A Large-Scale Palaeozoic Dextral Ductile Strike-Slip Zone:the Aqqikkudug-Weiya Zone along the Northern Margin of the Central Tianshan Belt,Xinjiang,NW China

Abstract The nearly E-W-trending Aqqikkudug-Weiya zone, more than 1000 km long and about 30 km wide, is an important segment in the Central Asian tectonic framework. It is distributed along the northern margin of the Central Tianshan belt in Xinjiang, NW China and is composed of mylonitized Early Palaeozoic greywacke, volcanic rocks, ophiolitic blocks as a mélange complex, HP/LT-type bleuschist blocks and mylonitized Neoproterozoic schist, gneiss and orthogneiss. Nearly vertical mylonitic foliation and sub-horizontal stretching lineation define its strike-slip feature; various kinematic indicators, such as asymmetric folds, non-coaxial asymmetric macro- to micro-structures and C-axis fabrics of quartz grains of mylonites, suggest that it is a dextral strike-slip ductile shear zone oriented in a nearly E-W direction characterized by “flower” strusture with thrusting or extruding across the zone toward the two sides and upright folds with gently plunging hinges. The Aqqikkudug-Weiya zone experienced at least two stages of ductile shear tectonic evolution: Early Palaeozoic north vergent thrusting ductile shear and Late Carboniferous-Early Permian strike-slip deformation. The strike-slip ductile shear likely took place during Late Palaeozoic time, dated at 269±5 Ma by the40Ar/39Ar analysis on neo-muscovites. The strike-slip deformation was followed by the Hercynian violent S-type granitic magmatism. Geodynamical analysis suggests that the large-scale dextral strike-slip ductile shearing is likely the result of intracontinental adjustment deformation after the collision of the Siberian continental plate towards the northern margin of the Tarim continental plate during the Late Carboniferous. The Himalayan tectonism locally deformed the zone, marked by final uplift, brittle layer-slip and step-type thrust faults, transcurrent faults and E-W-elongated Mesozoic-Cenozoic basins.

Late Paleozoic Element Migration and Accumulation under Intracontinental Sinistral Strike-slip Faulting in the West Junggar Orogenic Belt, NW China

The migration,accumulation and dispersion of elements caused by tectonic dynamics have always been a focus of attention,and become the basis of tectono-geochemistry.However,the effects of faulting,especially strike-slip faulting,on the adjustment of geochemical element distribution,are still not clear.In this paper,we select the West Junggar Orogenic Belt(WJOB),NW China,as a case study to test the migration behavior of elements under tectonic dynamics.The WJOB is dominated by NE-trending large-scale sinistral strike-slip faults such as the Darabut Fault,the Mayile Fault,and the Baerluke Fault,which formed during the intracontinental adjustment under N-S compression during ocean-continental conversion in the Late Paleozoic.Geochemical maps of 13 elements,Al,W,Sn,Mo,Cu,Pb,Zn,As,Sb,Hg,Fe,Ni,and Au,are analyzed for the effects of faulting and folding on element distribution at the regional scale.The results show that the element distribution in the WJOB is controlled mainly by two mechanisms during tectonic deformation:first is the material transporting mechanism,where the movement of geological units is consistent with the direction of tectonic movement;second is the diffusion mechanism,especially by tectonic pressure dissolution driven by tectonic dynamics,where the migration of elements is approximately perpendicular or opposite to the direction of tectonic movement.We conclude that the adjustment of element distributions has been determined by the combined actions of transporting and diffusion mechanisms,and that the diffusion mechanism plays an important role in the formation of geochemical Au blocks in the WJOB.

