The Carboniferous at the Northern Foot of the Dabie Mountains and Its Tectonic Implications

In the Qinling orogenic belt. oceanic crust originated in the Early Palaeozoic. while the product of conti-nental collision appeared as late as after the Triassic. The Late Palaeozoic records there are of major impor-tance for understanding the tectonic regime at that time. The Carboniferous and even Permian sequences andthe distribution of sedimentary facies in northern Huaiyang indicate that the rocks were formed in a large basinopening towards the south. Regional stratigraphic correlation shows that the interior of the Qinling orogenicbelt was a sea trough lying between the Yangtze and North China plates in the middle part of the LatePalaeozoic. With subsequent northward migration of the South China Sea, the two seas were connected witheach other. Both the melanges and the Dabie block ia the eastern sector of the Qinling belt were formed in theMesozoic ?.

Lower time limit on the UHPM rock exhumation: Discovery of eclogite pebbles in the Late Jurassic conglomerates from the northern foot of the Dabie Mountains, eastern China

Eclogite pebbles are first discovered in late Jurassic conglomerates of the Fenghuangtai Formation from the northern foot of the Dabie Mountains, eastern China. The eclogite shows relatively strong retrograde metamor-phism. The major remnant minerals are garnet, phengite, quartz, rutile, clinozoisite, fingerprint(or worm)-form sym-plectite and pseudomorphic enclosure of coesite in garnet. End-member components of the garnet mainly made up of grossular (27.7%-37.8%), almandinc (45.5%-49.0%) and pyrope (12.3%-25.7%). End-member components of the pyrope is less than 30%, i.e. equivalent to C type eclogite. Si-cations of the phengite are 3.44-3.54 p.f.u. (taking O=11as standard). It is estimated that the pressures are 2.5-3.2 GPa, the temperatures are 600-900℃. Discovery of the eclogite pebbles in the late Jurassic conglomerates from the northern foot of the Dabie Mountains suggests that the HP-UHP metamorphic rocks of the Dabie Mountains, which were formed in Triassic, had been exposed to the surface in

Retrogressive Microstructures of the Eclogites from the Northern Dabie Mountains, Central China: Evidence for Rapid Exhumation

The ultrahigh-pressure eclogites from the northern Dabie Mountains in central China occurred as tectonic lens or blocks within granitic gneisses or meta-peridotites. Petrologic studies suggest that the studied eclogites experienced strongly retrogressive metamorphism and produced a series of characteristic retrogressive microstructures. The retrograde structures mainly include: (1) oriented needle mineral exsolution, e.g., quartz needles in Na-clinopyroxene and rutile, clinopyroxene and apatite exsolution in garnet formed under decreasing pressure conditions during exhumation; (2) symplectite, especially, two generations of symplectites developed outside the garnet grains, which are called “double symplectite” here; (3) compositional zoning of minerals such as garnet and clinopyroxene; (4) minerals with a reaction rim or retrograde rim, e.g., omphacite with a diopside rim, diopside with an amphibole rim and rutile with a rim of ilmenite. These retrograde textures, especially mineral zoning and symplectite, provide important petrologic evidence for the exhumation process and uplift of high-grade metamorphic rocks such as eclogite in the northern Dabie Mountains, indicating a rapid exhumation process.

What are the keys to influence the life satisfaction of eco-migrants in the northern foot of the Qilian Mountains?A test based on the livelihood risk interaction

Eco-migrants'ability to adapt to livelihood risks and their satisfaction with lives directly affect the ecological and economic benefits of ecological migration engineering.To formulate an effective livelihood risk prevention system and welfare guarantee mechanism,we took the ecomigrants in Wuwei City as an example,developed an integrated analytical framework for life satisfaction and employed linear regression models to identify the interactions between livelihood risk and life satisfaction.Our findings indicate that 94.66%of eco-migrants in Wuwei City are threatened by livelihood risks after relocation.High living expenses,poor quality of redistributed production goods,and re-poverty constitute the main risks.The risk multiplicity index is 2.96.Besides cultural types,there are no significant differences in regions and livelihoods.A total of 55.73%of eco-migrants are satisfied with their lives,with the Liangzhou district scoring the highest.Except for satisfaction with development potential and public services,no significant intergroup differences were found among regions and livelihood patterns.Eco-migrant's life satisfaction is significantly affected by livelihood risks.Eco-migrants'satisfaction with living income,social integration,farmer-friendly policies and overall life is negatively affected by the risk of repoverty and inadequate social security.An ecomigrant's satisfaction with development potential and community construction is not influenced by one type of risk alone,but the interaction between risks has a strong influence.The interaction of welfare risks with economic risks and policy risks will balance and weaken the adverse effects of a single risk on those elements in the economic and policy spheres.This study offers novel ideas for rural revitalization,hollow governance,and well-being assurance.

