大别山太湖地区宿松变质杂岩中石榴斜长角闪岩的P-T轨迹及反映的俯冲过程   总被引：1，自引：0，他引：1       下载免费PDF全文

石永红  林伟  王清晨 《地质科学》2007,42(3):518-531

依据对大别山太湖地区宿松变质杂岩中的石榴斜长角闪岩的岩相学、矿物成份分析和P-T条件评价,将变质作用分为Ⅰ、Ⅱ、Ⅲ和Ⅳ4个阶段,其中Ⅰ、Ⅱ阶段经历了绿帘角闪岩相的变质;Ⅲ阶段为峰期变质,变质条件为T=580℃,P=1.31GPa,为角闪石—榴辉岩相变质;Ⅳ阶段为绿片岩相变质。构建的P-T轨迹显示了顺时针的演化特征,反映了宿松变质杂岩分阶段的、不等速的俯冲和折返过程:早期短暂的迅速俯冲→峰期缓慢俯冲→晚期可能的相对缓慢抬升。研究表明宿松变质杂岩的峰期变质条件偏离“俯冲梯度”线,显示了大幅增温、压力变化轻微的特征,这一增温可能是由于受到扰动的热结构恢复所致。结合前人对高压榴辉岩的峰期变质条件的研究,认为宿松变质杂岩与高压-超高压榴辉岩单元至少有0.5GPa的压力差,约15km厚的地壳损失,两者为太湖—马庙断层(F₂)所分隔。  相似文献   

Pullout resistance of single vertical shallow helical and plate anchors in sand   总被引：1，自引：1，他引：1  

Adel Hanna  Tahar Ayadat  Mohab Sabry 《Geotechnical and Geological Engineering》2007,25(5):559-573

This paper presents analytical models to predict the pullout capacity and the load–displacement relationship for shallow single vertical helical and plate anchors in sand. The models were developed based on the failure mechanism deduced from laboratory testing and utilize the limit equilibrium technique. Expression was given to estimate the critical depth for a given anchor/soil conditions, which separates deep from shallow anchors. Furthermore, the radius of influence of a individual anchor on the ground surface is established, and accordingly, the spacing between anchors can be determined to avoid anchors interactions between anchors. The proposed theory compared well with the theories and the experimental data available in the literature.

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Résumé Cet article présente un model analytique pour prédire la résistance à l’arrachement et la relation charge-diplacement pour les ancrages à vis et plats verticaux superficiels ancrés dans le sable. Le model est basé sur le mécanisme de rupture déduit des essais de laboratoire et utilise la méthode d’analyse à l’équilibre limite. En outre, une expression a été proposé pour éstimer la profondeur critique pour un ancrage donné permettant d’identifier l’ancrage comme superficiel ou profond. Le rayon d’influence d’un ancrage à la surface du sable autour de l’ancrage a été établi, et par conséquent, l’espacement entre ancrages peut être déterminer pour éviter toute interaction. La théorie proposée montre une bonne concordance avec des résultats theoriques et expérimentaux rapports dans la literature.

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扬子板块海相中古生界盆地的递进变形改造   总被引：2，自引：0，他引：2  

丁道桂刘光祥  吕俊祥潘文蕾 《地质通报》2007,26(9):1178-1188

印支—早燕山期由于古特提斯洋盆的关闭,扬子板块大陆边缘受到了挤压与碰撞作用,在板内形成了江南-雪峰基底拆离体(A带),从SE向NW方向的大规模水平推挤作用使扬子板内中古生界盆地发生了由强及弱的递进(衰减)变形改造。在其前缘形成了高角度冲断层-断弯褶皱带(B带)、逆掩断层-断展褶皱带(C带)、滑脱断层-滑脱褶皱带(D带)、共轭冲断层-膝折褶皱带(E带)和古隆起-单斜带(F带);在其后缘则形成了滑覆断层-滑脱褶皱带(G带)。不同的构造变形区带具有不同的水平位移量、压缩变形量,不同的逆冲断裂、褶皱的空间配置和不同的构造圈闭类型、保存条件,因而控制了不同类型的油气聚集与分布。  相似文献   