From the Iron Curtain to the European Green Belt Creating a Vision for a 2^nd Transformation to a Life-Sustaining Europe/World

The European Green Belt developed from the wasteland of the former death strip along the iron curtain over decades to a green life line of biodiversity. It is an ecological network with a unique natural and cultural heritage, an emotional human and political history, meaning and transformative power. Due to the former border situation, it is a transnational green infrastructure with biodiversity hotspots in a more and more fragmented, intensively used and degraded European landscape and connects people from 24 European countries and valuable landscapes. But now, nearly 30 years after the peaceful transition in 1989, the gaps in the European Green Belt cover already 50%. These gaps are not protected and are subject to adverse effects, like ongoing landscape fragmentation and ongoing chemo-industrial agriculture. Alarming signals of a new death zone are not only the gaps within the European Green Belt, but generally and closely related the mass extinction of species, climate change, resource depletion, financial and economic crisis, demographic change, emigration, unemployment and/or precarious work worldwide. To save the European Green Belt and life on earth there is a great need ofa 2^nd transformation to a life-sustaining world.

Cultural Sharing, Connectivity and Road Expansion——Cultural Transformation and Anthropology Study of World Care from the Belt and Road Initiative

The era of cultural sharing marks itself mainly in the following three aspects: First, the virtual presence which bridges the world together and further broadens our horizons to observe the world in an even more extensive way. Second, the formerly stable structural relationship between peripheral regions and central regions gradually grows uncertain. Third, the establishment of cyberized roads or the cyberized expansion of roads leads the advance toward a global connectivity where the virtual world closely interacts with the real world. After "the Belt" concept comes into being, the anthropologists must upgrade their research from previously established fixed-point perspective to a more extensive observation over the "Belt" or a wider range, while the concept of "the Road" encourages anthropologists to study the culture of the other half of the world, namely, to read the world history as a whole new picture from a Chinese or eastern point of view. It is necessary for anthropology to break the geological and cultural borders in the real world to extend its antenna to a more extensive range, which will also bring the "otherness" of this field to a more prominent and obvious play. It is inevitable that all human cultures are about to take a core standing in the Belt and Road Initiative.

Theoretical Model on Transformation Factors of Scientific and Technological Achievements under the Belt and Road Initiative

With the continuous deepening of the Belt and Road Initiative,the countries involved are increasingly connected in the field of science and technology.Based on the transformation theory of scientific and technological(S&T)achievements,this study establishes a theoretical model of transformation factors of S&T achievements under the Belt and Road Initiative.Combined with the data analysis from questionnaire,it is found that in S&T achievements transformation process,there is a significant positive correlation between the innovation factors and the transfer factors,between the transfer factors and the diffusion factors,and between the diffusion factors and the transformation results.These conclusions provide reference for the subsequent S&T achievements transformation activities under the Belt and Road Initiative.Therefore,in the process of promoting the transformation of S&T achievements under the Belt and Road Initiative in the future,innovation factors such as information innovation,service innovation,and cooperative innovation should be fully reflected.Relevant agencies should take the transfer factors of S&T achievements as guidance;promote and apply the results of incubation through diffusion media and diffusion channels.

DEFINITING AND ITS GEOLOGIC MEANING OF SOUTH-NORTH TREND FAULTED STRUCTURE BELT IN QIANGTANG BASIN, NORTH PART OF TIBET

There were more expounding to north—west (west) trend fault and north\|east trend fault within Qiangtang Basin, North Part of Tibet, in the past literature. With increasing of geophysical exploration data, nearly east\|west trend structure began to be taken note to. Since the year of 1995, by a synthetic study to geophysical and geological data, that south\|north trend faulted structures are well developed. These structures should be paid much more attention to, because they have important theoretical meaning and practical significance.1 Spreading of south\|north faulted structure belt According to different geological and geophysical data, the six larger scale nearly south\|north faulted structure belt could be distinguished within the scope of east longitude 84°～96° and near Qiangtang Basin. The actual location of the six belts are nearly located in the west of the six meridian of east longitude 85°,87°,89°,91°,93°,95° or located near these meridian. The six south\|north faulted structure belts spread in the same interval with near 2° longitude interval. The more clear and much more significance of south\|north trend faulted structure belts are the two S—N trend faulted structure belts of east longitude 87° and 89°. There are S—N trend faulted structure belts in the west of east longitude 83°,81°, or near the longitudes. The structure belts spreading features,manifestation,geological function and its importance, and inter texture and structure are not exactly so same. The structure belts all different degree caused different region of geological structure or gravity field and magnetic field. There is different scale near S—N trend faulted structure belt between the belts.

