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Factors Influencing the Successful Adoption of Human Resource Information System: The Content of Aqaba Special Economic Zone Authority
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作者 Hisham Al-Mobaideen Sattam Allahawiah Eman Basioni 《Intelligent Information Management》 2013年第1期1-9,共9页
This study examines the key factors that have impact on the successful adoption of Human Resource Information System (HRIS) within the Aqaba Special Economic Zone Authority (ASEZA)/Jordan. In order to accomplish the p... This study examines the key factors that have impact on the successful adoption of Human Resource Information System (HRIS) within the Aqaba Special Economic Zone Authority (ASEZA)/Jordan. In order to accomplish the purpose of the study four critical factors are inquired. So, four critical factors are inquired: First, TAM Model (Perceived Ease of Use (PEOU) and Perceived Usefulness (PU)). Second, Information Technology Infrastructure (ITI). Third, Top Management Support (TMS). Finally, Individual Experience with Computer (IEC). The research model was applied to collect data from the questionnaires answered by 45 users of HRIS as a source of primary data, based on a convenience sample the response rate was about 91%. In addition, the results were analyzed by utilizing the Statistical Package for Social Software (SPSS). Furthermore, the findings were analyzed;multiple Regression analysis indicated that all research variables have significant relationship on successful adoption of HRIS. The findings indicated IT infrastructures have a positive and significant effect on the successful adoption of HRIS. But there is no significant of PU, PEOU, TMS, and IEC on the successful adoption of HRIS. Finally, the results indicated that no significant statistical differences of demographic characteristics on HRIS adoption. Depending on the research’s findings;the researchers proposed a set of recommendations for better adoption of HRIS in SEZA. 展开更多
关键词 Human Resource INFORMATION System (HRIS) Aqaba Special Economic zone AUTHORITY (ASEZA) PERCEIVED USEFULNESS (PU) INFORMATION Technology Infrastructure (ITI) Top Management Support (TMS) and Individual Experience with Computer (IEC)
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Vertical dominant migration channel and hydrocarbon migration in complex fault zone, Bohai Bay sag, China
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作者 XU Changgui PENG Jingsong +2 位作者 WU Qingxun SUN Zhe YE Tao 《Petroleum Exploration and Development》 2019年第4期720-728,共9页
The quantitatively/semi-quantitatively formation conditions of vertical dominant hydrocarbon migration pathways were analyzed based on the big data analysis of petroleum geological parameters of complex fault Zone zon... The quantitatively/semi-quantitatively formation conditions of vertical dominant hydrocarbon migration pathways were analyzed based on the big data analysis of petroleum geological parameters of complex fault Zone zone in the central-south Bohai Bay. According to this condition, the vertical dominant migration pathway and its charge points/segments are searched through structural modeling assistant analysis in the East Sag of Huanghekou. Under the constraints of charge points/segments, numerical simulation of hydrocarbon charge and migration is carried out to successfully predict hydrocarbon migration pathways and hydrocarbon enrichment blocks in shallow layers of complex fault zone. The main results are as follows:(1) The hydrocarbon charge in shallow layers of the active fault zone is differential, the charge points/sections of vertical dominant migration pathways are the starting points of shallow hydrocarbon migration and are very important for the hydrocarbon migration and accumulation in the shallow layers.(2) Among the shallow faults, those cutting the deep transfer bins or deep major migration pathways, with fault throw of more than 80 m in the accumulation period and the juxtaposition thickness between fault and caprock of the deep layers of less than 400 m are likely to be vertical dominant migration pathways in the sag area.(3) By controlling the vertical dominant migration pathways and charging points/segments in carrier layer, Neo-tectonic movement caused the differential hydrocarbon accumulation in the complex fault zone. The research results are of great significance for the fine exploration of the complex fault zone. 展开更多