Space Structuring of the Northern Foot of the Qinling Mountains(Xi'an Section) based on Landscape City

Northern foot of the Qinling Mountains(Xi'an Section) is a transitional section between the Qinling Mountains and Xi'an City, so it has great ecological signifi cance. On the basis of sorting out landscape city, space structuring of the northern foot of the Qinling Mountains was studied within the theoretical framework of landscape city, it was disclosed that northern foot of the Qinling Mountains was a signifi cant ecological screen for the landscape city spatial pattern of Xi'an, and an important carrier for its "mountain, water and city" cultures. Then, fi ve infl uence factors for the space structuring of the study area were given, and basic contents of the space structuring analyzed from fi ve perspectives of spatial structure, spatial form, ecological environment, integration of regional spaces, historical and cultural context, so as to explore ecological conservation and moderate utilization of the northern foot of the Qinling Mountains from the perspective of space structuring.

Mineral Composition and Metamorphic P-T Conditions of the Eclogitic Rocks in the Eastern Dabie Mountains and Their Genetic Implication

There are obvious differences in the mineral assemblage and metamorphic P-T conditions between the eclogites from the northern and southern parts of the eastern Dabie Mountains. Those from the northern part of the mountains are developed in Alpine peridotite and gneiss. They have a mineral assemblage of garnet+diopside with no quartz, and were formed at temperatures of 600℃-740℃. Those from the southern part are developed in gneiss and marble. They consist of garnet+omphacite+less quartz and were metamorphosed at temperatures in the range of 650°-800℃. These differences suggest that the former may be formed during the metamorphism of the deep subducted oceanic crust, whereas the latter may be genetically related to the subduction of the continental crust in this area.

Thrusting and Exhumation Processes of a Bounding Mountain Belt: Constraints from Sediment Provenance Analysis of the Hefei Basin

Lithic (or gravel) composition analyses of the Jurassic Sanjianpu Formation and Fenghuangtai Formation in the Hefei basin show that the sediment provenance consists mainly of four kinds of rock units: the basement metamorphic complex, granitic rocks, medium- and low-grade metamorphic rocks, and sandy and muddy sedimentary rocks, which are distributed along the bounding thrust belt. The whole stratigraphic section can be divided into 2 lithic sequences and 7 subsequences. The regular distribution and changes of lithic fragments and gravels in lithic (or gravel) sequences reflect that the bounding thrust belt of basin has undergone 2 thrusting cycles and 7 thrusting events. Lithic (or gravel) composition analyses of the basin fully reveal that the northern Dabie basement metamorphic complex was exhumed on the earth's surface in the Middle and Late Jurassic, and extensive intermediate and acid intrusive rocks were developed in the southern North Huaiyang or northern Dabie Mountains during the basin's syndepositional stage.

内蒙古阴山北麓丘陵地区城镇绿化现状与对策分析--以四子王旗乌兰花镇为例

文章对四子王旗乌兰花镇城镇绿化现状进行实地调查和统计分析。结果表明:2012-2022年间,乌兰花镇周边8个行政村村屯绿化工程面积达134.2 hm^(2),存活乔灌木8.2万株,主要树种有胡杨、云杉等,其中,生盖营村绿化面积最大,为25.1 hm^(2);乌兰花镇建成区绿地率为32.6%,绿化覆盖率为35.5%。建成区内防护绿地面积最大(231.20 hm^(2)),占绿地面积的45.5%;其次是附属绿地(151.18 hm^(2)),占29.7%;公园绿地面积(92.52 hm^(2))占18.2%,人均公园绿地面积14.20 m^(2),建成区公园绿地服务半径覆盖率为72.2%。该地区绿地系统存在水资源匮乏、围封设施不完善、养护资金投入不足、树种选择不合理及绿化用地逐年减少等问题,在此基础上提出合理布局水资源、完善配套设施、增加养护资金投入、优化树种选择和加强绿化用地保护等相应对策,旨在为促进该地区城镇绿地规划和城镇绿地系统的可持续发展提供科学依据和指导。