Intra-continental deformation and tectonic evolution of the West Junggar Orogenic Belt,Central Asia:Evidence from remote sensing and structural geological analyses

The West Junggar Orogenic Belt(WJOB)in northwestern Xinjiang,China,is located in the core of the western part of the Central Asian Orogenic Belt(CAOB).It has suffered two stage tectonic evolutions in Phanerozoic,before and after the ocean–continental conversion in Late Paleozoic.The later on intracontinental deformation,characterized by the development of the NE-trending West Junggar sinistral strike-slip fault system(WJFS)since Late Carboniferous and Early Permian,and the NW-trending Chingiz-Junggar dextral strike-slip fault(CJF)in Mesozoic and Cenozoic,has an important significance for the tectonic evolution of the WJOB and the CAOB.In this paper,we conduct geometric and kinematic analyses of the WJOB,based on field geological survey and structural interpretation of remote sensing image data.Using some piercing points such as truncated plutons and anticlines,an average magnitude of^73 km for the left-lateral strike-slip is calculated for the Darabut Fault,a major fault of the WJFS.Some partial of the displacement should be accommodated by strike-slip fault-related folds developed during the strike-slip faulting.Circular and curved faults,asymmetrical folds,and irregular contribution of ultramafic bodies,implies potential opposite vertical rotation of the Miao’ergou and the Akebasitao batholiths,resulted from the sinistral strike-slipping along the Darabut Fault.Due to conjugate shearing set of the sinistral WJFS and the dextral CJF since Early Mesozoic,superimposed folds formed with N–S convergence in southwestern part of the WJOB.

Transpressive Structures in the Ghadir Shear Belt, Eastern Desert, Egypt: Evidence for Partitioning of Oblique Convergence in the Arabian-Nubian Shield during Gondwana Agglutination

Transpressional deformation has played an important role in the late Neoproterozoic evolution of the ArabianNubian Shield including the Central Eastern Desert of Egypt.The Ghadir Shear Belt is a 35 km-long,NW-oriented brittleductile shear zone that underwent overall sinistral transpression during the Late Neoproterozoic.Within this shear belt,strain is highly partitioned into shortening,oblique,extensional and strike-slip structures at multiple scales.Moreover,strain partitioning is heterogeneous along-strike giving rise to three distinct structural domains.In the East Ghadir and Ambaut shear belts,the strain is pure-shear dominated whereas the narrow sectors parallel to the shear walls in the West Ghadir Shear Zone are simple-shear dominated.These domains are comparable to splay-dominated and thrust-dominated strike-slip shear zones.The kinematic transition along the Ghadir shear belt is consistent with separate strike-slip and thrustsense shear zones.The earlier fabric(S1),is locally recognized in low strain areas and SW-ward thrusts.S2 is associated with a shallowly plunging stretching lineation(L2),and defines^NW-SE major upright macroscopic folds in the East Ghadir shear belt.F2 folds are superimposed by^NNW–SSE tight-minor and major F3 folds that are kinematically compatible with sinistral transpressional deformation along the West Ghadir Shear Zone and may represent strain partitioning during deformation.F2 and F3 folds are superimposed by ENE–WSW gentle F4 folds in the Ambaut shear belt.The sub-parallelism of F3 and F4 fold axes with the shear zones may have resulted from strain partitioning associated with simple shear deformation along narrow mylonite zones and pure shear-dominant deformation in fold zones.Dextral ENEstriking shear zones were subsequently active at ca.595 Ma,coeval with sinistral shearing along NW-to NNW-striking shear zones.The occurrence of upright folds and folds with vertical axes suggests that transpression plays a significant role in the tectonic evolution of the Ghadir shear belt.Oblique convergence may have been provoked by the buckling of the Hafafit gneiss-cored domes and relative rotations between its segments.Upright folds,fold with vertical axes and sinistral strike-slip shear zones developed in response to strain partitioning.The West Ghadir Shear Zone contains thrusts and strikeslip shear zones that resulted from lateral escape tectonics associated with lateral imbrication and transpression in response to oblique squeezing of the Arabian-Nubian Shield during agglutination of East and West Gondwana.