关键词 offshore Bohai Bay Basin SAG area VERTICAL DOMINANT MIGRATION pathway COMPLEX fault zone charge points NEOTECTONIC movement big data analysis
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Characterizing Potential Fishing Zone of Skipjack Tuna during the Southeast Monsoon in the Bone Bay-Flores Sea Using Remotely Sensed Oceanographic Data 被引量:1
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作者 Mukti Zainuddin Alfa Nelwan +4 位作者 Siti Aisjah Farhum Najamuddin   Muhammad A. Ibnu Hajar Muhammad Kurnia Sudirman   《International Journal of Geosciences》 2013年第1期259-266,共8页
Potential fishing zones for skipjack tuna in the Bone Bay-Flores Sea were investigated from satellite-based oceanography and catch data, using a linear model (generalized linear model) constructed from generalized add... Potential fishing zones for skipjack tuna in the Bone Bay-Flores Sea were investigated from satellite-based oceanography and catch data, using a linear model (generalized linear model) constructed from generalized additive models and geographic information systems. Monthly mean remotely sensed sea surface temperature and surface chlorophyll-a concentration during the southeast monsoon (April-August) were used for the year 2012. The best generalized additive model was selected to assess the effect of marine environment variables (sea surface temperature and chlorophyll-a concentration) on skipjack tuna abundance (catch per unit effort). Then, the appropriate linear model was constructed from the functional relationship of the generalized additive model for generating a robust predictive model. Model selection process for the generalized additive model was based on significance of model terms, decrease in residual deviance, and increase in cumulative variance explained, whereas the model selection for the linear model was based on decrease in residual deviance, reduction in Akaike’s Information Criterion, increasing cumulative variance explained and significance of model terms. The best model was selected to predict skipjack tuna abundance and their spatial distribution patterns over entire study area. A simple linear model was used to verify the predicted values. Results indicated that the distribution pattern of potential fishing zones for skipjack during the southeast monsoon were well characterized by sea surface temperatures ranging from 28.5℃ to 30.5 ℃ and chlorophyll-a ranging from 0.10 to 0.20 mg·m-3. Predicted highest catch per unit efforts were significantly consistent with the fishing data (P 2 = 0.8), suggesting that the oceanographic indicators may correspond well with the potential feeding ground for skipjack tuna. This good feeding opportunity for skipjack was driven the dynamics of upwelling operating within study area which are capable of creating a highly potential fishing zone during the southeast monsoon. 展开更多
关键词 Skipjack Tuna Satellite Data Generalized Additive Model Linear Model Upwelling Potential FISHING zones BONE BAY and FLORES SEA Southeast MONSOON
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四川盆地志留系层序地层及有利储集层分布 被引量:27
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作者 张林 魏国齐 +3 位作者 郭英海 汪泽成 吴世祥 沈珏红 《天然气工业》 EI CAS CSCD 北大核心 2005年第5期6-8,共3页
四川盆地志留系在加里东运动抬升剥蚀中仅残留下统地层,文章旨在研究其层序特征,指出有利勘探区。应用层序地层学方法,识别志留系进行层序界面,划分划分出5个层序、10个体系域,建立等时地层格架,分析储集层展布规律。志留系层序由加积... 四川盆地志留系在加里东运动抬升剥蚀中仅残留下统地层,文章旨在研究其层序特征,指出有利勘探区。应用层序地层学方法,识别志留系进行层序界面,划分划分出5个层序、10个体系域,建立等时地层格架,分析储集层展布规律。志留系层序由加积—退积的准层序组构成海侵体系和加积—进积的准层序组构成的高位体系域组成。储集岩有滨岸砂坝相的砂质岩和生物礁及生物浅滩碳酸盐岩,川东以“小河坝砂岩”碎屑岩储集层为主;川南以生物礁及生物浅滩灰岩储集层为主。 展开更多
关键词
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A Newly Discovered Oil-bearing Mesoproterozoic Erathem within the Niu D1 Well, Liaoxi Depression, Yanliao Faulted Depression Zone, NE China 被引量:3
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作者 SUN Qiushi GAO Xiaoyong +5 位作者 ZONG Wenming SUN Shouliang ZHANG Tao XIAO Fei LI Yongfei SHI Lei 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2020年第1期202-203,共2页