Discovery of the eclogite and its petrography in the Northern Dabie Mountain

Eclogite from the Northern Dabie Mountain is a new finding by the authors. These eclogites in foliated perdotite are enveloped by banded gneiss and occur in the mafic-ultramafic rock belt. They are mainly composed of omphacite, garnet, diopside, orthopyroxene, amphibole, plagioclase and magnetite, and a small amount of rutile, spinel, olivin and 鏾rundum. The mineral association of peak metamorphism of the eclogite is omphacite+garnet+rutile. The existence of eclogite in the Northern Dabie Mountain implies that there was an eclogitic metamorphism prior to the granulitic facies one in the mafic-ultramafic rock belt.

Eclogites from the Northern Dabie Mountains, eastern China: Geochemical characteristics, Sr-Nd isotopic compositions and tectonic implications

The petrologic geochemical and Sr-Nd isotopic compositions of the eclogites from the mafic-ultramafic rock belt (MUMRB) in the Northern Dabie Mountains indicate that: (1) the protoliths of most of eclogites are tholeiitic basalt and a few may be gabbro, and most of them produced from the Yangtze subducted continental crust (lower crust and formed during the deep subduction) and a part may be from paleo-oceanic relics between the Yangtze and North China continental plates; (2) their positive Nb anomalies and related trace element characteristics show that they did not form in the island-arc setting; (3) the metamorphosed MUMRB with eclogite and meta-peridotite blocks along the southern part of the Mozitan-Xiaotian fault zone may represent the suture zone produced during the collision between the Yangtze and North China continental plates, which included the Yangtze subducted continental crust and paleo-oceanic relics.

Quartz and clinoenstatite exsolutions in clinopyroxene of garnet-pyroxenolite from the North Dabie Mountains,eastern China

The exsolution lamellae of quartz and clinoen-statite are idenfied in diopside of garnet-pyroxenolite from the North Dabie Mountain by transmission electron microscopy, which is interpreted that the lamellae are originally exsolved from a former ultra-high-pressure clinopyroxene due to decreasing of pressure. Study of petrography shows that there is compositional zoning hi the diopside itself. It is implied that the garnet-pyroxenolite had undergone intensive high-temperature granulite fades and high-amphibolitic fades retrogressive metamorphism, while the peridotite (the garnet-pyroxenolite’s host rock) emplaced the

基于“两山”理论的秦岭北麓乡村空间营建策略研究

空间营建是秦岭北麓乡村地区“两山”实践的重要保障.研究提出在乡村“资源-资产-资本”的转化过程中,应构建“两环节、三层次、多主体”的“两山”转化空间营建路径:以生态基础培育和多元增值开发为两大空间营建环节,构建“区域→单元→地块”三层次营建体系,建立多主体参与共赢的营建机制.研究以西安鄠邑区为例,梳理其在大都市圈发展背景下“两山”转化的乡村空间营建问题,提出“要素统筹、生境修复、产居转型、有序共建”四方面空间营建策略,形成地域适宜性的绿色共建模式,以期为地区乡村振兴和高质量建设提供借鉴.