长白山天池火山地震活动机理研究   总被引：2，自引：0，他引：2  

吕政  洪汉净  魏海泉 《东北地震研究》2007,23(1):40-48

对1999年以来长白山火山观测站记录到的火山地震活动进行了研究,发现在西北太平洋5.0级以上中深源地震发生前后,均有火山地震活动发生变化。我们统计发现有以下三种情况:第一种是深源地震发生后火山地震随之增强;第二种是火山震群活动结束后发生中深源地震;第三种是深源地震前后火山地震活动频繁,在火山地震活动较少时发生中深源地震。本文通过对近年来长白山火山地震活动与西北太平洋俯冲板块的中、深源地震关系以及火山玄武岩地幔性质和长白山地热活动等资料并参考前人研究成果,建立了长白山地幔柱模型,对长白山火山地震活动机制进行了初步探讨。  相似文献   

Mountain belt growth inferred from histories of past plate convergence: A new tectonic inverse problem     

Giampiero Iaffaldano  Hans-Peter Bunge  Martin Bücker 《Earth and Planetary Science Letters》2007,260(3-4):516-523

Past plate motions display a range of variability, including speedups and slowdowns that cannot easily be attributed to changes in mantle related driving forces. One key controlling factor for these variations is the surface topography at convergent margins, as previous modeling shows that the topographic load of large mountain belts consumes a significant amount of the driving forces available for plate tectonics by increasing frictional forces between downgoing and overriding plates. Here we use this insight to pose a new tectonic inverse problem and to infer the growth of mountain belts from a record of past plate convergence. We introduce the automatic differentiation method, which is a technique to produce derivative code free of truncation error by source transformation of the forward model. We apply the method to a publicly available global tectonic thin-shell model and generate a simple derivative code to relate Nazca/South America plate convergence to gross topography of the Andes mountain belt. We test the code in a search algorithm to infer an optimal paleotopography of the Andes 3.2 m.y. ago from the well-known history of Nazca/South America plate convergence. Our modeling results are in excellent agreement with published estimates of Andean paleotopography and support the notion of strong feedback between mountain belt growth and plate convergence.  相似文献   

组合剪力墙的抗震研究与发展   总被引：4，自引：3，他引：4  

王敏  曹万林  张建伟 《地震工程与工程振动》2007,27(5):80-87

剪力墙是高层建筑结构中的核心抗侧力部件,研制抗震性能好的剪力墙,是建筑抗震设计的关键技术之一。组合剪力墙包括不同材料和不同结构形式的组合,可以发挥不同材料和不同结构形式各自的优势,使剪力墙的延性和耗能能力得以提高,从而改善其抗震性能。本文对国内外一些新型组合剪力墙的抗震研究工作进行了归纳总结,并对其发展作一展望。  相似文献   

Multi-hazard performance assessment of a transfer-plate high-rise building     

徐幼麟 《地震工程与工程振动(英文版)》2007,6(4):371-382

Many urban areas are located in regions of moderate seismicity and are subjected to strong wind. Buildings in these regions are often designed without seismic provisions. As a result, in the event of an earthquake, the potential for damage and loss of lives may not be known. In this paper, the performance of a typical high-rise building with a thick transfer plate (TP), which is one type of building structure commonly found in Hong Kong, is assessed against both earthquake and wind hazards. Seismic- and wind-resistant performance objectives are fi rst reviewed based on relevant codes and design guidelines for high-rise buildings. After a brief introduction of wind-resistant design of the building, various methodologies, including equivalent static load analysis (ESLA), response spectrum analysis (RSA), pushover analysis (POA), linear and nonlinear time-history analysis (LTHA and NTHA), are employed to assess the seismic performance of the building when subjected to frequent earthquakes, design based earthquakes and maximum credible earthquakes. The effects of design wind and seismic action with a common 50-year return period are also compared. The results indicate that most performance objectives can be satisfi ed by the building, but there are some objectives, such as inter-story drift ratio, that cannot be achieved when subjected to the frequent earthquakes. It is concluded that in addition to wind, seismic action may need to be explicitly considered in the design of buildings in regions of moderate seismicity.  相似文献   

Late stage thermal history of the Songliao Basin and its tectonic implications: Evidence from apatite fission track (AFT) analyses     

Xiang CaiFu  Feng ZhiQiang  Pang XiongQi  Wu HeYong  Li JunHong 《中国科学D辑(英文版)》2007,50(10):1479-1487