Objective The Yanshan Fold Belt is located within the northern margin of the North China platform and contains welldeveloped and widespread Neoproterozoic and Mesoproterozoic sedimentary units with a total thickness o... Objective The Yanshan Fold Belt is located within the northern margin of the North China platform and contains welldeveloped and widespread Neoproterozoic and Mesoproterozoic sedimentary units with a total thickness of up to 9000 m.Previous studies identified many oil seedlings as well as asphalt and ancient hydrocarbon reservoirs in Northern Hebei depression and western Liaoning depression.This research indicates that the Mesoproterozoic and Neoproterozoic sedimentary units are ideally suited for the formation of significant oil and gas resources.The Niu D1 well was drilled by the China Geological Survey(CGS)in the Niuyingzi area and intercepted oil immersions and oil-and gas-bearing units within a limestone reservoir in the middle Proterozoic Gaoyuzhuang Formation(Fig.1).This study presents new biomarker compound and carbon isotope data that indicate that the oil within this formation was derived from hydrocarbon source rocks of the Hongshuizhuang Formation,part of the Mesoproterozoic Jixian Series,and the reservoir type is overthrust fault fractured anticline hydrocarbon reservoir.The oil reservoir within the Gaoyuzhuang Formation limestone might represent the oldest oil reservoir discovered to date within the Yanliao faulted depression zone. 展开更多
关键词 NE China A NEWLY Discovered Oil-bearing MESOPROTEROZOIC Erathem within the Niu D1 WELL Yanliao Faulted DEPRESSION zone Liaoxi DEPRESSION
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Acoustic Monitoring of Anomaly Stressed Zones, Determination Their Positions, Surfaces, Evaluation of Catastrophic Risk
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作者 Olga Hachay Oleg Khachay 《Open Journal of Geology》 2020年第5期501-509,共9页
Abstract Problem statement. Self-organization is not a universal property of matter, it exists under certain internal and external conditions and this is not associated with a special class of substances. The study of... Abstract Problem statement. Self-organization is not a universal property of matter, it exists under certain internal and external conditions and this is not associated with a special class of substances. The study of the morphology and dynamics of migration of anomalous zones associated with increased stresses is of particular importance in the development of deep deposits, complicated by dynamic phenomena in the form of rock impacts. Applied method and design: An important tool for this study is geophysical exploration. To describe the geological environment in the form of an array of rocks with its natural and technogenic heterogeneity, one should use its more adequate description, which is a discrete model of the medium in the form of a piecewise heterogeneous block medium with embedded heterogeneities of a lower rank than the block size. This nesting can be traced several times, i.e. changing the scale of the study;we see that heterogeneities of a lower rank now appear in the form of blocks for heterogeneities of the next rank. A simple averaging of the measured geophysical parameters can lead to distorted ideas about the structure of the medium and its evolution. Typical results: We have analyzed the morphology of the structural features of disintegration zones before a strong dynamic phenomenon. The introduction of the proposed integrated passive and active geophysical monitoring into the mining system, aimed at studying the transient processes of the redistribution of stress-strain and phase states, can help prevent catastrophic dynamic manifestations during the development of deep-located deposits. Concluding note (Practical value/implications): Active geophysical monitoring methods should be tuned to a model of a hierarchical heterogeneous environment. Iterative algorithms for 2-D modeling and interpretation for sound diffraction and a linearly polarized transverse elastic wave on the inclusion with a hierarchical elastic structure located in the J-th layer of the N-layer elastic medium are constructed. 展开更多
