一、YICHANG INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文文献综述）
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[1]（2016）在《Status of Stratigraphy Research in China》文中提出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.
王训练,周洪瑞,王振涛,沈阳,于子栋,杨志华[2]（2019）在《扬子板块西北缘早中泥盆世构造演化:来自略阳地区踏坡组岩石学、锆石年代学和微量元素组成的约束》文中研究说明碧口地块北缘下中泥盆统踏坡组的物源长期被认为来自碧口地块新元古界基底——碧口岩群,但一直缺少碎屑锆石物源数据的支持。本文对略阳地区泥盆系踏坡组不同层位的3个碎屑岩样品开展了系统的岩石学、锆石岩相学及其U-Pb定年和微量元素组成研究。锆石晶体特征对比分析显示,研究样品存在两种类型的锆石:普遍发育变质增生边的碎屑锆石（剖面北段样品）和不发育变质增生边的典型岩浆成因的碎屑锆石（剖面南、中段样品）。前者显示2个年龄峰值（～2.5 Ga主峰、～2.0 Ga次峰）,还形成了2473±24 Ma的上交点年龄和359±84 Ma的下交点年龄,而后者两个样品有着一致的年龄峰值（～2.0 Ga主峰、～2.5 Ga次峰和～1.39 Ga微小峰值）。3个样品的谐和年龄均大于1.3 Ga,并不能限定踏坡组的沉积时代,且均不支持其物源主要来自碧口岩群的传统认识。碎屑锆石地球化学判别图解指示它们的源岩主要为形成于造山带环境中的花岗岩类（花岗闪长岩和英云闪长岩）、基性岩和钾镁煌斑岩。基于样品中的岩屑类型,结合区域地质、古流向、锆石年龄对比和源岩判别,认为踏坡组的原始物源来自位于扬子板块北缘的太古宙—古元古代基底（鱼洞子杂岩和崆岭杂岩）,并且鱼洞子杂岩在踏坡组沉积后期曾大面积出露/抬升。同时表明碧口地块可能至少在早中泥盆世就与扬子板块拼合在一起了。
Jiayu RONG,Yi WANG,Renbin ZHAN,Junxuan FAN,Bing HUANG,Peng TANG,Yue LI,Xiaole ZHANG,Rongchang WU,Guangxu WANG,Xin WEI[3]（2019）在《Silurian integrative stratigraphy and timescale of China》文中认为Silurian is a period with the shortest duration in Phanerozoic except for the Neogene and Quaternary. It represents an important and unique interval when the biotic diversity recovered quickly after the end-Ordovician mass extinction, different paleoplates or terranes conjoined, big oceans disappeared or narrowed, climate and sea level changed frequently, global biotic provincialism became weaker, some primitive plants started to occupy the land. Silurian is also the first system of which all the chronostratigraphic stratotypes（i.e. the GSSPs） including four series and seven stages were established by the International Subcommission on Silurian Stratigraphy（ISSS）. Nonetheless, during the post-GSSP studies conducted by ISSS in the middle1980 s, some Silurian GSSPs were found to have some congenital defects such as no index fossils available that hinder the high resolution subdivision and correlation on a regional or global scale. In this paper, based on the latest development of Silurian study in China, the progress in biostratigraphy, chronostratigraphy, event stratigraphy（such as facies differentiation, heterochrony of black shales, marine red beds, carbonate rocks and reefs）, chemostratigraphy, and tectonic stratigraphy（e.g., widespread of the late Silurian rocks in South China and its tectonic implication） are systematically summarized. Some existing problems and the areas to be focused in future work are also discussed. It is suitable for chronostratigraphic study to concentrate not only on the boundary but also doing multidisciplinary analysis on the biotic, chemical, magnetic, environmental, and chronologic aspects, in order to enhance the reliability and the potential for regional and global correlation of a certain GSSP.Some important achievements are expected in these areas in the Silurian study in China:（1） ecostratigraphy and basin analysis of the Llandovery, and the correlation of integrative stratigraphy with a high resolution;（2） establishment of the Wenlock to Pridoli chronostratigraphic framework;（3） the chemo-and magnetic stratigraphy and the age of some key intervals and horizons;（4）further investigation on paleogeography and plate tectonics; and（5） origin and early evolution of the terrestrial ecosystem. Some new breakthroughs might occur in the restudy on some of those problematic GSSPs of some particular series and stages.