Apatite Fission Track (AFT) data from the Songliao Basin indicates that the late stage tectonic movements in the Songliao Basin have zoning in space and episodes in time. The late stage tectonic movements started from the east part of the basin and migrated westward. AFT ages in the east part of the basin are older than those in the west part of the basin, suggesting that the uplift occurred earlier in the east than in the west. The denudation thickness in the east part of the basin is significantly greater than that in the centre and west. The thermal history evolved two episodes of rapid cooling and subsequent slow cooling processes. Age-depth relationship derived from the AFT data indicates a four-episode denudation history. Further Monte Carlo random simulation of the AFT data reveals the four changing points of the thermal evolution at 65 Ma, 43.5 Ma, 28 Ma and 15 Ma, respectively. The uplifting and denudation rates from different episodes of evolution are proportional to the plate convergence rate. Based on the above analyses and the regional geologic background, it is concluded that the late stage thermal events in the Songliao Basin are the far field response to the subduction of the Pacific Plate under the Eurasian Plate. The first episode of the rapid cooling probably started at the end of the Nenjiang Formation, climaxed at the end of the Cretaceous and ceased at the Late Eocene. The subsequent slow cooling lasts another 15 Ma. The first episode of the evolution is the far field response to the major episode of the Yanshan Movement and subsequent series of the tectonic reorganization, especially the directional change of the Pacific Movement and also the subduction of the Indian Plate underneath the Eurasian Plate. While the second episode of the evolution is the far field response to the extension and closure of the Sea of Japan. Extension led to the migration and converging of the mantle heat flow to the Sea of Japan and resulted in the rapid cooling of the Songliao Basin.  相似文献   

Geochemical characteristics of Bikou volcanic group and Sr-Nd-Pb isotopic composition: Evidence for breakup event in the north margin of Yangtze plate, Jining era     

LI YongFei  LAI ShaoCong  QIN JiangFeng  LIU Xin  WANG Juan 《中国科学D辑(英文版)》2007,50(Z2):339-350

The geodynamic setting of the Bikou volcanic group is a critical question to trace the Precambrain tectonic framework and evolution for the Yangtze plate. This study has suggested that the Bikou volcanic group is composed of several residual oceanic crust units MORB (mid-ocean ridge basalt), Alk-OIB (alkaline ocean island basalt) and Th-OIB (tholeiitic ocean island basalt) as well as subduction-related volcanic rocks. According to field observation, those distinct rocks occurred collectively in form of tectonic contact, implying that the Bikou volcanic group was an ophiolitic mélange. Coupled with geochronological data, a perished oceanic basin at the northern margin of the Yangtze block during Neoproterozoic was tested by this ophiolitic mélange. Meanwhile, the isogeochemical data suggest that the ocean occurred in the Southern Hemisphere identical to Indian, South Atlantic and South Pacific oceans in terms of their Dupal anomalies, and the original source of the rocks could be probably mixing by EMⅠand EMⅡ component caused by dehydration melting of subducting oceanic crust during subduction process. On the basis of geochemical characteristics of the studied rocks, the Bikou volcanic group could imply that a partial breakup event occurred in the northern margin of Yangtze plate during the Neoproterozoic era.  相似文献   

新疆塔里木板块西北缘早二叠世深水遗迹化石的发现及意义   总被引：2，自引：0，他引：2  

丁孝忠  吴绍祖 《沉积学报》2000,18(4):495-500

在新疆塔里木板块西北缘下二叠统比尤勒提群中部首次发现了大量深水遗迹化石,主要包括Glockeria Ksiazkiewicz1968,Helminthoida sp.,Megagrapton sp.,Paleodictyon sp.,Paleodictyon(Glenodictyum)Croaticum Ulchman1995,Planolites sp.,Protopaleodictyon sp.,Scalaritubamissouriensis Weller1899,Spirophycus sp.等,代表典型深海环境的Nereites遗迹相。根据对温古尔剖面的研究,比尤勒提群下部为浅海陆棚相砂泥质灰岩、粉砂质泥岩、粉砂岩、泥晶灰岩等;而含丰富遗迹化石的比尤勒提群中部为一套深海海底扇沉积的浊积岩系夹少量硅质岩,并且在浊积扇的不同位置所产遗迹组合类型也明显不同,扇根以觅食迹为主,含大量穿相分子,扇中开始出现牧食迹,扇梢则出现特征的耕作迹;比尤勒提群上部为浅海陆棚-滨海相沉积的硅质灰岩、泥晶灰岩和砂质灰岩及粉砂质泥岩、钙质砂岩等。该套遗迹化石组合与深海浊积事件密切相关,同时表明塔里木板块西北缘早二叠世时期存在一个陆棚浅海-深海盆地沉积环境,晚二叠世时期海水向西退去形成陆相沉积。  相似文献