Junction and Evolution of the Qinling,Qilian and Kunlun Orogenic Belts

As the main part of the “central mountain system” in the continent of China, the Qinling, Qilian and Kunlun orogenic belts have been comprehensively and deeply studied since the 1970s and rich fruits have been reaped. However, these achievements were mostly confined to an individual orogenic belt and the study of the mutual relationship among the three orogenic belts was obliged to depend on comparative studies. Different views were produced therefrom. The material composition and structural features of the junction region show that there are several epicontinental and intracontinental transform faults developed in different periods. Restricted by these transform faults, the large-scale lateral movements and, as a consequence, complicated magmatism and tectonic deformation took place in the orogenic belts. According to these features, the authors put forward a three-stage junction and evolution model and point out that there is not a single junction zone traversing from west to east but that the three orogenic belts have been joined progressively by the epicontinental and intracontinental transform faults.

Decadal Seismicity before Great Earthquakes—Strike-Slip Faults and Plate Interiors: Major Asperities and Low-Coupling Zones

Decadal forerunning seismic activity is examined for very large, shallow earthquakes along strike-slip and intraplate faults of the world. It includes forerunning shocks of magnitude Mw ≥ 5.0 for 21 mainshocks of Mw 7.5 to 8.6 from 1989 to 2020. Much forerunning activity occurred at what are interpreted to be smaller asperities along the peripheries of the rupture zones of great mainshocks at transform faults and subduction zones. Several great asperities as ascertained from forerunning activity agree with the areas of high seismic slip as determined by others using geodetic, mapping of surface faulting, and finite-source seismic modeling. The zones of high slip in many great earthquakes were nearly quiescent beforehand and are identified as the sites of great asperities. Asperities are strong, well-coupled portions of plate interfaces. Different patterns of forerunning activity on time scales of up to 45 years are attributed to the sizes and spacing of asperities (or lack of). This permits at least some great asperities along transform faults to be mapped decades before they rupture in great shocks. Rupture zones of many great mainshocks along transform faults are bordered either along strike, at depth or regionally by zones of lower plate coupling including either fault creep forerunning activity, aftershocks and/or slow-slip events. Forerunning activity to transforms in continental areas is more widespread spatially than that adjacent to oceanic transforms. The parts of the San Andreas fault themselves that ruptured in great California earthquakes during 1812, 1857 and 1906 have been very quiet since 1920;moderate to large shocks have been concentrated on their peripheries. The intraplate shocks studied, however, exhibited few if any forerunning events, which is attributed to the short period of time studied compared to their repeat times. The detection of forerunning and precursory activities for various time scales should be sought on the peripheries of great asperities and not just along the major faults themselves. This paper compliments that on decadal forerunning activity to great and giant earthquakes along subduction zones.

TECTONIC-GEOMORPHIC FEATURES OF THE STRIKE-SLIP FAULT ZONE IN EASTERN HUNAN AND WESTERN JIANGXI

Eastern Hunan-western Jiangxi, the main distribution domain of the Luoxiao MountainRange, is one of the key districts of the Circum-Pacific tectonically active belt in China, in whichNNE-trending en echelon strike-slip faulting since Cenozoic time has obviously controlled thefundamental framework of the modern land forms. Based on the study of tectonic evolution and ac-tive strike-slip faults, this paper discusses the forms, types and combinations of the modern tec-tonic land forms in this region.

