|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Temporal and regional variations of China's fertilizer consumption by crops during 1998-2008显示文摘The agricultural and land policies in China are always focused on protecting its food supply and security because of the country's large population and improved diets.The crop production guide 'Take Grain as the Key Link' prompted peasants to plant grain on most of the agricultural land,leading to the majority of fertilizer being used in grain crops for many years in China.This situation has changed dramatically in recent years.Based on data pertaining to provincial crops sown area and fertilizer use per unit area in 1998 and 2008,the temporal and spatial variations of China's fertilizer consumption by crops were analyzed at the provincial level,and the results are presented here.(1) Fertilizer consumption in China grew strongly in the last decade,while the growth was mainly attributable to the increase of fertilizer con-sumption by horticultural crops.The fertilizer consumption of grain crops dropped from 71.0% in 1998 to 57.8% in 2008.Thus,it is concluded that the emphasis of fertilizer consumption is shifting toward horticultural crops.(2) There were marked differences in the growth rates of fertilizer consumption from the regional point of view.The national average growth rate of fertilizer consumption was 31.9% during 1998-2008.The western and northeastern parts of the country came close to the national average,while the eastern part was lower,with an average of 13.0%,and central China was much higher(50.8%).The increase of fertilizer consumption in central and west China was higher than the other zones,which already ac-counted for 77.9% of the national total.Thus,it is concluded that the consumption emphasis of chemical fertilizer shifts toward the central and western regions.(3) The decline of fertilizer consumption by grain crops was largely due to the decrease in sown area compared with the increase by vegetable crops attributable to the enlarging sown area;the increase by orchard crops was affected by both expanding the sown area and fertilizer use per unit area. | XIN Liangjie LI Xiubin TAN Minghong | 2012 | Journal of Geographical Sciences2012，22，4： | 49 |
| 2 | China’s Potential of Grain Production Due to Changes in Agricultural Land Utilization in Recent Years显示文摘The changes in utilization of agricultural land have gradually grown into one of the major factors impacting grain output in China. This study explores the various components of agricultural production in China from the land utilization perspective, involving changes in grain production per unit area, multi-cropping index, and adjustment of agricultural structure. Compared with the record values, different research methodologies are used to analyze the po- tential of above three components. The results indicate that grain production potential of 65.68×109kg was unexploited in 2006, in which 45.8×109kg came from the restructuring in agriculture. So we can infer that the reduction of grain production in China could be primarily attributed to agricultural restructuring in recent years. So the productive poten- tial can be fully restored by increasing agricultural investment, or recovering agricultural structure in favorable condi- tions. So we can say that China’s current condition of food security is good. | XIN Liangjie LI Xiubin ZHU Huiyi TAN Minghong | 2009 | Chinese Geographical Science2009，19，2： | 19 |