晁红丽,任建德,吕际根,谢朝永,李莹琪,李瑞强,焦静华[4]（2020）在《河南省三川幅1:50000地质图数据库》文中提出河南省三川幅（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[5]（2016）在《Progress and Prospects of Salt Lake Research in China》文中提出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 Baoguo,ZHANG Jiuchen,YANG Mengmeng[6]（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.
郭振威,赖健清,张可能,毛先成,王智琳,郭荣文,邓浩,孙平贺,张绍和,于淼,崔益安,柳建新[7]（2020）在《中南大学地球科学进展与前沿（英文）》文中进行了进一步梳理中南大学地质资源与地质工程一级学科自主创立了国际领先的地洼学说、伪随机多频电磁场理论及广域电磁勘探系统,在壳体大地构造学、地电场勘探理论与装置系统、多因复成成矿理论、三维成矿预测、复杂地层钻井技术等领域形成了具有国际影响的中南学派。2000年以来,伪随机电磁法勘探系统和广域电磁法勘探系统在国内外开展了广泛的推广应用,其中"均匀广谱伪随机电磁法及其应用"于2006年获得国家技术发明二等奖、"大深度高精度广域电磁勘探技术与装备"于2018年获得国家技术发明一等奖。本学科是危机矿山深边部接替资源勘探、地质和地球物理有机结合并直接服务于国民经济主战场的国家级重点学科。20年来,本学科以创立的成矿与找矿理论为指导,以自主研制的国家领先的电磁勘探系统为手段,在国内外矿山和成矿区带的深边部资源勘探中大显身手,在国内外众多矿山找到了一大批矿产资源,缓解了大批矿山的资源危机,取得了巨大的经济社会效益。本学科还在复杂地层钻进技术与极端地层钻具研制理论与技术、地质灾害监测与防治、三维可视化定位定量预测等方面的成果在国内享有盛誉。
WANG Chenghui,WANG Denghong,XU Jue,YING Lijuan,LIU Lijun,LIU Shanbao[8]（2015）在《A Preliminary Review of Metallogenic Regularity of Gold Deposits in China》文中认为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.
MAO Jianren1,LI Zilong2,ZHAO Xilin1,ZHOU Jie1,YE Haimin1,and ZENG Qitao3 1 Nanjing Institute of Mineral Resources,Nanjing 210016,China 2 Department of Earth Sciences,Zhejiang University,Hangzhou 310027,China 3 Department of Earth Sciences,Nanjing University,Nanjing 210093,China[9]（2010）在《Geochemical characteristics,cooling history and mineralization significance of Zhangtiantang pluton in South Jiangxi Province,P.R. China》文中进行了进一步梳理The zircon SHRIMP dating of the Zhangtiantang granite gave an age of 159±7 Ma.,which shows that the granite was produced at the early Late Jurassic.The Ar-Ar plateau ages of biotite and K-feldspar from the Zhangtiantang pluton are 153.2±1.1 Ma and 135.8±1.2 Ma,respectively.The Ar-Ar anti-isochrone ages of biotite and K-feldspar are 152.5±1.7Ma and 135.4±2.7Ma,respectively.The ages represent the isotopic closure ages of minerals in the pluton.The Zhangtiantang granites are regarded as peraluminous crust-derived type granites to possess the typical geochemical characteristics of calc-alkaline rocks on continental margin,with enriched Si,K,Al（average value of A/CNK as 1.18）,HREE,Rb,U,and Th,heavily depleted V,Cr,Co,Ni,Ti,Nb-Ta,Zr,Sr,P,and Ba,strongly negative Eu and common corundum normative（average value of C as 1.84）.The εNd（t） values of the Zhangtiantang granite are-5.84 to-7.79,and t2DM values are 1.69 to 1.83 Ga,which indicates partial melting of continental-crust metamorphic sedimentary rocks during the Middle Proterozoic.The cooling history of the Zhangtiantang granitic pluton indicates that the cooling velocity of pluton was faster（about 67℃ /Ma） from zircon（158 Ma） to biotite（152 Ma）,and was slower（about12℃ /Ma） from biotite（152.5 Ma） to K-feldspar（135.8 Ma）.It can be deduced that the temporal gap（about 10 Ma） between the granite formmation and W-Sn mineralization in South China may be related to ordinary magma-hydrothermal processes by the variational cooling curve of the pluton.The Zhangtiantang pluton was formed in a compressive setting,with differentiation evolution and mineralization occurring in a relative relaxation setting.
