一、TIANJIN INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文文献综述）
晁红丽,任建德,吕际根,谢朝永,李莹琪,李瑞强,焦静华[1]（2020）在《河南省三川幅1:50000地质图数据库》文中进行了进一步梳理河南省三川幅（I49E013014）1:50000地质图数据库的数据源采用实测和数字填图方法获得,野外数据采集过程中实施构造–岩性填图,注重特殊地质体及非正式填图单位的表达,共采集薄片66件,全岩岩石化学样品180件,同位素测年样品19件,化学分析样品21件。图幅主要成果有:在陶湾群层型剖面上发现多门类、时限短的微体化石,确定陶湾群为奥陶纪;在陶湾群发现碱性火山岩夹层,指示奥陶纪在华北板块南缘发育伸展性盆地;确定宽坪岩群四岔口岩组、谢湾岩组内的绿片岩为板内火山岩,指示宽坪岩群主体形成于伸展性盆地;在图幅区南部填绘出志留纪碱长花岗斑岩岩墙群,限定了秦岭洋关闭的时代不晚于志留纪;将晚中生代侵入岩划分为5个侵入期次;厘定了栾川断裂带存在早古生代、早中生代、晚中生代3期活动;在区内新发现震旦纪冰积物。该数据库的数据内容分为基本要素类、综合要素类和对象类,数据量约为63.5 MB,充分反映了本图幅区的地质矿产成果资料,对该区矿产勘查与开发、地质灾害防治、秦岭造山带研究与地质科普等提供基础数据支撑。
ZHENG Mianping,ZHANG Yongsheng,LIU Xifang,NIE Zhen,KONG Fanjing,QI Wen,Jia Qingxian,PU Linzhong,HOU Xianhua,WANG Hailei,ZHANG Zhen,KONG Weigang,LIN Yongjie[2]（2016）在《Progress and Prospects of Salt Lake Research in China》文中研究表明China has unique salt lake resources, and they are distributed in the east of Eurasian salt lake subzone of the Northern Hemisphere Salt Lake Zone, mainly concentrated in the regions with modern mean annual precipitation lower than 500 mm. This paper preliminarily reviews the progress made in salt lake research in China for the past 60 years. In the research of Paleoclimate and paleoenvironment from salt lake sediments, a series of salts have been proposed to be indicators of paleoclimate, and have been well accepted by scholars. The chloride-sulfate depositional regions of the west Qaidam and the east Tarim have been revealed to be the drought center of China since the Quaternary, and more than 6 spreading stages of arid climate（salt forming） have been identified. Five pan-lake periods with highstands have been proved to exist during the late Quaternary on the Tibetan Plateau. In mineral resource prospecting and theories of the forming of salt deposits: the atlas（1:2500000） of hydrochemical zoning of salt lakes on the Tibetan Plateau has been compiled for the first time, revealing the zonal distribution and transition from carbonate type to chloride type from south to north and presenting corresponding mineral assemblages for different type of salt lakes; several large continental salt deposits have been discovered and the theory of continental potash deposition has been developed, including the salt deposition in deep basins surrounded by high mountains, the mineral deposition from multistage evolution through chains of moderate or shallow lakes with multilevels, the origin of potassium rich brines in gravel layers, and the forming of potassium deposits through the inheriting from ancient salt deposits, thus establishing the framework of "Continental Potash Deposition Theory"; several new types of Mg-borate deposits have been discovered, including the ulexite and pinnoite bed in Da Qaidam Lake, Qinghai, the pinnoite and kurnakovite bed in Chagcam Caka, Tibet, the kurnakovite bed in Lake Nyer, and the corresponding model of borate deposition from the cooling and dissolution of boron rich brines was proposed based on principles of geology, physics and chemistry. The anti-floatation-cold crystallization method developed independently has improved the capacity of KCl production to 3 million tons per year for the Qarham, serving the famous brand of potash fertilizer products. One 1.2 million ton K-sulfate production line, the biggest in the world, has been built in Lop Nor, and K-sulfate of about 1.6 million tons was produced in 2015. Supported by the new technology, i.e. brine preparation in winter-cooling-solarization-isolation-lithium deposition from salt gradient solar pond" the highest lithium production base at Zabuye Lake（4421 m）, Tibet, has been established, which is the first lithium production base in China that reaches the year production of 5000 tons of lithium carbonate. The concept of Salt lake agriculture（Salt land agriculture） has been established based on the mass growth of Dunaliella and other bacillus-algae and the occurrence of various halophytes in saltmarsh and salt saline-alkali lands, finding a new way to increase arable lands and develop related green industry in salt rich environments. Finally this paper presents some new thoughts for the further research and development on salt science, and the further progress in salt science and technology will facilitate the maturing of the interdisciplinary science "Salinology".