秦岭北麓乡村可持续发展的环境美学评价体系构建

构建秦岭北麓乡村的环境美学评价体系,旨在优化景观发展,通过视觉美感、自然环境、生态平衡、文化传承和居民满意度等多维度指标,采用定量与定性分析,为乡村规划提供科学支持,促进生态文明,推动区域可持续发展,并为相似乡村地区提供参考。

大别山北缘不同生活型木本植物叶功能性状及其耦合关系

【目的】探讨大别山北缘不同生活型木本植物叶功能性状变异,研究叶功能性状指标之间的耦合关系,为解析植物对气候变化的响应机制提供依据。【方法】采集大别山北缘连康山国家级自然保护区30种常见的不同生活型木本植物(常绿、落叶、乔木、灌木)的叶片,测定其叶绿素含量(以SPAD表示)、干鲜比、氮质量分数、磷质量分数、钾质量分数、氮磷比、叶面积、比叶面积共8个叶功能性状指标,分析了不同生活型木本植物叶功能性状及其相关性。【结果】不同生活型木本植物叶功能性状指标具有一定的差异性,其中常绿和落叶树种的叶片SPAD、氮质量分数、磷质量分数、钾质量分数、叶面积和比叶面积之间差异显著(P<0.05);乔木与灌木树种的叶面积、氮质量分数、磷质量分数、钾质量分数、干鲜比与氮磷比差异显著(P<0.05)。部分叶功能性状指标之间存在一定的相关性,叶片氮、磷质量分数与钾质量分数呈显著正相关(P<0.05),叶片氮质量分数与磷质量分数呈显著正相关(P<0.05);叶面积与叶片氮、磷、钾质量分数呈显著正相关(P<0.05),比叶面积与叶片氮、磷、钾质量分数呈显著正相关(P<0.05)。主成分分析结果表明:叶片磷、氮、钾质量分数是较为重要的叶功能性状指示指标,可将30种木本植物归为4个功能组,且第1和第2主成分对植物叶功能性状变异的贡献率分别为55.2%和12.8%。【结论】叶功能性状指标在不同生活型木本植物之间存在一定差异,其中叶磷、氮、钾质量分数是指示性指标,且与叶面积显著正相关。图4表1参28.

基于AHP-EWM-TOPSIS的秦岭北麓西安段冰酒葡萄生态适宜性评价

本研究旨在评估冰酒葡萄(Ice wine grape)在秦岭北麓西安段的生态适宜性,以促进该作物种植的经济潜力并优化当地葡萄产业结构。根据冰酒葡萄生长需求和秦岭北麓自然气候特点,研究选取最冷月均温、≥10℃有效积温、生长季干燥度、坡度、土壤pH等评价因子,确立冰酒葡萄适宜性评价体系。基于秦岭北麓西安段2000—2021年逐日气象观测数据、生态数据,采用层次分析法(AHP)、改进熵值法(EWM)、TOPSIS综合评价法,本研究构建了一个冰酒葡萄种植综合区划评估模型,对影响冰酒葡萄种植的气候、地形、土壤三大指标的空间分布进行分析。经统计分析得出最适宜区、适宜区、次适宜区和不适宜区4个等级。结果表明,所提出的方法能够有效地识别秦岭北麓西安段内冰酒葡萄种植的生态优势区域,且所得区划结果与实际情况高度一致。这一发现对冰酒葡萄种植的区域布局和科学规划提供了重要参考。

秦岭北麓筠竹种子育苗试验

因气候条件的限制,秦岭北麓很难获得竹子种子,因而难以通过播种育苗获得造林绿化所需要的大量苗木。2019年7月在秦岭北麓陕西省楼观台国有生态实验林场辖区的森林公园内发现了一株筠竹开花并结实,遂采集种子,开展了播种试验,以期探讨秦岭北麓竹种子育苗的可行性。结果显示,筠竹采种后在室温下贮藏,第2年播种的出苗率为25.4%;实生苗前3年的生长状况优于秦岭北麓优势竹种淡竹的生长。该研究表明,在秦岭北麓筠竹通过播种进行繁殖是可行的,并探索了一套实生苗繁育的管理经验,可在一定范围内推广,为绿化造林和生态建设提供大量苗木。

秦岭北麓西安段峪口村落洪涝适应性营建智慧研究

秦岭北麓西安段为洪涝灾害多发区域.在长期同雨洪博弈共生的过程中,当地传统村落形成了以低技术、低成本、低维护为特征的洪涝适应性智慧.在洪涝风险日益增多的当下,这些传统实践智慧对促进区域人水和谐、洪涝韧性和可持续发展具有重要借鉴意义.以秦岭北麓典型区域内峪口传统村落为例,基于田野调查、多源数据比对互证法和图解分析法,本文旨在阐明洪涝适应与村落营建关系的基础上,在选址、街巷布局及洪涝管控设施系统等三个方面,系统研究其洪涝适应性营建智慧,以期在新时期为城乡洪涝韧性人居环境规划营建,提供理论和经验借鉴.