| 3 | Differential responses of short-term soil respiration dynamics to the experimental addition of nitrogen and water in the temperate semi-arid steppe of Inner Mongolia, China显示文摘We examined the effects of simulated rainfall and increasing N supply of different levels on CO2 pulse emission from typical Inner Mongolian steppe soil using the static opaque chamber technique, respectively in a dry June and a rainy August. The treatments included NH4NO3 additions at rates of 0, 5, 10, and 20 g N/(m2·year) with or without water. Immediately after the experimental simulated rainfall events, the CO2 effluxes in the watering plots without N addition(WCK) increased greatly and reached the maximum value at 2 hr. However, the efflux level reverted to the background level within 48 hr. The cumulative CO2 effluxes in the soil ranged from 5.60 to 6.49 g C/m2over 48 hr after a single water application, thus showing an increase of approximately 148.64% and 48.36% in the effluxes during both observation periods. By contrast, the addition of different N levels without water addition did not result in a significant change in soil respiration in the short term. Two-way ANOVA showed that the effects of the interaction between water and N addition were insignificant in short-term soil CO2 effluxes in the soil. The cumulative soil CO2fluxes of different treatments over 48 hr accounted for approximately 5.34% to 6.91% and 2.36% to 2.93% of annual C emission in both experimental periods. These results stress the need for improving the sampling frequency after rainfall in future studies to ensure more accurate evaluation of the grassland C emission contribution. | Yuchun Qi Xinchao Liu Yunshe Dong Qin Peng Yating He Liangjie Sun Junqiang Jia Congcong Cao | 2014 | Journal of Environmental Sciences2014，26，4： | 17 |
| 4 | Litter decomposition and C and N dynamics as affected by N additions in a semi-arid temperate steppe, Inner Mongolia of China显示文摘Litter decomposition is the fundamental process in nutrient cycling and soil carbon(C) sequestration in terrestrial ecosystems. The global-wide increase in nitrogen(N) inputs is expected to alter litter decomposition and,ultimately, affect ecosystem C storage and nutrient status. Temperate grassland ecosystems in China are usually N-deficient and particularly sensitive to the changes in exogenous N additions. In this paper, we conducted a 1,200-day in situ experiment in a typical semi-arid temperate steppe in Inner Mongolia to investigate the litter decomposition as well as the dynamics of litter C and N concentrations under three N addition levels(low N with 50 kg N/(hm2?a)(LN), medium N with 100 kg N/(hm2?a)(MN), and high N with 200 kg N/(hm2?a)(HN)) and three N addition forms(ammonium-N-based with 100 kg N/(hm2?a) as ammonium sulfate(AS), nitrate-N-based with 100 kg N/(hm2?a) as sodium nitrate(SN), and mixed-N-based with 100 kg N/(hm2?a) as calcium ammonium nitrate(CAN)) compared to control with no N addition(CK). The results indicated that the litter mass remaining in all N treatments exhibited a similar decomposition pattern: fast decomposition within the initial 120 days, followed by a relatively slow decomposition in the remaining observation period(120–1,200 days). The decomposition pattern in each treatment was fitted well in two split-phase models, namely, a single exponential decay model in phase I(<398 days) and a linear decay function in phase II(≥398 days). The three N addition levels exerted insignificant effects on litter decomposition in the early stages(<398 days, phase I; P>0.05). However, MN and HN treatments inhibited litter mass loss after 398 and 746 days, respectively(P<0.05). AS and SN treatments exerted similar effects on litter mass remaining during the entire decomposition period(P>0.05). The