CHEN Jianping,XIANG Jie,HU Qiao,YANG Wei,LAI Zili,HU Bin,WEI Wei[3]（2016）在《Quantitative Geoscience and Geological Big Data Development:A Review》文中提出After long-term development, mathematical geology has today become an independent discipline. Big Data science, which has become a new scientific paradigm in the 21 st century, gives rise to the geological Big Data, i.e. mathematical geology and quantitative geoscience. Thanks to a robust macro strategy for big data, China’s quantitative geoscience and geological big data’s rapid development meets present requirements and has kept up with international levels. This paper presents China’s decade-long achievements in quantitative prediction and assessment of mineral resources, geoscience information and software systems, geological information platform development, etc., with an emphasis on application of geological big data in informatics, quantitative mineral prediction, geological environment and disaster management, digital land survey, digital city, etc. Looking ahead, mathematical geology is moving towards "Digital Geology", "Digital Land" and "Geological Cloud", eventually realizing China’s grand "Digital China" blueprint, and these valuable results will be showcased on the international academic arena.
DING Xiaozhong,ZHANG Kexin,GAO Linzhi,LU Songnian,PAN Guitang,XIAO Qinghui,LIU Yong,PANG Jianfeng[4]（2020）在《Research Progress and the Main Achievements of The Regional Geology of China Preface》文中进行了进一步梳理Introduction to The Regional Geology of China In 2008, a new project concerning the recompilation of The Regional Geology of China （RGC） was assigned by the Chinese Geological Survey （CGS） and undertaken by the Institute of Geology, Chinese Academy of Geological Sciences （CAGS）. Li Tingdong, an academician of the Chinese Academy of Sciences （CAS）, is the chief leader and chief scientist of the project. The last time The Regional Geology of China was compiled was in the 1980s （Cheng, 1994）.
CHEN Baoguo,ZHANG Jiuchen,YANG Mengmeng[5]（2016）在《The Present Research and Prospect of Chinese Geosciences History》文中研究表明It has been over a hundred years since the birth of research on Chinese geosciences history, which was accompanied by the continuous progress of Chinese geosciences. For hundreds of years, it has grown out of nothing to brilliant performance by several generations of Chinese geologists committing their hearts and minds with the spirit of exert and strive without stop to promote the process of China’s industrialization and to produce the significant impact on serving the society. The study of Chinese geosciences history reflects objectively and historically the history of geosciences in China, which has recorded, analyzed and evaluated the dynamic process sitting in the background and clue of the history of Chinese geosciences development. The study of the history of geological science has roughly experienced two stages in China. The first stage is the study of individual researchers. It spanned approximately 70 years from the early 20th century to the end of the 1970s. The research contents were mainly based on the evolution of geological organizations, the development and utilization of individual mineral species, the history of deposit discovery and the research of geological characters. The main representatives are Zhang Hongzhao, Ding Wenjiang, Weng Wenhao and Li Siguang, Ye Liangfu, Huang Jiqing, Yang Zhongjian, Xie Jiarong, Gao Zhenxi, Wang Bingzhang and etc. The most prominent feature of this period is the accumulation of a very valuable document for the study of the history of China’s geological history and lays a foundation for the exchange of geological science between China and foreign countries. The second stage is organized group study. It took around 60 years from the 1920s to 1980s. It includes the history of Chinese geology, the history of geological organizations, the history of geological disciplines, the history of geological education, the history of geological philosophy, the history of Chinese and foreign geological science communication, the history of geologists and etc. The most chief feature of this stage is the birth of academic research institute―the establishment of the Commission on the History of Geology of the Geological Society of China.
WANG Chenghui,WANG Denghong,XU Jue,YING Lijuan,LIU Lijun,LIU Shanbao[6]（2015）在《A Preliminary Review of Metallogenic Regularity of Gold Deposits in China》文中指出Gold is one of the most important mineral resources in China with its rich mineral resources. In recent years,significant progress has been made on the process of gold resource exploration. Some large and giant gold deposits were newly found and some important expansions in the main mining regions were also been completed. Studies on metallogenic regularity of gold deposits in China also have made achievements with a long–term work. This review aims to conclude the achievements of research on gold metallogenic regularity in China. Based on the data of about 2000 gold deposits and other ore（mineralized） occurrences,gold deposits in China were classified into five prediction types: gold deposits genetically related to granite–greenstone formation,gold deposits related to sedimentary formation（including the Carlin type and the metamorphosed clastic rock related vein gold deposit）,gold deposits genetically related to volcanic rocks（including the continental and marine types）,gold deposits genetically related to intrusions（including the porphyry type and the inner intrusion and contact zone related gold deposit）,gold deposits of supergenesis（including fracture zone–altered rock gold deposit,placer gold deposit,gossan type gold deposit and soil type gold deposit）. Statistics on precise chronology data of gold deposits indicate that there occurred 5 main periods of gold–mineralization in geological history of China. They were Neoarchean to Paleoproterozoic,Meso–Neoproterozoic,Paleozoic,Mesozoic,and Cenozoic. Gold deposits in China mainly formed in the Mesozoic and the Cenozoic. On the studies of the spatial–temporal distribution characteristics of gold deposits,53 gold–forming belts were delineated in China. The metallogenic regularity of gold deposits was preliminarily summarized and 71 gold metallogenic series were proposed in China. This suggests that it is necceary to deepen the study on metallogenic regularity of gold deposits and to provide the theory guide for the ore–prospecting for gold resources in China.