大别山东南麓中新生代碎屑岩地球化学特征及其对物源的制约

位于大别山东南麓的安庆-潜山地区中新生代碎屑岩比较发育,主元素分析表明,砂岩主要为杂砂岩,其次是岩屑砂岩和长石砂岩。根据主元素、微量元素和稀土元素特征值分析结果,中、上三叠统和下、中侏罗统的源岩来源广泛,属于大陆岛弧、活动大陆边缘和被动大陆边缘构造背景,可能反映了前陆盆地物源的二元特征。古近系源岩主要为活动大陆边缘和大陆岛弧构造环境,说明物源仅来自大别山造山带。稀土元素比值及相关系数分析揭示,中晚三叠世黄马青群的源岩主要为宿松群的长英质片岩、浅粒岩以及大别杂岩,侏罗纪磨山组大致类似于大别群的花岗片麻岩,罗岭组与大别群比较类似。显示大别山造山带在中晚三叠世已经隆升并遭受剥露。

大别山北部榴辉岩的大地构造属性及冷却史

岩石地球化学及同位素年代学研究表明 ,大别山北部榴辉岩的大部分属印支期扬子俯冲陆壳 (下地壳 )的一部分 ;大致沿磨子潭 -晓天断裂附近分布的含榴辉岩、大理岩和变质橄榄岩的镁铁 -超镁铁质岩带可能代表扬子与华北 2个大陆板块之间的变质构造混杂岩带 ,它应接近于扬子与华北 2个大陆板块之间的缝合线 (镁铁 -超镁铁质岩带以北 ) ,而五河 -水吼剪切带则可能代表扬子俯冲陆壳内部的 1条拆离带或滑脱带 .冷却史研究表明 ,大别山北部榴辉岩峰期变质后初期 (2 30～ 2 10Ma)仅抬升到下地壳水平 ,因而未经历降温过程并具有比大别山南部榴辉岩较低的抬升速率 ,峰期变质后较慢的抬升速率及相应的近于等温或局部升温阶段也许是造成大别山北部榴辉岩与南部超高压带中榴辉岩差异的重要原因之一 ;同时 。

大别山北部镁铁-超镁铁质岩带中榴辉岩的分布与变质温压条件

大别山北部镁铁-超镁铁质岩带中的榴辉岩主要有两种产状,一是产于变形较强(面理化)的橄榄岩中,另一种是产于片麻岩中。其中,绿辉石中硬玉端元组分大多为Jd=20mol％～52mol％。产于橄榄岩和片麻岩中榴辉岩的石榴子石成分分别相当于Coleman的B型和C型榴辉岩。石榴子石成分特征及钠质单斜辉石中石英针状出溶体的出现表明,本区榴辉岩早期可能经历过超高压变质作用,且至少经历了3个变质阶段,即:①榴辉岩相峰期变质阶段,主要矿物共生组合为石榴子石+绿辉石+金红石±蓝晶石+石英(或柯石英假象?),p≥2.5GPa、t=595～874℃;②高压麻粒岩相变质阶段,主要矿物共生组合为石榴子石+透辉石+紫苏辉石+钛铁矿+尖晶石+斜长石等,p=1.1～1.37GPa、t=817～909℃;③角闪岩相变质阶段,主要矿物共生组合为角闪石+斜长石+磁铁矿等,p=0.5～0.6GPa、t=500～600℃。该区榴辉岩独特的麻粒岩相退变质阶段,表明榴辉岩在折返初期并未能上升到中上地壳,而处于下地壳,它与南部超高压变质岩有不同的p-t演化史,即在榴辉岩相峰期变质之后经历了近等温减压(或稍升温减压)和降温减压变质过程。