) changes from 70 km beneath Eastern Tibet to about 110 km beneath Longquanshan, Sichuan Basin, which is consistent with the receiver function imaging results. The very thin mantle part of the lithosphere beneath Eastern Tibet may suggest the lithosphere delamination due to strong interaction between the Tibetan eastward escaping flow and the rigid resisting Sichuan basin, which can be further supported by the existences of two high-velocity anomalies beneath LAB in our imaging result. We also find there are two related low-velocity anomalies beneath the LMS fault belt, which may indicate magmatic upwelling from lithosphere delamination and account for the origin of tremendous energy needed by the devastating Wenchuan earthquake.  相似文献   

Source characteristics of the Yutian earthquake in 2008 from inversion of the co-seismic deformation field mapped by InSAR     

Xinjian Shan  Guohong Zhang  Chisheng Wang  Chunyan Qu  Xiaogang Song  Guifang Zhang  Liming Guo 《Journal of Asian Earth Sciences》2011,40(4):935-942

On 21 March 2008, an Ms7.3 earthquake occurred at Yutian County, Xinjiang Uygur Autonomous Region, which is in the same year as 2008 Mw 7.9 Wenchuan earthquake. These two earthquakes both took place in the Bayar Har block, while Yutian earthquake is located in the west edge and Wenchuan earthquake is in the east. The research on source characteristics of Yutian earthquake can serve to better understand Wenchuan earthquake mechanism. We attempt to reveal the features of the causative fault of Yutian shock and its co-seismic deformation field by a sensitivity-based iterative fitting (SBIF) method. Our work is based on analysis and interpretation to high-resolution satellite (Quickbird) images as well as D-InSAR data from the satellite Envisat ASAR, in conjunction with the analysis of seismicity, focal mechanism solutions and active tectonics in this region. The result shows that the 22 km long, nearly NS trending surface rupture zone by this event lies on a range-front alluvial platform in the Qira County. It is characterized by distinct linear traces and a simple structure with 1–3 m-wide individual seams and maximum 6.5 m width of a collapse fracture. Along the rupture zone are seen many secondary fractures and fault-bounded blocks by collapse, exhibiting remarkable extension. The co-seismic deformation affected a big range 100 km × 40 km. D-InSAR analysis indicates that the interferometric deformation field is dominated by extensional faulting with a small strike-slip component. Along the causative fault, the western wall fell down and the eastern wall, that is the active unit, rose up, both with westerly vergence. The maximum subsidence displacement is ～2.6 m in the LOS, and the maximum uplift is 1.2 m. The maximum relative vertical dislocation reaches 4.1 m, which is 10 km distant from the starting rupture point to south. The 42 km-long seismogenic fault in the subsurface extends in NS direction as an arc, and it dipping angle changes from 70° near the surface to 52° at depth ～10 km. The slip on the fault plane is concentrated in the depth range 0–8 km, forming a belt of length 30 km along strike on the fault plane. There are three areas of concentrating slip, in which the largest slip is 10.5 m located at the area 10 km distant from the initial point of the rupture.  相似文献   

山东诸城晚白垩世古地震事件与恐龙化石埋藏   总被引：2，自引：0，他引：2  

何碧竹  乔秀夫  田洪水  陈树清  张艳霞 《古地理学报》2011,13(6):615-626

在山东诸城库沟、龙骨涧、西见屯集群恐龙化石埋藏层——上白垩统王氏群辛格庄组与红土崖组中,发现存在脆性、塑性及液化等多种类型的软沉积物变形构造,主要包括负载构造、球一枕构造、挤入构造(火焰构造)、液化卷曲变形、液化脉状构造、混插沉积构造及地震断裂等典型的粗碎屑沉积物形成的古地震记录.多层的软沉积物变形构造及未变形沉积层间...  相似文献   

Geomorphological and sedimentological comparison of fluvial terraces and karst caves in Zhangjiajie,northwest Hunan,China: an archive of sandstone landform development     

Guifang Yang  Xujiao Zhang  Mingzhong Tian  Yamin Ping  Anze Chen  Zhiliang Ge  Zhiyun Ni  Zhen Yang 《Environmental Earth Sciences》2011,64(3):671-683

The Zhangjiajie Sandstone Peak Forest Geopark (Zhangjiajie World Geopark) of northwest Hunan, China hosts a well-preserved sequence of fluvial terraces and karst caves. In this contribution, a comparative study of fluvial terraces with karst caves along the middle-lower Suoxi River in Zhangjiajie World Geopark is presented to improve the understanding of the development of striking sandstone landscape in the upper Suoxi River. By integrating geomorphological, sedimentological, and geochronological techniques, the possible correlation between fluvial terraces and karst caves, as well as their climatic and tectonic implications is investigated. The available electron spin resonance and thermo-luminescence numerical ages coupled with morphostratigraphic analysis indicate that aggradation of fluvial terrace levels occurred at ca. 347 ± 34 ka (T₄), 104.45 ± 8.88 to 117.62 ± 9.99 ka (T₃), 60.95 ± 5.18 ka (T₂), and Holocene (T₁), followed by the stream incision. Fluvial terrace levels (T₄ to T₁) correlate morphologically with the karst cave levels (L₁ to L₄), yet the proposed chronology for the fluvial terrace levels is a bit later than the chronological data obtained from karst caves. In northwest Hunan, where a unique sandstone peak forest landscape was extensively developed, the fluvial terrace sequences as well as the cave systems are the important archives for studying the evolution of the sandstone landscape. The beginning of the sandstone landscape development must be earlier than the aggradation of the fluvial terrace T₄, allowing this unique landscape to occur in the Middle Pleistocene.  相似文献   