Lisaia Daria（达丽娅）[7]（2019）在《俄罗斯城市可持续发展及其对中国城市的启示研究》文中进行了进一步梳理城市可持续发展是我们地球繁荣未来的一个重要方面。根据2005年联合国世界峰会的成果,可持续发展的概念包含三个基本要素:社会、经济和环境。社会经济发展问题是国家政策的核心。从方法和途径到解决（具体）问题的方案取决于国家的繁荣和国民的经济生活水平。面对严峻的全球竞争,城市居住模式的管理以及寻求组织和管理人力、国土和生产资源的最佳解决方案是社会经济发展的途径之一。目前国家最高一级的国土开发规划和管理流程的演变正在进行,并与其他各级政府的规划系统进行协调。根据在2017年5月8日至12日举行的联合国人类住区规划署理事会第二十六届会议的报告,这是在城市（市政）层面提高国家政策执行效率和改善城市环境质量的关键要求之一。国家政策发展的另一个重要要求是将传统经济转变为知识经济,并带领该国走向世界技术领先,这是最可持续的经济发展方式。建立国家的创新基础设施是实现这些任务的必要条件之一。在此背景下,对世界上最大的两个国家（俄罗斯和中国）的城市发展经验的研究正在成为城市规划、设计和建筑广阔领域专家的宝贵知识来源。本文的研究目标是明确俄罗斯和中国社会经济政策的优先事项并对其在国土和城市规划层面的实施机制进行比较分析,这两者是国家可持续发展的重要条件。全文分为五个部分,共八章。其中第一部分（第1章）对课题相关的文献进行综述和分析,并制定研究目标、研究对象、研究假设和研究方法。第二部分（第2-3章）介绍第一项研究成果,即俄罗斯和中国城市可持续发展的比较分析,并对可持续城市规划和城市化进程两个主题进行详细描述与对第一项研究的结果进行讨论。第三部分（第4-7章）介绍第二项研究成果,即俄罗斯的案例研究,相关主题包括:俄罗斯城市可持续发展的社会经济问题;俄罗斯的创新基础设施;从科学定居点到斯科尔科沃创新中心的苏联科学城市发展历史回顾;斯科尔科沃创新中心的城市规划理念。第四部分（第8章）对第二项研究的结果进行讨论,探讨城市发展在国家可持续发展过程中的作用。第五部分介绍结论并对后续的科研工作提出建议。论文作者对俄罗斯和中国的历史,以及两国在20世纪和当下建设现代国家的过程中所经历的困难道路深表敬意和理解。尽管在经济、社会、文化和地缘上存在差异,两个国家都是在现在和未来为和平与稳定做出巨大努力的强大的现代国家。
JIN Ruoshi,MIAO Peisen,SIMA Xianzhang,LI Jianguo,ZHAO Hualei,ZHAO Fengqing,FEN Xiaoxi,CHEN Yin,CHEN Lulu,ZHAO Lijun,ZHU Qiang[8]（2016）在《Structure Styles of Mesozoic-Cenozoic U-bearing Rock Series in Northern China》文中认为In Northern China,sandstone-type uranium（U） deposits are mostly developed in MesozoicCenozoic basins. These U deposits are usually hosted in unvarying horizons within the basins and exhibit typical U-forming sedimentary associations,which is referred to as U-bearing rock series. This study describes the structural features of U-bearing rock series within the main Mesozoic-Cenozoic Uproducing continental basins in Kazakhstan,Uzbekistan,and Russia in the western segment of the Central Asian Metallogenic Belt（CAMB）,and Northern China in the eastern segment of the CAMB. We analyze the basic structural conditions and sedimentary environments of U-bearing rock series in Northern China and classify their structural styles in typical basins into river valley,basin margin,and intrabasin uplift margin types. The intrabasin uplift margin structural style proposed in this study can be used to indicate directions for the exploration of sandstone-type U deposits hosted in the center of a basin. At the same time,the study of structural style provides a new idea for exploring sandstone-type U deposits in Mesozoic-Cenozoic basins and it is of great significance to prospecting of sandstone-type uranium deposits.