effects of these two N addition forms differed greatly from those of CAN after 746 and 1,053 days, respectively(P<0.05). During the decomposition period, N concentrations in the decomposing litter increased whereas C concentrations decreased, which also led to an exponential decrease in litter C:N ratios in all treatments. No significant effects were induced by N addition levels and forms on litter C and N concentrations(P>0.05). Our results indicated that exogenous N additions could exhibit neutral or inhibitory effects on litter decomposition, and the inhibitory effects of N additions on litter decomposition in the final decay stages are not caused by the changes in the chemical qualities of the litter, such as endogenous N and C concentrations. These results will provide an important data basis for the simulation and prediction of C cycle processes in future N-deposition scenarios. | Qin PENG YuChun QI YunShe DONG YaTing HE ShengSheng XIAO XinChao LIU LiangJie SUN JunQiang JIA ShuFang GUO CongCong CAO | 2014 | Journal of Arid Land2014，6，4： | 16 |
| 5 | Impact of the shrinking winter wheat sown area on agricultural water consumption in the Hebei Plain显示文摘这研究第一分析了冬季小麦的收缩和基于 11 个城市的农业统计数据和气象学的数据从 1998~2010 在 Hebei 平原收割系统的变化,包括每日的温度, 降水,水蒸汽,来自 22 个气象学的车站的风速度和最小的相对湿度数据,然后计算了水赤字,灌溉水资源由不同收割要求系统,以及灌溉浇是保存的资源一结果如下。1 ) 在都在学习时期期间缩小的 Hebei 平原的 11 个城市里的冬季小麦的播种区域。收缩率是16.07%,全部的收缩区域等于离子的液体是的 49.62f 10wt%( 0.1 g 离子的液体/ 1 g 活跃的碳搬运人)并且Pd2+的理论内容是5wt%( 0.05 g Pd2+/ 1 g 活跃的碳搬运人),吗最高催化的活动 2 963.64 gSTCO/( gPd 訐?訐?? | WANG Xue LI Xiubin XIN Liangjie | 2014 | Journal of Geographical Sciences2014，24，2： | 16 |
| 6 | Thick-skinned Contractional Salt Structures in the Kuqa Depression,the Northern Tarim Basin:Constraints from Physical Experiments显示文摘摘要:脸皮厚的 contractional 盐结构广泛地在西方的 Kuqa 消沉被开发,北 Tarim 盆。为了理解管理这些的发展的机制,组织,物理实验被进行,结果证明他们被地下室差错并且形成 paleo 高举和地下室斜坡的活动大部分管理。在这研究的模型材料是干燥的沙,矿脂和 plasticene (或难泡沫) ,分别地模仿 suprasalt,盐,和 subsalt 层。实验证明由于地下室差错并且形成 paleo 高举的活动,盐身体通常在被预先退出的边界差错抑制的 paleo 高举的中间的顶上显著地积累并且变厚。大规模戳差错和盐越过水坝落下的水的发展被地下室赞成与更大的剧降泼出。实验也断定因为盐层的存在,那微分结构的变丑能发生在 subsalt 和 suprasalt 层之间。他们的几何学和结构的高度的地点是不同的,尽管有高举的区域的大类似。穿透的盐挤入构造没在实验被观察,它显示弄短的 contractional 有效地不加速盐挤入构造的发展。 | YU Yixin TANG Liangjie YANG Wenjing JIN Wenzheng PENG Gengxin LEI Ganglin | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 15 |
| 7 | Effects of a conversion from grassland to cropland on the different soil organic carbon fractions in Inner Mongolia, China显示文摘耕作是除放牧以外影响草地生态系统的最重要的人的活动之一,但是它土壤上的影响总计器官的碳(C) ,特别在有倾向的器官的 C 部分上还充分没被理解。在这份报纸,在土壤收割不同部分的器官的 C 水池的角色在中国,和在不同 C 部分之间的关系的内部蒙古在一个草地大草原区域被调查也被讨论。结果显示在大草原和栽培土地的不同 C 部分的集中都与土壤深度日益增多地减少了。在到为 36 年的春天小麦地的从大草原的变换以后,在 0~100 厘米土壤深度的全部的器官的碳( TOC )集中在12.3%~28.2%减少了,并且表面土壤地平线的 TOC ,特别那些更显著地 030 厘米减少了( p < 0.01 )。溶解的器官的碳(文档) 和在 040 厘米的深度的微生物引起的生物资源碳(MBC ) 被发现分别地在 66.7% ~ 77.1% 和 36.5% ~ 42.4% 减少了。在 S。baicalensis 大草原,春天小麦地里的到 TOC 的文档在 0.52% 和 0.60% 之间改变了的土壤的比率,和那些仅仅在 0.18%0.20% 的范围。在春天小麦的微生物引起的商(qMBs ) 回答,从 1.11% ~ 1.40% 变化,也是比在 S 的那些低的。baicalensis 大草原,它在 1.50%1.63% 的范围。文档的变化对耕作骚乱更敏感。土壤 TOC,文档,和 MBC 是显著地积极的在 S 与对方一起相关。baicalensis 大草原,但是在春天小麦地里,在文档之间的相互关系和在文档和 MBC 之间的 TOC 和那没到达 0.05 的意义水平。 | QI Yuchun DONG Yunshe PENG Qin XIAO Shengsheng HE Yating LIU Xinchao SUN Liangjie JIA Junqiang YANG Zhijie | 2012 | Journal of Geographical Sciences2012，22，2： | 13 |