关键词 High-Stressed zoneS Electromagnetic Induction METHOD Acoustic METHOD Hierarchical INCLUSIONS Layered-Block Medium Algorithms of Modeling And Interpretation Estimation of MASSIF No Stability
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Fault characteristics and control on hydrocarbon accumulation of middle-shallow layers in the slope zone of Mahu sag, Junggar Basin, NW China 被引量:3
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作者 CHEN Yongbo CHENG Xiaogan +3 位作者 ZHANG Han LI Chunyang MA Yongping WANG Guodong 《Petroleum Exploration and Development》 2018年第6期1050-1060,共11页
The development, evolution and formation mechanism of faults and their control on the migration and accumulation of Mesozoic oil and gas in the middle-shallow layers of the slope zone of Mahu sag were studied by the i... The development, evolution and formation mechanism of faults and their control on the migration and accumulation of Mesozoic oil and gas in the middle-shallow layers of the slope zone of Mahu sag were studied by the interpretation of seismic and drilling data. Two types of faults, normal and strike-slip, are developed in the middle-shallow layers of the slope zone of the Mahu sag and they are mostly active in the Yanshanian period. They are divided into four grade faults: The grade I strike-slip faults with NWW to near EW direction are related to the left-lateral transpressive fault zones in the northwest of Junggar Basin since the end of the Triassic. The grade II faults with NE to NNE direction are the normal faults located at the junction of the fault zone and the slope zone, and their formation is related to the extension at the top of the nose-like structures in the fault zone. The grade III faults, which are also the normal faults, are the result of the extension at the top of the lower uplifts in the slope zone and differential compaction. The grade IV faults with NE direction are normal faults, which may be related to the extension environment at the tip of the lower uplifts. Faults not only are the channel for the vertical migration of oil and gas, but also control the oil-gas accumulation. There are two types of oil-gas reservoirs in the middle-shallow layers of slope zone of Mahu sag: fault block reservoirs and fault-lithologic reservoirs. They have large traps and promising exploration potential. 展开更多
关键词 JUNGGAR Basin SLOPE zone of Mahu SAG middle-shallow layers fault genetic mechanism nose-like structure lower uplift hydrocarbon accumulation
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滇西吉义独蛇绿混杂岩的岩石地球化学特征、成因和构造环境探讨 被引量:2
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作者 何琦 肖龙 +1 位作者 魏启荣 倪平泽 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第12期3229-3240,共12页
滇西吉义独蛇绿混杂岩位于金沙江缝合带的南端,岩石组合出露较齐全,包括堆晶橄榄岩、堆晶辉石岩、堆晶辉长岩以及玄武岩等,它们呈构造岩片的形式产出并与外来岩块组成蛇绿混杂岩。堆晶橄榄岩和辉石岩具低Al_2O_3,低TiO_2,而高Mg~#值(Mg~... 滇西吉义独蛇绿混杂岩位于金沙江缝合带的南端,岩石组合出露较齐全,包括堆晶橄榄岩、堆晶辉石岩、堆晶辉长岩以及玄武岩等,它们呈构造岩片的形式产出并与外来岩块组成蛇绿混杂岩。堆晶橄榄岩和辉石岩具低Al_2O_3,低TiO_2,而高Mg~#值(Mg~#=0.88~0.92),富集Cr和Ni,稀土总量偏低(∑REE=14.82×10^(-6)~27.75×10^(-6)),倒"U"型的稀土元素分布特征。堆晶辉长岩和玄武岩的Mg~#值较低,分别为0.70~0.79和0.51~0.66,具拉斑系列的演化趋势。玄武岩可以细分为2组:第一组玄武岩以平坦型稀土配分模式,低Mg~#(Mg~#=0.44~0.46),低稀土总量(∑REE=52.29×10^(-6)~60.26×10^(-6))为特征;第二组玄武岩则为LREE弱富集型的稀土配分模式,其Mg~#较高(Mg~#=0.54~0.68),稀土总量也较高(ΣREE=62.13×10^(-6)~101.87×10^(-6))。在原始地幔标准化的微量元素配分图解中,两组玄武岩均相对富集大离子亲石元素而亏损Nb、Ta和Ti,与岛弧岩浆岩类似,明显不同于N-MORB。岩石的Sr-Nd同位素组成较为均一和稳定,堆晶橄榄岩和辉石岩的(^(87)Sr/^(86)Sr);=0.7051~0.7056,ε_(Nd)(t)=2.8~4.1,玄武岩的(^(87)Sr/^(86)Sr)_i=0.7050~0.7056,ε_(Nd)(t)=5.1~5.8,且显示出原始地幔的同位素组成特征,暗示这些岩石为同源岩浆分异演化而成的岩浆产物。岩浆演化的主要方式为分离结晶作用,受地壳混染不明显。岩浆结晶形成岩石的顺序为:堆晶橄榄岩→堆晶辉石岩→堆晶辉长岩→玄武岩2组→玄武岩1组。岩石地球化学特征表明,吉义独蛇绿岩的形成与俯冲作用有关,且形成于金沙江洋内俯冲的消减环境。 展开更多
关键词 西 绿 ophiolitic MELANGE geochemical characteristics REE fractional crystallization rare earth elements Jinshajiang suture zone basic unit
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大兴安岭地区德尔布干断裂带北段构造年代学研究 被引量:44
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作者 郑常青 周建波 +4 位作者 金巍 季建清 张兴洲 马志红 丁雪 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第8期1989-2000,共12页