唐一昂,赖健清,杨牧,梅嘉靖,刘启,吴剑,谌后成,郭兰萱,胡理芳,和秋姣[10]（2017）在《广东韶关市一六钨矿床流体包裹体特征及成矿作用》文中进行了进一步梳理一六钨矿大地构造位置位于南岭成矿带中段南缘,粤北曲仁盆地西南缘,是粤北地区近年来重要的找矿勘查成果之一。矿床为典型的矽卡岩矿床,矿体赋存于上泥盆统帽子峰组矽卡岩以及NWW向钾长石-石英-白钨矿脉和云母石英脉中。通过野外观察和镜下研究,本文将成矿过程分为矽卡岩期（A）和热液期（B）,矽卡岩期可以分为早期矽卡岩阶段（A1）、晚期矽卡岩阶段（A2）、钾长石英白钨矿阶段（A3）,热液期可以分为云母石英脉阶段（B1）和石英碳酸盐阶段（B2）。矿区包含4种类型的包裹体:含子矿物三相包裹体（Ⅰ型）、气液两相水溶液包裹体（Ⅱ型）、CO2水溶液三相包裹体（Ⅲ型）、纯CO2包裹体（Ⅳ型）,Ⅰ型包裹体仅见于A3阶段;Ⅱ型、Ⅲ型以及Ⅳ型包裹体在A3和B1阶段石英中均有发育,在A3和B1阶段白钨矿中还发育Ⅱ型包裹体。A3阶段Ⅰ型包裹体完全均一温度为162381℃,盐度为30.1%45.4%（wt%NaClequiv,下同省略）,Ⅱ型包裹体完全均一温度为154363℃,盐度为1.49%11.0%,Ⅲ型包裹体完全均一温度为290390℃,盐度为2.20%6.88%;B1阶段Ⅱ型包裹体完全均一温度为152381℃,盐度为1.65%9.32%,Ⅲ型包裹体完全均一温度为281378℃,盐度为2.00%8.82%。激光拉曼探针分析表明,A3阶段和B1阶段流体中存在H2O、CO2、CH4和少量CO32-,指示流体处于还原的环境。包裹体完全均一温度—盐度关系图表明,数据点主要集中于三个区域:a区对应早期出溶成因的高盐度流体,b区反映流体发生了不混溶作用,c区反映早期高盐度流体与低盐度地下水混合特征。各区包裹体代表了岩浆期后残余原始流体不同阶段的演化产物。通过Ⅰ型包裹体计算得出的成矿压力范围为86.0415.8MPa,用Ⅱ、Ⅳ型包裹体对成矿压力进行校正得出,A3阶段成矿压力范围为86115MPa,成矿温度为176279℃;B1阶段成矿压力范围为5593 MPa,成矿温度为160228℃,估算成矿深度范围为3.624.26km。研究认为,流体在演化早期存在局部高压,流体不混溶作用要比外来流体混入更早发生,而流体混入促进了流体的不混溶作用。流体物理化学条件的改变、外来流体混入以及流体不混溶作用是引起钨矿沉淀的主要原因。
二、YICHANG INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文开题报告）
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实验法：通过主支变革、控制研究对象来发现与确认事物间的因果关系。
文献研究法：通过调查文献来获得资料，从而全面的、正确的了解掌握研究方法。
实证研究法：依据现有的科学理论和实践的需要提出设计。
定性分析法：对研究对象进行“质”的方面的研究，这个方法需要计算的数据较少。
定量分析法：通过具体的数字，使人们对研究对象的认识进一步精确化。
跨学科研究法：运用多学科的理论、方法和成果从整体上对某一课题进行研究。
功能分析法：这是社会科学用来分析社会现象的一种方法，从某一功能出发研究多个方面的影响。
模拟法：通过创设一个与原型相似的模型来间接研究原型某种特性的一种形容方法。
三、YICHANG INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文提纲范文）
（1）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 |
（2）扬子板块西北缘早中泥盆世构造演化:来自略阳地区踏坡组岩石学、锆石年代学和微量元素组成的约束（论文提纲范文）
| 1 区域地质概况 |
| 2 踏坡组地层特征与样品描述 |
| 3 分析方法 |
| 4 结果 |
| 4.1 锆石晶体特征 |
| 4.2 锆石微量元素组成特征 |
| 4.3 锆石U-Pb年龄 |
| 5 讨论 |
| 5.1 踏坡组碎屑岩的物源 |
| 5.2 碧口地块北缘踏坡组的形成模式 |
| 6 结论 |
（3）Silurian integrative stratigraphy and timescale of China（论文提纲范文）
| 1. Introduction |
| 2. Global Silurian chronostratigraphy and re-lated problems |
| 3. Global Silurian timescale |