YAO Jianxin,BO Jingfang,HOU Hongfei,WANG Zejiu,MA Xiulan,LIU Fengshan,HU Guangxiao,JI Zhansheng,WU Guichun,WU Zhenjie,LI Suping,GUO Caiqing,LI Ya[9]（2016）在《Status of Stratigraphy Research in China》文中研究说明Scientific research and productive practice for earth history are inseparable from the accurate stratigraphic framework and time framework. Establishing the globally unified, precise and reliable chronostratigraphic series and geological time series is the major goal of the International Commission on Stratigraphy（ICS）. Under the leadership of the ICS, the countries around the world have carried out research on the Global Standard Stratotype-section and Points（GSSPs） for the boundaries of chronostratigraphic systems. In the current International Chronostratigraphic Chart（ICC）, 65 GSSPs have been erected in the Phanerozoic Eonothem, and one has yet been erected in the Precambrian Eonothem. Based on the progress of research on stratigraphy especially that from its subcommissions, the ICS is constantly revising the ICC, and will publish a new International Stratigraphic Guide in 2020. After continual efforts and broad international cooperation of Chinese stratigraphers, 10 GSSPs within the Phanerozoic Eonothem have been approved and ratified to erect in China by the ICS and IUGS. To establish the standards for stratigraphic division and correlation of China, with the support from the Ministry of Science and Technology, the National Natural Science Foundation of China and the China Geological Survey, Chinese stratigraphers have carried out research on the establishment of Stages in China. A total of 102 stages have been defined in the "Regional Chronostratigraphic Chart of China（geologic time）", in which 59 stages were studied in depth. In 2014, the "Stratigraphic Chart of China" was compiled, with the essential contents as follows: the correlation between international chronostratigraphy and regional chronostratigraphy of China（geologic time）, the distributive status of lithostratigraphy, the characteristics of geological ages, the biostratigraphic sequence, the magnetostratigraphy, the geological events and eustatic sea-level change during every geological stage. The "Stratigraphical Guide of China and its Explanation（2014）" was also published. Chinese stratigraphers have paid much attention to stratigraphic research in south China, northeast China, north China and northwest China and they have made great achievements in special research on stratigraphy, based on the 1:1000000, 1:250000, 1:200000 and 1:50000 regional geological survey projects. Manifold new stratigraphic units were discovered and established by the regional geological surveys, which are helpful to improve the regional chronostratigraphic series of China. On the strength of the investigation in coastal and offshore areas, the status of marine strata in China has been expounded. According to the developing situation of international stratigraphy and the characteristics of Chinese stratigraphic work, the contrast relation between regional stratigraphic units of China and GSSPs will be established in the future, which will improve the application value of GSSPs and the standard of regional stratigraphic division and correlation. In addition, the study of stratigraphy of the Precambrian, terrestrial basins and orogenic belts will be strengthened, the Stratigraphic Chart of China will be improved, the typical stratigraphic sections in China will be protected and the applied study of stratigraphy in the fields of oil and gas, solid minerals, etc. will be promoted. On the ground of these actions, stratigraphic research will continue to play a great role in the social and economic development of China.
LI Yingjie,WANG Jinfang,WANG Genhou,DONG Peipei,LI Hongyang,HU Xiaojia[10]（2018）在《Discovery of the Plagiogranites in the Diyanmiao Ophiolite, Southeastern Central Asian Orogenic Belt, Inner Mongolia, China and Its Tectonic Significance》文中认为In this study, plagiogranites in the Diyanmiao ophiolite of the southeastern Central Asian Orogenic Belt（Altaids） were investigated for the first time. The plagiogranites are composed predominantly of albite and quartz, and occur as irregular intrusive veins in pillow basalts. The plagiogranites have high SiO2（74.37–76.68 wt%） and low Al2O3（11.99–13.30 wt%）, and intensively high Na2O（4.52–5.49 wt%） and low K2O（0.03–0.40 wt%） resulting in high Na2O/K2O ratios（11.3–183）. These rocks are classified as part of the low-K tholeiitic series. The plagiogranites have low total rare earth element contents（∑REE）（23.62–39.77 ppm）, small negative Eu anomalies（δEu=0.44–0.62）, and flat to slightly LREE-depleted chondrite-normalized REE patterns（（La/Yb）N=0.68–0.76）, similar to N-MORB. The plagiogranites are also characterized by Th, U, Zr, and Hf enrichment, and Nb, P, and Ti depletion, have overall flat primitivemantle-normalized trace element patterns. Field and petrological observations and geochemical data suggest that the plagiogranites in the Diyanmiao ophiolite are similar to fractionation-type plagiogranites. Furthermore, the REE patterns of the plagiogranites are similar to those of the gabbros and pillow basalts in the ophiolite. In plots of SREE–SiO2, La–SiO2, and Yb–SiO2, the plagiogranites, pillow basalts, and gabbros show trends typical of crystal fractionation. As such, the plagiogranites are oceanic in origin, formed by crystal fractionation from basaltic magmas derived from depleted mantle, and are part of the Diyanmiao ophiolite. LA–ICP–MS U–Pb dating of zircons from the plagiogranites yielded ages of 328.6±2.1 and 327.1±2.1 Ma, indicating an early Carboniferous age for the Diyanmiao ophiolite. These results provide petrological and geochronological evidence for the identification of the Erenhot–Hegenshan oceanic basin and Hegenshan suture of the Paleo-Asian Ocean.