德尔布干断裂带是大兴安岭隆起西侧NE向的重要断裂带,处在海拉尔-拉布达林-根河盆地西缘,是著名德尔布干成矿区东南边界断裂带。为了确定德尔布干断裂带运动性质、活动时间,深入探讨该断裂带与中生代海拉尔-拉布达林-根河盆地及大兴安... 德尔布干断裂带是大兴安岭隆起西侧NE向的重要断裂带,处在海拉尔-拉布达林-根河盆地西缘,是著名德尔布干成矿区东南边界断裂带。为了确定德尔布干断裂带运动性质、活动时间,深入探讨该断裂带与中生代海拉尔-拉布达林-根河盆地及大兴安岭盆山格局、认识德尔布干断裂带多金属矿床成因等问题,本文应用锆石SHRIMP和云母^(40)At/^(39)Ar定年技术,分别对断裂带内的细粒黑云母花岗岩侵入体、韧性变形的花岗闪长质片麻岩、白云母石英片岩,进行了同位素年代学研究。其中花岗闪长质片麻岩岩浆型锆石SHRIMP谐和年龄300.6±9.3Ma,为花岗闪长质片麻岩海西期的侵位年龄;而花岗闪长质片麻岩中黑云母^(40)At/^(39)Ar坪年龄是130.9±1.4Ma,白云母石英片岩的白云母^(40)Ar/^(39)Ar坪年龄是115.6±1.6Ma,代表早白垩世伸展构造变形年龄;细粒黑云母花岗岩侵入体岩浆型锆石SHRIMP谐和年龄130.1±1.4Ma,为同伸展构造变形侵位的岩浆事件。上述地质年代说明德尔布干断裂带是早白垩世(110~130Ma)该区最年轻的重大伸展构造变形产物。控制NE向大兴安岭隆起和中生代海拉尔-拉布达林-根河等火山沉积盆地的发育格局、以及中生代以来的地壳演化与成矿类型。 展开更多
关键词 fault zone SHRIMP plateau age EXTENSIONAL structure PROTOLITH ages DUCTILE deformation during Early CRETACEOUS
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一种新的宏、细观变形全场测量方法(英文) 被引量:1
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作者 王世斌 李翔宇 +6 位作者 佟景伟 P.Goudeau 王志勇 李林安 沈珉 岳澄 李鸿琦 《实验力学》 CSCD 北大核心 2005年第1期65-71,共7页
基于光学干涉和衍射理论,提出了一种新的用于宏、细观面内变形测量的光学方法。利用三束准直相干光之间的干涉,分别得到面内位移U+V和U-V的两幅耦合条纹图。借助于FFT相移技术,直接计算出全场的U和V分布。本实验系统中包含有长距离显微... 基于光学干涉和衍射理论,提出了一种新的用于宏、细观面内变形测量的光学方法。利用三束准直相干光之间的干涉,分别得到面内位移U+V和U-V的两幅耦合条纹图。借助于FFT相移技术,直接计算出全场的U和V分布。本实验系统中包含有长距离显微镜,三光束系统,数字图像采集和处理系统等。它具有光路简单,避开条纹级次的确定,直接计算得到U、V场等优点。将它用于热塑性复合材料 56层板AS4/PEEK[0/±45/90]7S三点弯曲梁位移场的宏、细观测量。得到了层间的变形规律。本文还利用三维各向异性弹性有限元法对AS4/PEEK[0/±45/90]7S三点弯曲梁进行了数值计算,得到了自由表面的位移场和应变场的数值解。定量分析了层间的变形传递规律,有助于进一步分析AS4/PEEK[0/±45/90]7S层合板宏、细观变形。 展开更多
关键词 FF
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Regional Geochemical Characteristics and Influence Factors of Soil Elements in the Pearl River Delta Economic Zone, China 被引量:2
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作者 Lei Dou Tingting Li 《International Journal of Geosciences》 2015年第6期593-604,共12页
Soil heavy metal pollution is one of the main environmental problems in Pearl River Delta Economic?Zone of China. Based on multi-purpose regional geochemical survey, regional eco-geochemical assessment, local eco-geoc... Soil heavy metal pollution is one of the main environmental problems in Pearl River Delta Economic?Zone of China. Based on multi-purpose regional geochemical survey, regional eco-geochemical assessment, local eco-geochemical assessment and comprehensive appraisal, the eco-geochemical survey and assessment in Pearl River Delta Economic Zone of 41,698 km2?were completed. Samples from soils were collected in accordance with the two-layer grid method. Totally 54 elements and indicators for soils were determined. Compared to deep soils, the sampled surface soils are enriched in OrgC, N, P, Cd, S,Hg, Ag, B, Au, S and poor with As, Ni, I, Co, Cr, V, MgO, Sc, Al2O3, Fe2O3?etc. The characteristics of geochemical reference value of element in soil that inherited soil parent material and regional elements combined features reflected that the elements enriched in the soil was interrelated with acid rock, sandstone and shale. The spatial distribution characteristics of element regional geochemistry were conditional by regional environmental geological conditions,and effected by human activities. The Pearl River Delta plain is a typical geochemical landscape area with regional anomaly of multiple-elements. The north, western and eastern parts of the Pearl River Delta Economic Zone are quite different in geochemical features due to regional geological background, soil parent materials, geomorphic characteristics and human activities. Environment quality evaluation results show that the grade I and grade II soil accounted for 19.9% and 57.3% of the total area. Many samples that widely distributed in the economic developed of Pearl River Delta Plain area reached the third-grade of national soil environment standard. The soil enriched in Cd, Hg, As, and the area ratio accounting for 22.8% of the total area. It is mainly controlled by the geochemical background, the Pearl River Delta formation evolution process, especially the marine transgression process lead to Cd, Cu, Zn and Pb enrichment in Pearl River Delta plain. At the same time, under the influence of higher pressure of human activities, all kinds of exogenous input material carrying heavy metal pollutants on soil environmental quality also could not to ignore. 展开更多