| 4. General features of the Silurian rocks of each paleoplate in China |
| 4.1 South China |
| 4.2 North China |
| 4.3 Tarim |
| 4.4 Hinggan-Altay |
| 4.5 West Junggar-Northern Tianshan |
| 4.6 Qaidam |
| 4.7 Lhasa |
| 4.8 Sibumasu (including western Yunnan) |
| 4.9 Indo-China (including southern Yunnan) |
| 5. Silurian biostratigraphy and chronostrati-graphy of China |
| 5.1 Llandovery |
| 5.2 Wenlock, Ludlow, and Pridoli |
| 5.3 Other fossils |
| 6. Differentiative distribution of Silurian litho-facies and their controlling factors in China |
| 6.1 Black shales |
| 6.2 Shallow marine clastic red beds |
| 6.3 Carbonates and reefal facies |
| 7. Characters and evidences of the Silurian tectonic stratigraphy in China |
| 8. Preliminary report on Silurian chemostrati-graphic study in China |
| 9. Problems and prospects |
| 9.1 Integrative stratigraphy |
| 9.2 Paleobiology |
| 9.3 The use of numerical methods and statistical soft-wares |
| 9.4 Chemostratigraphy and event stratigraphy |
| 9.5 Geologic chronology |
| 9.6 Paleogeography |
| 9.7 Sedimentological facies |
| 9.8 Early terrestrial ecosystem |
（5）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 |
（6）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 |
（9）Geochemical characteristics,cooling history and mineralization significance of Zhangtiantang pluton in South Jiangxi Province,P.R. China（论文提纲范文）
| 1 Introduction |
| 2 Geology and petrology of the pluton and its relation with W mineralization |
| 2.1 Geology and petrology of the pluton |
| 2.2 Relationship between the pluton and W miner-alization |
| 3 Analytical methods |
| 3.1 Zircon U-Pb SHRIMP dating |
| 3.2 Single mineral Ar-Ar analytical method |
| 3.3 Element geochemistry |
| 3.4 Sr-Nd isotopes |
| 4 Results |
| 4.1 Geochronology |
| 4.2 Geochemistry |
| 4.3 Isotope geochemistry |
| 5 Discussion |
| 5.1 Thermal evolution history |
| 5.2 Petrogenesis |
| 5.3 Tectonic environment |
| 6 Conclusions |
（10）广东韶关市一六钨矿床流体包裹体特征及成矿作用（论文提纲范文）
| 1 成矿地质背景 |
| 2 样品采集及研究方法 |
| 3 流体包裹体研究 |
| 3.1 岩相学特征 |