| 8 | PKM2 coordinates glycolysis with mitochondrial fusion and oxidative phosphorylation显示文摘A change in the metabolic flux of glucose from mitochondrial oxidative phosphorylation (OXPHOS) to aerobic glycolysis is regarded as one hallmark of cancer. However, the mechanisms underlying the metabolic switch between aerobic glycolysis and OXPHOS are unclear. Here we show that the M2 isoform of pyruvate kinase (PKM2), one of the rate-limiting enzymes in glycolysis, interacts with mitofusin 2 (MFN2), a key regulator of mitochondrial fusion, to promote mitochondrial fusion and OXPHOS, and attenuate glycolysis. mTOR increases the PKM2:MFN2 interaction by phosphorylating MFN2 and thereby modulates the effect of PKM2: MFN2 on glycolysis, mitochondrial fusion and OXPHOS. Thus, an mTOR-MFN2-PKM2 signaling axis couples glycolysis and OXPHOS to modulate cancer cell growth. | Tong Li Jinbo Han Liangjie Jia Xiao Hu Liqun Chen Yiguo Wang | 2019 | Protein & Cell2019，10，8： | 10 |
| 9 | Tectonic Evolution of the Middle Frontal Area of the Longmen Mountain Thrust Belt,Western Sichuan Basin,China显示文摘由分析平衡的生气的节和 Longmen 山戳带的沉淀历史,中国,我们断定它经历了五个构造阶段:(1 ) 形成阶段(T 3 x ) Longmen 的缩影,山,早 Indosinian 运动,和 Anxian 构造运动创造了 Longmen 山;(2 ) 稳定的构造阶段(更弱的构造运动导致了 Longmen 山戳带的 J 1) 稍微正在被高举并且稍微减退低岬盆;(3 ) 强烈构造阶段(J2.3 ) ,也就是早 Yanshan 运动;(4 ) 连续构造运动(K-E ) ,也就是迟了的 Yanshan 运动和早喜玛拉雅的运动;并且(5 ) Longmen 山(N-Q ) 的形成,也就是晚喜玛拉雅的运动。在那些构造变丑阶段期间, Anxian 运动和喜玛拉雅的运动在 Longmen 山的形成起了重要作用。喜玛拉雅的运动影响了 Longmen 山大多数;阶层强烈地推进了并且严重地被侵蚀。因为一些越过水坝落下的水被推,在 Longmen 山戳带的中间的部分有某 klippes 在以后向东南构造变丑。 | JIN Wenzheng TANG Liangjie YANG Keming WAN Guimei Lü Zhizhou YU Yixin | 2009 | Acta Geologica Sinica(English Edition)2009，83，1： | 10 |
| 10 | Realization Methodology of a 5-axis Spline Interpolator in an Open CNC System显示文摘由使用不一致的合理B花键( NURBS )曲线的优点代表空间曲线,有对5轴合适的两倍 NURBS 曲线的一种说明格式协调了即时插值被介绍代替当前的5轴协调线性插值方法有缺陷者在低速度,在 sculptured 的低精确性、庞大的数字控制( NC )文件出现用机器制造。有介绍格式的 NC 文件的一个产生过程被介绍并且在一台开的计算机认识到插值的方法数字控制(计算机数值控制) 系统自己被开发。这些说明了建议方法和它避免 5 轴的所有缺乏的能力的可行性线性插值方法。 | Wang Yongzhang Ma Xiongbo Chen Liangji Han Zhenyu | 2007 | Chinese Journal of Aeronautics2007，20，4： | 10 |
| 11 | Spatial Characteristics and Controlling Factors of the Strikeslip Fault Zones in the Northern Slope of Tazhong Uplift, Tarim Basin: Insight from 3D Seismic Data显示文摘The detailed characteristics of the Paleozoic strike-slip fault zones developed in the northern slope of Tazhong uplift are closely related to hydrocarbon explorations. In this study, five major strike-slip fault zones that cut through the Cambrian-Middle Devonian units are identified, by using 3D seismic data. Each of the strike-slip fault zones is characterized by two styles of deformation, namely deeper strike-slip faults and shallower en-echelon faults. By counting the reverse separation of the horizon along the deeper faults, activity intensity on the deeper strike-slip faults in the south is stronger than that on the northern ones. The angle between the strike of the shallower en-echelon normal faults and the principal displacement zone(PDZ) below them is likely to have a tendency to decrease slightly from the south to the north, which may indicate that activity intensity on the shallower southern en-echelon faults is stronger than that on the northern ones. Comparing the reverse separation along the deeper faults and the fault throw of the shallower faults, activity intensity of the Fault zone S1 is similar across different layers, while the activity intensity of the southern faults is larger than that of the northern ones. It is obvious that both the activity intensity of the same layer in different fault zones and different layers in the same fault zone have a macro characteristic in that the southern faults show stronger activity intensity than the northern ones. The Late Ordovician décollement layer developed in the Tazhong area and the peripheral tectonic events of the Tarim Basin have been considered two main factors in the differential deformation characteristics of the strike-slip fault zones in the northern slope of Tazhong uplift. They controlled the differences in the multi-level and multi-stage deformations of the strike-slip faults, respectively. In particular, peripheral tectonic events of the Tarim Basin were the dynamic source of the formatting and evolution of the strike-slip fault zones, and good candidates to accommodate the differential activity intensity of these faults. | HAN Xiaoying TANG Liangjie DENG Shang CAO Zicheng | 2020 | Acta Geologica Sinica(English Edition)2020，94，2： | 9 |