关键词 Regional GEOCHEMICAL Characteristic Soil ELEMENTS Source of ANOMALOUS ELEMENTS Influence Factors PEARL River Delta Economic zone China
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An overview of the resources and environment conditions and major geological problems in the Yangtze River economic zone, China 被引量:7
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作者 Yue-hua Jiang Liang-jun Lin +16 位作者 Li-de Chen Hua-yong Ni Wei-ya Ge Hang-xin Cheng Gang-yi Zhai Gui-ling Wang Yi-zhong Ban Yuan Li Ming-tang Lei Cheng-xuan Tan Jing-wen Su Quan-ping Zhou Tai-li Zhang Yun Li Hong-ying Liu Ke Peng Han-mei Wang 《China Geology》 2018年第3期435-449,共15页
Focusing on the Yangtze River economic zone,the previous geological researches are systematically summarized,resources and environment conditions and major geological problems which are needing to be concerned in land... Focusing on the Yangtze River economic zone,the previous geological researches are systematically summarized,resources and environment conditions and major geological problems which are needing to be concerned in land planning and construction are studied.The results show that the resource conditions of cultivated land,shale gas,geotherm,lithium and so on are superior in the Yangtze River economic zone,and the resources and environment conditions are conducive to develop the modern agriculture,clean energy industry and strategic emerging industries.3×1013 m^2 farmlands without heavy metal pollution are concentrated;there are three national level shale gas exploration and development bases with explored reserves of 5.441×1011 m^3;geothermal availability is 2.4×109 t of standard coal each year,equivalent to 19% of the amount of coal in 2014;Asia's largest energy lithium metal ore deposit is found.In some parts of Yangtze River economic zone,there are some major geological problems such as active faults,karst collapse,ground subsidence,landslide-collapse-debris flow,affecting the river-crossing channels,high-speed railway,urban agglomeration and green ecological corridor planning and construction.Those problems should be concerned,and the relevant suggestions and countermeasures are put forward.Meanwhile,the ideas to further support the development of the Yangtze River economic zone are put forward. 展开更多
关键词 The Yangtze River economic zone Resources and environment CONDITIONS MAJOR geological problems Environmental GEOLOGY HYDROGEOLOGY Disaster GEOLOGY
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郯庐断裂带张八岭隆起南段肥东群石榴角闪岩变质P-T演化史对其构造属性的制约 被引量:21
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作者 石永红 朱光 王道轩 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第12期3335-3345,共11页
通过对张八岭隆起南端肥东群中磁铁石榴铁闪石岩的岩相学、矿物成分分析和热力学评价,并结合野外地质填图和共生围岩分析表明,该岩石经历了5期变质作用,展现了顺时针的P-T演化特征,早期阶段表现为近等压升温,晚期阶段为降温降压的过程,... 通过对张八岭隆起南端肥东群中磁铁石榴铁闪石岩的岩相学、矿物成分分析和热力学评价,并结合野外地质填图和共生围岩分析表明,该岩石经历了5期变质作用,展现了顺时针的P-T演化特征,早期阶段表现为近等压升温,晚期阶段为降温降压的过程,其峰期变质平均P-T条件为:524℃和0.49GPa。结合地质背景和郯庐断裂带的演化特征分析,早期过程可能反映的扬子基底所经历的区域变质过程,晚期过程可能是由于郯庐断裂的后期抬升分量所致,不具有造山带的P-T演化特征。对比前人对宿松群的变质演化历史的研究,肥东群和宿松群峰期变质压力差可达0.8GPa,表明两者属于不同变质级别的块体。因而,肥东群和宿松群不能作为被郯庐断裂左行错开的标志层。由此表明,张八岭隆起南段所出露的肥东群变质杂岩,属于扬子板块上的变质基底,郯庐断裂带活动中将其剥露地表,并没有经历过大别造山带的变质作用。 展开更多
关键词 influence fault zone temperature and PRESSURE analysis late stage 宿 belong to southern TERRAIN peak PRESSURE
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大陆造山运动:从大洋俯冲到大陆俯冲、碰撞、折返的时限--以北祁连山、柴北缘为例 被引量:104
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作者 宋述光 牛耀龄 +1 位作者 张立飞 张贵宾 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第9期2067-2077,共11页
北祁连山和柴北缘是典型的早古生代大陆造山带,分别发育有北祁连山大洋型俯冲缝合带和柴北缘大陆型俯冲碰撞带。作为早古生代大洋冷俯冲的典型代表,北祁连山经历了从新元古代-寒武纪大洋扩张、奥陶纪俯冲和闭合及早泥盆世隆升造山的过... 北祁连山和柴北缘是典型的早古生代大陆造山带,分别发育有北祁连山大洋型俯冲缝合带和柴北缘大陆型俯冲碰撞带。作为早古生代大洋冷俯冲的典型代表,北祁连山经历了从新元古代-寒武纪大洋扩张、奥陶纪俯冲和闭合及早泥盆世隆升造山的过程。高压变质岩变质年龄为490~440Ma,证明古祁连洋经历了至少50m.y.的俯冲过程。柴北缘超高压变质带是大陆深俯冲的结果,岩石学、地球化学和同位素年代学表明,柴北缘超高压变质带中榴辉岩的原岩分别来自洋壳和陆壳两种环境。高压/超高压变质的蛇绿岩原岩的年龄为517±11Ma,与祁连山蛇绿岩年龄一致。榴辉岩早期的变质年龄为443~473Ma,与祁连山高压变质年龄一致,代表大洋地壳俯冲的时代,而柯石英片麻岩和石榴橄榄岩所限定的超高压变质时代为420~426Ma,代表大陆俯冲的年龄。从大洋俯冲结束到大陆俯冲最大深度的转换时间最少需要20m.y.。自420Ma起,俯冲的大洋岩石圈与跟随俯冲的大陆岩石圈断离,大陆地壳开始折返,发生隆升和造山。北祁连山和柴北缘两个不同类型的高压-超高压变质带反映了早古生代从大洋俯冲到大陆俯冲、隆升折返的造山过程。 展开更多