长江经济带高端服务业绿色发展研究

绿色发展和可持续发展是当今世界的潮流。高端服务业是绿色服务业,绿色是服务业发展的方向。在国际发展绿色化的大背景下,长江经济带必须通过绿色发展,发展附加值高、技术先进的高端服务业,实现产业结构的绿色重组。创新高端服务业发展模式是促进长江经济带绿色发展的重要保障。文章以长江经济带省市面板数据作为研究对象,从省际层面对长江经济带高端服务业绿色发展进行评价。实证分析结果表明:绿色创新、绿色信贷、产业结构变迁、经济开放程度等会促进长江经济带高端服务业绿色发展。建议长江经济带在国家战略引导下,通过实质性绿色政策的推进,发挥中心城市在高端服务业发展中的领头作用,实现现代产业体系的绿色转型。

数智赋能“一带一路”教育合作与课程建设

“一带一路”教育合作正在不断深化,数智技术赋能“一带一路”教育合作,推进数智化课程建设,应从支持机制、资源建设、平台融合、智能升级等多方面进行剖析。数智化课程要充分体现正能量,匹配学习者需求,符合在线课程特点,具备灵活的交互机制,避免产生资源堆砌、与线下课程脱节和智能化程度不高等问题。建设好线下教育实践基地、增强课程的体验感对于发挥课程育人效果也非常关键。

地面高精度磁法测量在青海某区地质矿产调查中的应用

为综合研究青海某区成矿远景和找矿潜力,本文通过对该区1∶5万地面高精度磁法测量数据资料进行一系列位场转换处理,分析全区磁场分布规律和异常信息特征,结合地质背景、岩石磁性特征和化探水系沉积物测量等资料着重对M1异常进行解释推断,圈定1处与基性—超基性岩关系密切的铜钴镍多金属A类找矿靶区,采用2.5D人机交互反演,拟合出异常体埋深、形态等赋存情况。本研究建立的与基性—超基性岩带有关的铜钴多金属矿的找矿模型,为邻区甚至布青山—阿尼玛卿构造带区域内的找矿工作提供借鉴经验。

基于双目视觉的输送带表面损伤定量分析方法

为了对输送带表面损伤进行定量分析以有效判断其损伤程度,并根据损伤程度选择检修方法和时间,为工作人员检修提供依据,提出了一种基于双目立体视觉的输送带表面损伤定量分析方法。该方法首先对双目相机进行相机标定,对输送带表面损伤图像进行图像处理校正、立体匹配,基于视差原理根据三角测量原理获取目标点的三维空间信息,通过数学计算模型对损伤程度进行定量分析,提出了改进的Census变换和SGM(semi-global matching)算法相结合的立体匹配算法。结果表明:提出的改进算法匹配效果有所提升,和Census变换算法及梯度算法进行对比,误匹配率分别降低了5.26百分点和3.92百分点,得出的视差图精度最高;通过提出的方法对输送带表面损伤进行定量分析,在输送带损伤长度、宽度、深度三者误差中,损伤深度误差最大为8.5%,仍在可接受范围。

长江经济带产业绿色转型升级:进展、挑战与路径

产业绿色转型升级是长江经济带实现高水平保护和高质量发展的重要支撑。近年来,长江经济带坚持共抓大保护、不搞大开发,坚持生态优先、绿色发展,产业结构和工业结构持续优化,绿色产业成为经济增长新引擎;积极推动产业绿色低碳技术改造,绿色制造体系初步建立;稳步推进沿江化工企业“关改搬转”,产业布局与产业结构更加合理。新时代,长江经济带产业绿色转型升级面临着传统行业规模大、企业内生动力不足、长效机制尚未形成、基础能力相对薄弱以及区域产业协同不畅等多方面挑战,下一阶段,长江经济带产业绿色转型升级应着重加强基础性工作,健全发展机制、优化发展环境、增强企业绿色转型升级的内在动力和能力。