| 12 | Hydrothermal Synthesis and Thermal Decomposition Mechanism of Alkaline Earth Benzoates显示文摘0IntroductionAlkalineearthbenzoatesareakindofstablecompound.Thecoordinationcompoundsformedbyalkalineearthandcarboxylicacidsha... | Zhang, Keli Yuan, Jibing Yuan, Liangjie Sun, Jutang | 1999 | Wuhan University Journal of Natural Sciences1999，4，1： | 9 |
| 13 | Spatial and Temporal Variability of Farm Size in China in Context of Rapid Urbanization显示文摘During the last 30 years,China has witnessed rapid economic growth and dramatic urbanization,with about 1.2 × 107rural people migrating annually into urban areas.Meanwhile,especially since 1995,the rural population has been declining,which is closely linked to land circulation and the increase in farm size in many villages.Increasing scale of farming operations is often regarded as a key to avoiding the abandonment of farmland and to increasing the income of rural farmers.However,until now,there has been little research on the spatial and temporal variability of farm size at the national level in China.Using data from the national agricultural census and rural household surveys,this study examines the characteristics of land use circulation and the consequent changes in the area of farmland per household.The results show that: 1) 12.2% of rural households were involved in land circulation at the national level.The highest amounts of land circulation have occurred in those provinces where the farmland per capita is more than 0.2 ha or less than 0.1 ha;2) over 80% of households operate less than 0.6 ha of farmland;3) the proportion of mid-sized farms(between 0.2 ha and 0.6 ha per household) has decreased while the smallest and the largest farms have increased.This bears some similarity with the phenomenon known as the ′disappearing middle′,referring to the changes in farm size.This study establishes a framework for interpreting the factors affecting the changes in farm size in China,which include two promoting factors(urbanization and agriculture) and four hindering factors(agricultual land system,household registration,stable clan system,and farmland loss). | TAN Minghong Guy M ROBINSON LI Xiubin XIN Liangjie | 2013 | Chinese Geographical Science2013，23，5： | 8 |
| 14 | Opposite effects of nitrogen fertilization and plastic film mulching on crop N and P stoichiometry in a temperate agroecosystem显示文摘Aims Crop nitrogen(N)and phosphorus(P)stoichiometry can influence food nutritive quality and many ecosystem processes.However,how and why N and P stoichiometry respond to long-term agricul-tural management practices(e.g.N fertilization and film mulching)are not clearly understood.Methods We collected maize tissues(leaf,stem,root and seed)and soil sam-ples from a temperate cropland under 30-year continuous N fer-tilization and plastic film mulching treatments,measured their C,N and P concentrations(the proportion(%)relative to the sample mass),and used structural equation models to uncover the re-sponding mechanisms for crop N and P contents(the total amount(g/m2)in crop biomass).Important Findings Long-term N fertilization