0908号台风“莫拉克”异常路径及其对台湾海峡两岸强降水的影响     

刘爱鸣  高珊 《台湾海峡》2011,30(2):151-157

应用常规资料,结合雷达、卫星云图和其他观测资料,分析了0908号台风＂莫拉克＂异常路径及其对台湾海峡两岸强降水的影响.结果表明：（1）500 hPa欧亚中高纬度为两槽一脊的形势和东北区域大范围的正变高使副热带高压加强西伸,以及0909号热带气旋＂艾涛＂前身低压阻挡了副热带高压南落的共同作用,使＂莫拉克＂台风前期向偏西方向移动.（2）高空冷涡提供了有利于热带低压维持和发展的动力条件,热带低压的维持又对＂莫拉克＂的移动造成影响.（3）冷空气持续南下造成副热带高压减弱,并且在＂莫拉克＂台风北侧形成稳定低能区;高空冷涡引起其北侧中高层高度下降和东风引导气流减弱;在弱环流和多热带气旋的环境场下,以及热带风暴＂天鹅＂（0907号）、＂艾涛＂对＂莫拉克＂台风的反方向作用力等因素的综合作用,是＂莫拉克＂台风在台湾海峡移速异常缓慢的原因.（4）＂莫拉克＂台风在台湾海峡滞留时间长,其北侧强偏东风和南侧强西南风带来充沛的水汽,及迎风坡辐合抬升所产生的中小尺度系统是造成闽北、浙南和台湾岛南部强降水持续时间长、累计雨量大的重要原因.  相似文献   

山东半岛北岸现代海滩层理及动态解释     

曹立华  栾天  庄振业  李兵  董威力  孙羽涵 《海洋地质前沿》2011,(9):1-5,31

海滩层理由冲、回流塑造的向海倾前滨楔状交错层理和冲越流形成的向陆倾后滨斜层理组成,二者构成假背斜构造.近年在烟台—莱州岸段海滩上开挖了10个垂岸探槽,揭示出这里海滩以向陆倾后滨层理为主,并且被暴风浪侵蚀面所斜切,该面向海的前滨层理只留下几十厘米的薄层,说明近几十年海岸持续遭受侵蚀,海滩的前滨层理被多次暴风浪切割掉;按暴...  相似文献   

A study of extratropical transition and re-intensification of Typhoon Mindulle (2004)     

Xiande Zhu  Qi Wang  Gang Fu  Yulong Liu  Ying Tian 《中国海洋大学学报(英文版)》2011,10(3):197-209

In this study,the fifth-generation Pennsylvania State University-National Center for Atmospheric Research (PSU-NCAR) Mesoscale Model (MM5) is used to simulate Typhoon Mindulle (2004) at high resolution (3-km grid size).The data from measurements show that in the upper atmosphere the existence of an upper jet is important to the transition cyclone.When Mindulle moved to the area of the upper jet entrance,where high-altitude divergence existed, the pumping of the high-altitude divergence would enhance the vertical motion and low-level cyclone convergence. The enhanced vertical motion was confirmed by the simulation results and indicated that the existence of upper divergence enhanced the vertical motion which was favorable for the maintenance of Typhoon Mindulle.The process of extratropical transition (ET) and re-intensification always accompanies the process of cold air invasion. This process enhances the baroclinicity of the atmosphere and the formation of front at high altitudes, which converts baroclinic potential energy into kinetic energy and strengthens the cyclone vortex.The distributions of equivalent potential temperature (θe) and temperature anomalies show that the warm-core of the typhoon at the tropopause aids the re-intensification of the system. As the typhoon reenters the ocean, latent heat flux (LHF) increases in the north and west and the strong reflectivity and vertical motion occur in the east and southeast,and the west.With the re-intensification of the typhoon the wind field evolves from an oval to a circle at the lower atmosphere, the area coverage by high winds increases, and the distribution of the tangential wind shows an asymmetric pattern.  相似文献   

Development of 57 novel polymorphic microsatellite markers in half-smooth tongue sole (Cynoglossus semilaevis)     

Guidong Miao  Ying Xu  Di Wang  Songlin Chen  Tingjun Fan  Yongsheng Tian 《中国海洋大学学报(英文版)》2011,10(3):241-245

Half-smooth tongue sole (Cynoglossus semilaevis) is a promising species for aquaculture in China.The wild population of C. semilaevis is under threat from environmental factors. Microsatellite markers are very suitable for assessing genetic diversity. Four microsatellite-enriched libraries of half smooth tongue sole (Cynoglossus semilaevis) were constructed,from which 57 polymorphic microsatellites were isolated and characterized.The polymorphism of these microsatellites was assessed by genotyping in 30 ind...  相似文献   

基于规划协调的乡镇土地利用统一分类研究   总被引：2，自引：0，他引：2  

张亚丽  黄珺嫦  蔡运龙  田华文 《地域研究与开发》2011,30(5)

清晰统一的用地分类是实现乡镇土地利用总体规划和村镇体系规划协调的基础。回顾了建设和国土部门土地利用分类的历程,提出统一土地分类的原则,对《土地利用现状分类》(GB/T 21010—2007)和《镇规划标准》(GB 50188—2007)中土地分类进行对比分析,确定了统一的乡镇土地利用分类,为有效指导农村区域土地资源利用和规划提供借鉴。统一的乡镇土地利用分类包括12个一级类,59个二级类,其中有9个二级类划分了三级类,三级类共有21个;以《土地利用现状分类》(GB/T 21010—2007)为准的一级类包括8个,二级类包括49个;以《镇规划标准》(GB 50188—2007)为准的二级类1个;两者综合并重新定义的一级类4个,二级类9个。  相似文献