二、TIANJIN INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文开题报告）
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三、TIANJIN INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文提纲范文）
（2）Progress and Prospects of Salt Lake Research in China（论文提纲范文）
| 1 Introduction |
| 2 Saline Lake Sediments,Paleoclimate and Paleoenvironment Study |
| 2.1 Salt minerals as climatic indicators |
| 2.2 Arid and salt deposit center and its expansion period in the Quaternary in China |
| 2.3 The Quaternary pan-lake(overflow)period and paleoclimate on the Qinghai-Tibetan Plateau |
| 2.3.1 Evidence of Quaternary pan-lakes on the Qinghai-Tibet Plateau |
| 2.3.1. 1 Siling Co pan-lake area |
| 2.3.1. 2 Zabuye-Zhari Namco pan-lake area |
| 2.3.1. 3 Qaidam and South Kunlun pan-lake areas |
| 2.3.1. 4 Gozha Co-Tianshuihai pan-lake area |
| 2.3.1. 5 Lumajangdong Co-Bangong Co pan-lake area |
| 2.3.1. 6 Nam Co pan-lake |
| 2.3.2 Timing and extent of high lake levels of pan-lakes on the Qinghai-Tibet Plateau |
| 3 New Knowledge of Mineralization and Salting Theory of Saline Lakes on the Qinghai-Tibet Plateau |
| 3.1 Classification criteria for the hydrochemical types of salt lakes |
| 3.2 Hydrochemical zoning and mineral assemblages of salt lakes on the Qinghai-Tibet Plateau |
| 3.2.1 Hydrochemical zonation |
| 3.2.2 Mineral assemblages for different types of salt lakes |
| 3.3 Deposition models for salts |
| 3.3.1 Mineralization model for multi-level moderate-shallow lake chains |
| 3.3.2 Salt deposition in large scale multi-level lakes in deep basins |
| 3.3.3 Studies of salt minerals of the Tibetan Plateau |
| 3.4 Discovery of potassium-rich salt lakes and progress in the theory on continental potassium deposition |
| 3.4.1 Overview |
| 3.4.2 Framework of the continental potash deposition theory |
| 3.4.2. 1 The primary cause for potassium accumulation in continental salt lakes |
| 3.4.2. 2 The model for the enrichment and deposition of continental potash |
| 3.4.3 Application of the continental salt deposition theory |
| 3.5 Discovery of a new type of magnesium borate deposits and the new insight on boron deposition from cooling and dilution |
| 3.5.1 Boron deposits in Da Qaidam lake:ulexite-pinnoite deposits |
| 3.5.2 Magnesium-borate deposits in Chagcam Caka,Tibet |
| 3.5.3 Kurnakovite deposits in Nyêr Co,Tibet |
| 3.5.3. 1 Introduction |
| 3.5.3. 2 Ore-bearing Strata |
| 3.5.4 New knowledge on the genesis of new type Mg-borate deposits and the theory of salt precipitation via cooling with diluting in the Qinghai-Tibet Plateau |
| 4 Salt Lake Chemistry and Sylvite,Lithium Resource Development and Utilization |
| 4.1 Salt lake chemistry |
| 4.2 Sylvite resource development and utilization-two case from Qarham salt lake and Lop Nur salt lake |
| 4.2.1 Qarham salt lake industry |
| 4.2.2 Lop Nur salt lake industry |
| 4.3 Studies on utilization of lithium resources-a case of Zhabuye salt lake |
| 4.3.1 Saltpan preparation and control technology of lithium-rich brine |
| 4.3.2 Heat accumulation and lithium precipitation and crystallization in the solar pond |
| 5 Saline Lake Geo-ecology,Halophiles and Saline Lake Agriculture |
| 5.1 The briny region |
| 5.2 Salt marshes,saline and alkaline lands |
| 6 Prospect of Scientific and Technological Development on Salt Lakes in China |
| 7 Conclusions |
（3）Quantitative Geoscience and Geological Big Data Development:A Review（论文提纲范文）
| 1 International Quantitative Geoscience and Big Data Research |
| 2 Quantitative Geoscience and Geological Big Data Research in China |
| 2.1 National macro strategies and plans |
| 2.2 Quantitative mineral resource prediction and assessment theories and methods |
| 2.2.1“Triple-type”metallogenic prediction theory |
| 2.2.2 Metallogenic prediction theory based on integrated information |
| 2.2.3 Deposit modeling and integrated geological information prediction method |
| 2.2.4 Prospecting method based on cube prediction model |
| 2.3 Geoscience information software system |
| 2.4 Construction of geoscience information platform |
| Stage I:PC–Stand-alone Workstation |
| Stage II:Local Area Network–Internet Stage |
| 2.5 Application of quantitative geosciences and geological big data in China |