increased N concentrations in all crop tissues but sharply decreased P concentrations in vegetative tis-sues(leaf,stem and root),thereby reducing their C/N ratio and increasing C/P and N/P ratios.The drop in P concentration in vegetative tissues was due to the dilution effect by biomass in-crement and the priority of P supply for seed production.In con-trast,film mulching decreased N concentration but increased P concentrations in most crop tissues,thereby increasing C/N ratio and reducing C/P and N/P ratios.Film mulching increased crop P content by increasing soil temperature and moisture;whereas,mulching showed little effect on crop N content,because a posi-tive effects of soil temperature may have canceled out a negative effect by soil moisture.This indicated a decoupling of P and N uptake by crops under film mulching.In conclusion,N fertiliza-tion and plastic film mulching showed opposite effects of on crop N and P stoichiometry. | Fan Ding Shuangyi Li Xiao-Tao Lü Feike A.Dijkstra Sean Schaeffer Tingting An Jiubo Pei Liangjie Sun Jingkuan Wang | 2019 | Journal of Plant Ecology2019，12，4： | 8 |
| 15 | Intelligent Flow Control Technique of ABR Service in ATM Networks Based on Fuzzy Neural Networks显示文摘InteligentFlowControlTechniqueofABRServiceinATMNetworksBasedonFuzzyNeuralNetworks①ZhangLiangjieLiYandaLiQinghuaWangPu(DeptofA... | Zhang Liangjie Li Yanda Li Qinghua Wang Pu (Dept of Automation, Tsinghua University, Beijing 100084) | 1997 | 通信学报1997，18，3： | 7 |
| 16 | Fault Systems and Their Mechanisms of the Formation and Distribution of the Tarim Basin,NW China显示文摘This article aims to analyze the main controlling factors of development,distribution and evolution of the fault systems in the Tarim Basin.Based on the seismic profile interpretation,comprehensive analysis of the drilling and geologic data,six fault systems maybe recognized in the Tarim Basin,they are the foreland fault system of the South Tianshan Mountain,the northern Tarim uplift fault system,North Tarim depression fault system,central fault system,Southwest Tarim fault system,and Southeast Tarim fault system.It is indicated that the main differences exist at the development,evolution and distribution of the fault systems in the Tarim Basin.The sub-fault systems can be recognized according to the differences of the fault development and distribution in the interior of the fault system.It is characterized that the multi-level differential development and distribution of the fault systems exist in the Tarim Basin.The fault belt developed in the Paleozoic strata mainly distribute at the paleo-uplift and paleo-slope in the interior of the Tarim Basin,and the fault belt occurred in the Meso–Cenozoic beds mainly develop at the peripheral foreland depressions.Zonal and segment differential development and distribution of the fault systems also exist in the Tarim Basin.The formation and distribution of the Tarim fault systems is of complex controlling mechanisms.Poly-phase structural movement and tectonic transition controls the multi-phase differential development and distribution of the fault systems in the Tarim Basin.Multi-level differential development and distribution is controlled by multi-level detachment belt and regional unconformities.Zonal and segment differential development and distribution of the Tarim fault systems maybe controlled by pre-existed basement structural texture.The major direction of the fault systems in the Tarim Basin is controlled by the later stage basin-mountain coupling. | Liangjie Tang Taizhu Huang Haijun Qiu Guimei Wan Meng Li Yong Yang Daqing Xie Gang Chen | 2014 | Journal of Earth Science2014，25，1： | 6 |