关键词 Time HP-UHP North Qilian suture zone Early Paleozoic CONTINENTAL deep subduction CONTINENTAL collision building stage
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广东南昆山A型花岗岩定年和环带云母研究 被引量:23
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作者 刘昌实 陈小明 +2 位作者 王汝成 张文兰 胡欢 《地质论评》 CAS CSCD 北大核心 2005年第2期193-200,i002,共9页
广东南昆山 A型花岗岩出露面积约 2 0 0 km2 ,中粒等粒结构、块状构造 ,由铁叶云母、钠长石、微斜条纹长石和石英组成。弱过铝质 ,强亚碱质 ,富氟 (5 5 36× 1 0 - 6 ~ 90 5 4× 1 0 - 6 )贫氯 ,高的锆石饱和温度 (81 0~ 84 7... 广东南昆山 A型花岗岩出露面积约 2 0 0 km2 ,中粒等粒结构、块状构造 ,由铁叶云母、钠长石、微斜条纹长石和石英组成。弱过铝质 ,强亚碱质 ,富氟 (5 5 36× 1 0 - 6 ~ 90 5 4× 1 0 - 6 )贫氯 ,高的锆石饱和温度 (81 0~ 84 7℃ ) ,高 1 0 4 Ga/ Al比值 (4.37~ 7.2 6 )和高 Zr+Nb+Ce+Y含量 (45 0× 1 0 - 6 ~ 5 85× 1 0 - 6 )等 ,均与澳大利亚铝质 A型花岗岩相似。岩石内普遍发育环带云母 ,电子探针分析表明 ,复杂环带云母通常由若干黑云母条带 (铁叶云母 )和白云母条带组成 ,可识别出 3个构成部分 :核部带 ,幔部带和边部带。核部带形成于原岩浆处在深位时结晶的 ,幔部带形成于岩浆自深位快速上升到浅位时结晶的 ,而边部带形成在岩浆冷凝终结时。它们之间不同的边界形态说明了岩浆经历过铁钛氧化物的分离结晶作用、外来岩浆注入作用和去气作用等。环带云母是岩浆结晶历史的极好指纹。花岗岩锆石 U- Pb定年为 1 4 7± 0 .8Ma,应为中侏罗世—晚侏罗世侵入的。 展开更多
关键词 广 A
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2004年12月26日印度尼西亚8.7级大地震构造背景的初步分析 被引量:12
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作者 徐杰 高祥林 +1 位作者 陈国光 周本刚 《地震地质》 EI CSCD 北大核心 2005年第2期324-331,共8页
2004年12月26日印度尼西亚西北近海8.7级大地震,是一次浅源的海沟俯冲型板间地震。震中位于印尼-美拉尼西亚板块边界构造带的西北端,2004年沿该带发生的8次M≥7地震显示总体由东向西迁移的特征,表明它们具有相互联系的统一动力过程。这... 2004年12月26日印度尼西亚西北近海8.7级大地震,是一次浅源的海沟俯冲型板间地震。震中位于印尼-美拉尼西亚板块边界构造带的西北端,2004年沿该带发生的8次M≥7地震显示总体由东向西迁移的特征,表明它们具有相互联系的统一动力过程。这些板间地震的发生与该地处于几个板块汇聚地带和较大的板块运动速率有关,它们导致了强烈而复杂的构造变形和构造活动。印度洋-澳大利亚板块向东南亚陆块的低角度俯冲,在俯冲带浅部形成积累应变能的巨大闭锁区,它的突然破裂和大尺度滑动是造成印尼8.7级大地震的直接原因。 展开更多
关键词 200412 西 西
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大港歧口沿岸带前第三系构造体系探讨 被引量:6
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作者 郝银全 潘懋 +1 位作者 常毓文 谢培工 《地球学报》 EI CAS CSCD 北大核心 2005年第3期223-228,共6页
大港歧口沿岸带位于太行山基底和鲁西基底接触的断裂带上———聊兰断裂北延段,沿海岸线呈NNE向展布。该带不仅是一个地理界线,而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。本文从分析区域构造背景入手,详细探... 大港歧口沿岸带位于太行山基底和鲁西基底接触的断裂带上———聊兰断裂北延段,沿海岸线呈NNE向展布。该带不仅是一个地理界线,而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。本文从分析区域构造背景入手,详细探讨了该带前第三系构造体系特征及其形成和演化过程。大港歧口沿岸带前第三系雁列褶皱带在平面上是由一系列NE向左阶排列的褶皱组成的左阶雁列构造,垂向上具有正花状断裂组合特征;是在印支期NEE向大型舒缓隆起的背景上,受燕山早期(晚三叠世到中侏罗世)深断裂的左旋压扭作用和燕山晚期的走滑作用形成,并在后期受到了喜马拉雅期伸展裂陷作用的强烈改造。 展开更多
关键词 沿 线 西
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Assessing fracturing mechanisms and evolution of excavation damaged zone of tunnels in interlocked rock masses at high stresses using a finitediscrete element approach 被引量:11
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作者 I.Vazaios N.Vlachopoulos M.S.Diederichs 《Journal of Rock Mechanics and Geotechnical Engineering》 SCIE CSCD 2019年第4期701-722,共22页
Deep underground excavations within hard rocks can result in damage to the surrounding rock mass mostly due to redistribution of stresses.Especially within rock masses with non-persistent joints,the role of the pre-ex... Deep underground excavations within hard rocks can result in damage to the surrounding rock mass mostly due to redistribution of stresses.Especially within rock masses with non-persistent joints,the role of the pre-existing joints in the damage evolution around the underground opening is of critical importance as they govern the fracturing mechanisms and influence the brittle responses of these hard rock masses under highly anisotropic in situ stresses.In this study,the main focus is the impact of joint network geometry,joint strength and applied field stresses on the rock mass behaviours and the evolution of excavation induced damage due to the loss of confinement as a tunnel face advances.Analysis of such a phenomenon was conducted using the finite-discrete element method (FDEM).The numerical model is initially calibrated in order to match the behaviour of the fracture-free,massive Lac du Bonnet granite during the excavation of the Underground Research Laboratory (URL) Test Tunnel,Canada.The influence of the pre-existing joints on the rock mass response during excavation is investigated by integrating discrete fracture networks (DFNs) of various characteristics into the numerical models under varying in situ stresses.The numerical results obtained