| 2.5.1 Informatization of basic geological data |
| 2.5.2 Quantitative prediction and prospecting of mineral resources |
| 2.5.3 Geological environment and disasters |
| (1)Early warning for geological disasters based on3S technology |
| (2)Geological 3D model technology-based disaster survey |
| 2.5.4 Digital Land |
| (1)“Digital Land”–“One Map”platform |
| (2)“Digital Land”–Develop integrated supervision system |
| (3)“Digital Land”–Construction of e-government land affairs platform |
| (4)“Digital Land”–Construction of land and resources information sharing platform |
| 2.5.5 Digital City |
| (1)3D urban geological survey and social services in Shanghai |
| (2)Construction and application of national Digital City geospatial framework technology system |
| (3)Construction of Digital City in Anhui |
| 3 Outlook |
| 4 Conclusion |
（4）Research Progress and the Main Achievements of The Regional Geology of China Preface（论文提纲范文）
| Introduction to The Regional Geology of China |
| Research Progress of the Project |
| Main Achievements of the Project |
| Congratulations and Acknowledgements |
（5）The Present Research and Prospect of Chinese Geosciences History（论文提纲范文）
| 1 The History and Present Situation of the Research on the History of International Geological Science |
| 1.1 The change of the content of the study |
| 1.2 Organizations and research institutes |
| 1.3 Publications and authors |
| 2 The Present Situation and Progress of the Study of the Chinese Geological Science History |
| 2.1 A brief account of the development of the Chinese geological science history |
| 2.2 Research institutes and research groups |
| 2.3 The guiding ideology of the research on the history of geological science |
| 2.4 Major progress in recent years |
| 2.4.1 Promote interaction between Chinese geological science and social development in China |
| 2.4.2 A study on the history of geological disciplines of China |
| 2.4.3 A study of geological characters |
| Kwong Yung Kong(1863-1965) |
| Woo Yang Tsang(1861-1939) |
| Gu Lang(1880-1939) |
| Lu Xun(1881-1936) |
| Wang Chongyou(1879-1985) |
| Zhang Hongzhao(1877-1951) |
| Ding Wenjiang(1887-1936) |
| Weng Wenhao(1889-1971) |
| Li Siguang(1889-1971) |
| R.Pumpelly(1837-1923) |
| Richthofen,Ferdinand von(1833-1905) |
| Amadeus Willian Grabau(1870-1946) |
| Johann Gunnay Andersson(1874-1960) |
| Prerre Teilhaya de Chardin(1881-1955) |
| 2.4.4 The study of history of ancient geological thoughts |
| 2.4.5 The study of the geological cause |
| 2.4.6 Research of the history of the communication of Chinese and foreign geological science |
| 3 Development Prospect |
| 4 Conclusion |
（7）俄罗斯城市可持续发展及其对中国城市的启示研究（论文提纲范文）
| 摘要 |
| ABSTRACT |
| CHAPTER Ⅰ Introduction |
| 1.1 Research background |
| 1.2 Research goal and objectives |
| 1.3 Literature review |
| 1.3.1 Concept of sustainable development |
| 1.3.2 Social-Economic aspects of regional planning and urban development in Russia |
| 1.4 Materials and methods |
| 1.4.1 Research framework |
| 1.4.2 Materials and methods |
| CHAPTER Ⅱ Concept of Sustainable Development |
| 2.1 Sustainable development |
| 2.1.1 Phenomenon 'climate change' |
| 2.1.2 Urbanization |
| 2.1.3 Relationship between climate change and urbanization |
| 2.1.4 International level commitments |
| 2.1.5 Conclusion |
| 2.2 Sustainable urban planning in Russian Federation |
| 2.2.1 Introduction |
| 2.2.2 Sustainable development in Russia |
| 2.2.3 Russian town-planning legislative base |
| 2.2.4 Russian national green building technical legislative base |
| 2.2.5 GIS Technology into the Russian town-planning practice |
| 2.2.6 Conclusion |
| 2.3 Sustainable urban planning in People's Republic of China |
| 2.3.1 Introduction |
| 2.3.2 Sustainable development in China |
| 2.3.3 Chinese urban planning legislative base National Garden City |
| 2.3.4 Chinese national green building technical legislative base |
| 2.3.5 Conclusion |
| References |
| CHAPTER Ⅲ Transformation of the Scientific Views on the Process of Urbanization |
| 3.1 Process of urbanization in Russian Federation |
| 3.1.1 Introduction |
| 3.1.2 Three waves of Russian urbanization |
| 3.1.3 First wave of urbanization1860s- |
| 3.1.4 Second wave of urbanization1926- |
| 3.1.5 Third wave of urbanization in1950s |