| 17 | Hierarchical MoS2 intercalated clay hybrid nanosheets with enhanced catalytic activity显示文摘新兴的层次瞬间 2/pillared-montmorillonite (瞬间 2/PMMT) 混血儿 nanosheets 成功地在 cetyltrimethylammonium 溴化物 PMMT 的夹层以内通过瞬间 2 的灵巧的在原处热水的合成被准备,并且他们的催化表演被 4-nitrophenol (4-NP ) 的减小反应作为 reductant 用 NaBH 4 评估。微观结构和形态学描述显示瞬间 2/PMMT 与 1.29 nm,和瞬间 2 nanosheets 的夹层间距展出了叠混血儿的分层的结构在 montmorillonite (MMT ) 以内被设置层,与大多数暴露于外面的边。瞬间 2/PMMT 的催化活动和稳定性被 MMT 两个都提高。与是的瞬间 2/PMMT 催化剂, 4-NP 减小的明显的反应率常数是 0.723 min 1 并且在 ~ 被维持在五反应以后的 0.679 min 1 骑车。为 4-NP 的减小反应的瞬间 2/PMMT 和可能的催化作用机制的结构的进化被调查。同样准备的瞬间 2/PMMT 混血儿 nanosheets 在水处理和生物医学的域为催化申请正在答应候选人。在这研究开发的策略能为设计混合 nanosheets 与提供卓见多样异构二维(2D ) nanomaterials。 | Kang Peng Liangjie Fu Huaming Yang Jing Ouyang Aidong Tang | 2017 | Nano Research2017，10，2： | 6 |
| 18 | Polygonal faults in the Sanzhao sag of the Songliao basin:their significance in hydrocarbon accumulation显示文摘Polygonal faults,generally distributed in fine-grained sediments,are layer-bound faults and are important in hydrocarbon accumulation.Using 3D seismic data,we analyzed the plane and profile features of faults developed in the Qingshankou formation of the Sanzhao sag.We identified these faults as having typical features of polygonal faults:1) layer-bound;2) normal faults;3) slight fault displacements and steep in dip angles;4) multi-directional in strike and 5) a single fault has a short horizontal extension.In addition,these faults intersect each other and form polygons.These polygonal faults are the result from the combined action of compaction,volume contraction and episodic hydraulic fracturing,conditions favorable for oil/gas accumulation.They are the dominant channels for migration of fluids in the Qingshankou mudstone,forming a large number of fault-lithologic oil traps.Polygonal faults improve reservoirs. | HE, Chunbo TANG, Liangjie HUANG, Deli SHI, Shangming | 2010 | Mining Science and Technology2010，20，2： | 6 |
| 19 | Differential Tectonic Deformation of the Longmen Mountain Thrust Belt,Western Sichuan Basin,China显示文摘地调查和地震的节解释证明 Longmen 山戳带有明显的微分变丑:带状配列,分割和层化。带状配列意味着那,从 NW 到 NE, Longmen 山戳带能被划分成 Songpan-Garz ê构造的带,可锻的变丑带,基础深奥的戳带,正面的褶层戳带,和低岬消沉。它能向南向北被划分成五个片断从到的分割工具:北片断, Anxian 转移地区,中心片断, Guanxian 转移地区和南部的片断。层化意味着分开层在侧面划分结构的式样。在 Longmen 山戳带的分开层能被分类进三个范畴:深水平的分开层包括外壳披风系统分开层, intracrustal 分开层,和 Presinian 系统基础分开层;中间级的分开层包括寒武纪奥陶纪的分开层,志留纪分开层,等等;并且浅水平的分开层,包括的上面的三叠纪的 Xujiahe 形成分开层和侏罗记分开层。多水平分开层在塑造和 Longmen 山戳带的进化上有很重要的效果。 | TANG Liangjie YANG Keming JIN Wenzheng WAN Guimei LüZhizhou YU Yixin | 2009 | Acta Geologica Sinica(English Edition)2009，83，1： | 6 |
| 20 | Multi-level Detachments and Petroleum Potential of the Tarim Basin显示文摘Four detachment systems have been found in the Tarim Basin. They are made up of the Proterozoic,Palaeozoic, Mesozoic-Eogene and Neogene-Quaternary, respectively. The shallow-level detachments are char-acterized by the occurrence of fold-thrust belts in the Meso-Cenozoic. The mid-level detachments are markedby nappes, decollement folds and drag anticlines in the Palaeozoic. The deep-level detachments are representedby ductile shear belts in the basement. Mid-and deep-level detachments mainly occur in the Northern, Centraland Southern Uplifts which are major hydrocarbon accumulation belts of large-scale oil fields. Shallow-leveldetachments mainly exist in the Kuqa, Southwestern and Southeastern Depressions, which are favourable beltsfor finding medium- and small-sized oil-gas fields. | Tang Liangjie Northwest Bureau of Petroleum Geology, Ministry of Geology and Mineral Resources, Urumqi, Xinjiang | 1992 | Acta Geologica Sinica(English Edition)1992，66，4： | 6 |
您所在的机构暂未开通此部分的功能，请联系管理员