县域耕地非农化、非粮化与乡村人口空心化的耦合协调关系——以长江经济带为例

耕地非农化、非粮化的不断扩大严重影响了我国的粮食安全,亟需研究其演变机制和管控措施。基于1990、2000、2010和2020年四期土地覆盖数据和农业劳动力数据,利用耦合协调度模型和探索性时空数据分析(ESTDA)方法,分析了长江经济带县域耕地非农化、非粮化和乡村人口空心化的时空演化特征及其耦合协调关系。结果表明:(1)非农化呈现东高西低的格局,且存在围绕中心城市高值集聚的态势。非粮化则大致呈现出西高东低的倾向,远离大城市的边远县域非粮化程度较高。研究期内非农化和非粮化呈整体加剧趋势,乡村人口空心化程度显著提升。(2)非农化、非粮化和乡村人口空心化之间呈现较强耦合作用,失调区域逐渐扩大。(3)非农化、非粮化和乡村人口空心化耦合协调度存在明显的空间集聚现象并逐渐增强。高值集聚区主要分布在上游地区且数量逐渐减少,低值集聚区分布相对分散。(4)非农化、非粮化和乡村人口空心化耦合协调度具有较强时空动态特征,但县域及其邻域协同变动的比例较高,表明具有较强的局域整合性。

新质生产力推动长江经济带高质量发展的内在逻辑与策略方向

长江经济带建设是党和国家着眼于发展全局做出的重大战略部署,是建设社会主义现代化强国、实现共同富裕的必由之路和具体要求。新质生产力是传统生产力的质态跃迁,是具有鲜明的时代特征、丰富的科学内涵、先进表现和实践路径的崭新概念。新质生产力赋能长江经济带建设从逻辑机理分析是坚持创新增强发展新动能,统筹协调稳定区域发展步伐,坚持绿色保障发展可持续,深化开放融合拓展发展空间,推进共建共享提升发展实效。实践表明,新质生产力的发展将坚持产业结构调整和技术创新驱动力作用,创新人才培养体系与优化新质人才要素规模,发挥数据要素乘数效应支撑发展数智化转型,深化改革开放和坚持城乡融合发展并行共举,通过这些举措助力长江经济带高质量发展,扎实推进强国建设、民族复兴伟业。

基于透视变换和SNc-YOLOv5的大块煤识别方法应用

为了提高带式输送机大块煤识别的准确率,避免大块煤堆积对皮带造成的磨损,延长输送机的使用寿命,提出了基于透视变换和SNc-YOLOv5的大块煤识别方法,该方法首先利用透视变换技术对原始图像进行处理,有效地将图像中的非输送机区域滤除,并对输送机区域进行坐标矫正;然后,采用SNc-YOLOv5模型对经过标准化处理的图像进行深度学习建模,得到大块煤识别模型;最后,通过试验分析和现场应用对该方法进行有效性验证。结果表明:该方法在1号煤矿数据集的试验分析精确率为94.8%,召回率为83.2%,在2号煤矿数据集的试验分析精确率为92.8%,召回率为85.3%,现场应用置信度达到0.9,与其他方法进行比较,精确率和召回率指标均优于其他方法;该方法在图像预处理阶段提取带式输送机区域对图像进行标准化,仅对感兴趣区域进行处理,提高了大块煤识别的准确率。该算法部署到某煤矿现场,能够实现实时监测,为带式输送机的安全运行和延长使用寿命提供了有力保障。

准确把握绿色发展要求 深入推动长江水文高质量发展

绿色发展是引领我国经济社会发展的五大发展理念之一,是关系我国发展全局的一个重要理念。水文事业是国民经济和社会发展的基础性公益事业,水文行业高质量发展也要体现绿色发展的要求。文章分析了绿色发展理念对水文提出的新要求,梳理了新阶段长江水文的工作思路,总结了在树立绿色发展理念、构建集约高效的水文网站体系、推动生产与管理方式绿色转型方面取得的成效以及在支撑水资源节约集约利用和河湖生态保护治理、服务经济社会高质量发展等方面开展的实践,并对长江水文深化绿色发展理念进行了展望。