| 3.2 流体包裹体显微测温结果 |
| 3.2.1 钾长石英白钨矿阶段包裹体测温特征 |
| 3.2.2 云母石英脉阶段包裹体测温特征 |
| 3.3 激光拉曼探针分析 |
| 4 讨论 |
| 4.1 成矿流体特征 |
| 4.2 成矿压力及深度 |
| 4.3 成矿流体演化特征 |
| 4.4 成矿作用分析 |
| 5 结论 |
四、YICHANG INSTITUTE OF GEOLOGY AND MINERAL RESOURCES——ACHIEVEMENTS OF RESEARCH（论文参考文献）
- [1]Status of Stratigraphy Research in China[J]. 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. Acta Geologica Sinica（English Edition）, 2016(04)
- [2]扬子板块西北缘早中泥盆世构造演化:来自略阳地区踏坡组岩石学、锆石年代学和微量元素组成的约束[J]. 王训练,周洪瑞,王振涛,沈阳,于子栋,杨志华. 地质学报, 2019(12)
- [3]Silurian integrative stratigraphy and timescale of China[J]. Jiayu RONG,Yi WANG,Renbin ZHAN,Junxuan FAN,Bing HUANG,Peng TANG,Yue LI,Xiaole ZHANG,Rongchang WU,Guangxu WANG,Xin WEI. Science China（Earth Sciences）, 2019(01)
- [4]河南省三川幅1:50000地质图数据库[J]. 晁红丽,任建德,吕际根,谢朝永,李莹琪,李瑞强,焦静华. 中国地质, 2020(S1)
- [5]Progress and Prospects of Salt Lake Research in China[J]. 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. Acta Geologica Sinica（English Edition）, 2016(04)
- [6]The Present Research and Prospect of Chinese Geosciences History[J]. CHEN Baoguo,ZHANG Jiuchen,YANG Mengmeng. Acta Geologica Sinica（English Edition）, 2016(04)
- [7]中南大学地球科学进展与前沿（英文）[J]. 郭振威,赖健清,张可能,毛先成,王智琳,郭荣文,邓浩,孙平贺,张绍和,于淼,崔益安,柳建新. Journal of Central South University, 2020(04)
- [8]A Preliminary Review of Metallogenic Regularity of Gold Deposits in China[J]. WANG Chenghui,WANG Denghong,XU Jue,YING Lijuan,LIU Lijun,LIU Shanbao. Acta Geologica Sinica（English Edition）, 2015(02)
- [9]Geochemical characteristics,cooling history and mineralization significance of Zhangtiantang pluton in South Jiangxi Province,P.R. China[J]. MAO Jianren1,LI Zilong2,ZHAO Xilin1,ZHOU Jie1,YE Haimin1,and ZENG Qitao3 1 Nanjing Institute of Mineral Resources,Nanjing 210016,China 2 Department of Earth Sciences,Zhejiang University,Hangzhou 310027,China 3 Department of Earth Sciences,Nanjing University,Nanjing 210093,China. Chinese Journal of Geochemistry, 2010(01)
- [10]广东韶关市一六钨矿床流体包裹体特征及成矿作用[J]. 唐一昂,赖健清,杨牧,梅嘉靖,刘启,吴剑,谌后成,郭兰萱,胡理芳,和秋姣. 地质学报, 2017(10)