highlight the significance of the pre-existing joints on the reduction of in situ rock mass strength and its capacity for extension with both factors controlling the brittle response of the material.Furthermore,the impact of spatial distribution of natural joints on the stability of an underground excavation is discussed,as well as the potentially minor influence of joint strength on the stress induced damage within joint systems of a non-persistent nature under specific conditions.Additionally,the in situ stress-joint network interaction is examined,revealing the complex fracturing mechanisms that may lead to uncontrolled fracture propagation that compromises the overall stability of an underground excavation. 展开更多
关键词 EXCAVATION damaged zone (EDZ) BRITTLE failure Finite-discrete element method (FDEM) TUNNELLING DISCRETE fracture network (DFN)
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A novel strategy of smart manipulation by micro-scale oscillatory networks of the reactionary zones for enhanced extreme thrust control of the next-generation solid propulsion systems
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作者 Alexander N.Lukin 《Defence Technology(防务技术)》 SCIE EI CAS CSCD 2018年第5期635-642,共8页
The main aim of this research is to get a better knowledge and understanding of the micro-scale oscillatory networks behavior in the solid propellants reactionary zones. Fundamental understanding of the micro-and nano... The main aim of this research is to get a better knowledge and understanding of the micro-scale oscillatory networks behavior in the solid propellants reactionary zones. Fundamental understanding of the micro-and nano-scale combustion mechanisms is essential to the development and further improvement of the next-generation technologies for extreme control of the solid propellant thrust. Both experiments and theory confirm that the micro-and nano-scale oscillatory networks excitation in the solid propellants reactionary zones is a rather universal phenomenon. In accordance with our concept,the micro-and nano-scale structures form both the fractal and self-organized wave patterns in the solid propellants reactionary zones. Control by the shape, the sizes and spacial orientation of the wave patterns allows manipulate by the energy exchange and release in the reactionary zones. A novel strategy for enhanced extreme thrust control in solid propulsion systems are based on manipulation by selforganization of the micro-and nano-scale oscillatory networks and self-organized patterns formation in the reactionary zones with use of the system of acoustic waves and electro-magnetic fields, generated by special kind of ring-shaped electric discharges along with resonance laser radiation. Application of special kind of the ring-shaped electric discharges demands the minimum expenses of energy and opens prospects for almost inertia-free control by combustion processes. Nano-sized additives will enhance self-organizing and self-synchronization of the micro-and nano-scale oscillatory networks on the nanometer scale. Suggested novel strategy opens the door for completely new ways for enhanced extreme thrust control of the solid propulsion systems. 展开更多
关键词 Solid propulsion systems EXTREME thrust control Reactionary zoneS MICRO-SCALE OSCILLATORY NETWORKS Self-organized wave patterns Energy-releasing areas
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北大别超高压榴辉岩的快速折返与缓慢冷却过程 被引量:8
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作者 刘贻灿 古晓锋 李曙光 《岩石学报》 SCIE EI CAS CSCD 北大核心 2009年第9期2149-2156,共8页
岩石学研究表明,北大别超高压榴辉岩经过了超高压和高压榴辉岩相变质作用以及麻粒岩相叠加和角闪岩相退变质作用。其中,高压麻粒岩相和角闪岩相变质阶段形成的后成合晶以及石榴子石和单斜辉石等矿物中成分分带的存在,证明该区榴辉岩经... 岩石学研究表明,北大别超高压榴辉岩经过了超高压和高压榴辉岩相变质作用以及麻粒岩相叠加和角闪岩相退变质作用。其中,高压麻粒岩相和角闪岩相变质阶段形成的后成合晶以及石榴子石和单斜辉石等矿物中成分分带的存在,证明该区榴辉岩经历了一个快速折返过程;而不同变质阶段的温度、压力和形成时代,却反映该区榴辉岩在峰期超高压变质作用之后又经历了一个缓慢冷却过程。超高压岩石折返期间的缓慢冷却过程也许正是北大别长期难以发现柯石英和有关超高压证据的重要原因。因此,本文为大别山不同超高压岩片的差异折返模型的建立提供了新的证据。 展开更多
关键词 the NORTH Dabie complex South China UHP metamorphism temperature and pressure garnet and CLINOPYROXENE CONTINENTAL collision CONTINENTAL crust rapid exhumation UHP eclogites NORTH China 退
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