| 3.1.6 Conclusion |
| 3.2 Process of urbanization in People's Republic of China |
| 3.2.1 Introduction |
| 3.2.2 Three great historical transformations of China |
| 3.2.3 First historical transformation(1911) |
| 3.2.4 Second historical transformation(1949) |
| 3.2.5 Third historical transformation(1978) |
| 3.2.6 Conclusion |
| References |
| 3.3 Results of the comparative analysis of sustainable urban development in Russian Federation and People's Republic of China |
| 3.3.1 Introduction |
| 3.3.2 Has comparative analysis value? |
| 3.3.3 What is the valuable experience of both countries in the modern urban development? |
| 3.3.4 Conclusion |
| CHAPTER Ⅳ Socio-economic aspects of regional planning and urban development in Russian Federation |
| 4.1 Introduction |
| 4.2 Literature review |
| 4.3 Historical background |
| 4.4 All-Russia forum‘Strategic Planning in the Regions and Cities of Russia’ |
| 4.5 Inquire into the relationship between priorities of sustainable development,strategic planning and Russian socio-economic policy |
| 4.5.1 Strategic planning system of the Russian Federation |
| 4.5.2 Spatial Development Strategy of the Russian Federation to 2025 |
| 4.5.3 Interrelation of the documents of strategic and territorial planning of Russian Federation |
| 4.5.4 Russian state policy of innovation development |
| 4.6 Conclusion |
| References |
| CHAPTER Ⅴ Historical overview of the Soviet science cities development |
| 5.1 Introduction |
| 5.2 Historical overview of the science cities development1917-1980s |
| 5.2.1 Urban design trends in the science settlements creation,1930s |
| 5.2.2 Urban design trends in science cities establishment after the Great Patriotic War.The beginning period of the Cold War |
| 5.2.3 Urban design trends in the science cities establishment in1960-1970.The period of the formulation of a standard approach to design and construction |
| 5.2.4 Summing up the results of the Soviet period of the construction of the science cities of1930s-1980s |
| 5.3 Urban design trends in the science cities establishment in1990s |
| 5.4 Urban design trends in the science cities establishment after2010s |
| 5.5 Conclusion |
| References |
| CHAPTER Ⅵ Russian innovation infrastructure |
| 6.1 Introduction |
| 6.2 National innovation system of the Russian Federation |
| 6.3 Innovation Infrastructure:territorial level |
| 6.3.1 Innovation special economic zones |
| 6.3.2 Innovation and industrial clusters' |
| 6.4 Innovation infrastructure physical level:technoparks and business incubators |
| 6.4.1 Technoparks |
| 6.4.2 Technopark-leaders of the II National Russian Technoparks Ranking-2016 |
| 6.5 Conclusion |
| References |
| CHAPTER Ⅶ CASE OF STUDY:Skolkovo Innovation Center |
| 7.1 Introduction |
| 7.1.1 Skolkovo Innovation Center |
| 7.2 Aim of creating Skolkovo Innovation Center |
| 7.3 Types of infrastructure of the Skolkovo Innovation Center |
| 7.4 Results of international competition for Skolkovo IC master plan concept |
| 7.4.1 Finalist of international competition for Skolkovo IC Masterplan OMA |
| 7.4.2 Winner of international competition for Skolkovo IC master plan- AREP |
| 7.5 Structure of Skolkovo IC Town Planning Board |
| 7.6 Development strategy and documents of Skolkovo IC master plan |
| 7.7 Skolkovo IC infrastructure construction financial program |
| 7.8 Transport accessibility to Skolkovo IC |
| 7.9 Key institutions facilities of the Skolkovo IC |
| 7.9.1 Skoltech- Skolkovo Institute of Science and Technology |
| 7.9.2 Research and development centres of the Skolkovo IC District D |
| 7.9.3 Skolkovo Technopark building |
| 7.9.4 Business Center Amaltea(BC Gallery) |
| 7.9.5 IT-Cluster Business Park of the Skolkovo IC |
| 7.9.6 Transmashholding Corporate Research Center |
| 7.9.7 Hypercube the First Building of Skolkovo IC |
| 7.9.8 Skolkovo Business Center(MatRex) |
| 7.9.9 Sberbank Technopark |
| 7.10 Social infrastructure facilities of Skolkovo IC |
| 7.11 Housing facilities of Skolkovo IC |
| 7.11.1 Central Zone Z |
| 7.11.2 South District D |
| 7.11.3 Technopark District D |
| 7.12 Skolkovo IC landscape design |
| 7.13 Conclusion |
| CHAPTER Ⅷ Russian town-planning science in the context of socio-economic transformations |
| 8.1 Introduction |
| 8.2 Definition of the term"gradostroitelstvo" |
| 8.3 Historical overview of the town-planning science in Russia |
| 8.3.1 Socialist town-planning1917- |
| 8.3.2 Socialist town-planning1933- |
| 8.3.3 Socialist town-planning1941- |
| 8.3.4 Socialist town-planning1941- |
| 8.4 Theoretical foundations and unique traditions of town-planning science in Russia |
| 8.5 Russian fundamental research in the field of town-planning |
| 8.6 Course of town-planning in the Russian education system |
| 8.6.1 The town-planning faculty of the Moscow Architectural Institute(State Academy)MARHI |
| 8.6.2 Vysokovsky Graduate School of Urbanism |
| 8.6.3 Strelka Institute for Media,Architecture and Design |
| 8.6.4 MARCH Architecture School |
| 8.6.5 Summarizing the analysis of four urban planning schools in Russia |
| 8.7 Applied town-planning science |
| 8.7.1 Methods of town-planning analysis |
| 8.7.2 Interdisciplinary methods of town-planning analysis |
| 8.8 Conclusion |
| References |
| CONCLUSION |
| SUMMARY AND RECOMMENDATIONS FOR FURTHER STUDY AND PRACTICE |
| APPENDIX Ⅰ |
| APPENDIX Ⅱ |
| APPENDIX Ⅲ |
| APPENDIX Ⅳ |
| APPENDIX Ⅴ |
| APPENDIX Ⅵ |
| APPENDIX Ⅶ |
| APPENDIX Ⅷ |
| APPENDIX Ⅸ |
| APPENDIX Ⅹ |
| APPENDIX ⅩⅠ |
| APPENDIX ⅩⅡ |
| ACKNOWLEDGEMENTS |
| SCIENTIFIC ACHIVEMENTS |
| Appreciate |
（8）Structure Styles of Mesozoic-Cenozoic U-bearing Rock Series in Northern China（论文提纲范文）
| 1 Introduction |
| 2 Concept Introduction |
| 3 Structural Styles of U-bearing Rock Series in Typical Basins in the Western Segment of the CAMB |
| 3.1 Features of U-bearing rock series in the Chu-Saleisu Basin in Kazakhstan |
| 3.2 Features of the U-bearing rock series in the Central Kyzylkum U metallogenic province in Uzbekistan |
| 3.3 Features of the U-bearing rock series in the Dalmatov U deposit in Russia |
| 4 Structural Styles of U-bearing Rock Series of Main Mesozoic-Cenozoic Basins in Northern China |
| 4.1 Features of the U-bearing rock series in the Yili Basin |
| 4.2 Features of U-bearing rock series in the Junggar Basin |
| 4.3 Features of U-bearing rock series in the Tarim basin |
| 4.4 Features of U-bearing rock series in the Qaidam Basin |
| 4.5 Features of U-bearing rock series of the Ordos Basin |
| 4.6 Features of U-bearing rock series in the Er’lian Basin |
| 4.7 Features of U-bearing rock series in the Songliao Basin |
| 5 Discussions |
| 6 Conclusions |
（9）Status of Stratigraphy Research in China（论文提纲范文）
| 1 Overview of International Stratigraphic Research |
| 2 Research Status of Stratigraphy in China |
| 2.1 Ten GSSPs erected in China |
| 2.2 Standards for stratigraphic division and correlation established in China |
| 2.3 Great achievements in special research on stratigraphy |
| 2.4 Abundant data for stratigraphic research acquired in national land and resources survey projects |
| 3 Future Development of Stratigraphy in China |
| 3.1 To improve the standard of regional stratigraphic division and correlation |
| 3.2 To establish the contrasting relationship between regional stratigraphic units and GSSPs |
| 3.3 To strengthen the study of the Precambrian time scale |
| 3.4 To strengthen the study of terrestrial basins |
| 3.5 To further supply and improve the Stratigraphic Chart of China |
| 3.6 To promote the study of stratigraphy in orogenic belts |
| 3.7 To protect the typical stratigraphic sections |
| 3.8 To reinforce the applied study of stratigraphy in the fields of oil and gas,solid minerals,etc. |
| 4 Conclusions |
（10）Discovery of the Plagiogranites in the Diyanmiao Ophiolite, Southeastern Central Asian Orogenic Belt, Inner Mongolia, China and Its Tectonic Significance（论文提纲范文）
| 1 Introduction |
| 2 Geology and Petrography |
| 3 Analytical Methods |
| 3.1 Zircon U-Pb dating analyses |
| 3.2 Mineral geochemistry |
| 3.3 Major and trace elemental analyses |
| 4 Analytical Results |
| 4.1 LA-ICP-MS zircon U-Pb dating |
| 4.2 Mineral geochemistry |
| 4.3 Whole-rock geochemistry |
| 5 Discussion |
| 5.1 Origin of the plagiogranites |
| 5.2 Age of the Diyanmiao ophiolite and its implications |
| 6 Conclusions |
四、TIANJIN INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文参考文献）
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