| 中国及邻区海陆大地构造图编制完成 |
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| 引用本文： | 易善锋
,沈显杰.中国及邻区海陆大地构造图编制完成[J].地质科学,1982,0(1):121-122. |
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| 作者姓名： | 易善锋 沈显杰 |
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| 摘 要： | 由中国科学院地质研究所张文佑教授主编的我国第一张中国及邻区海陆大地构造图已经编制完成。1981年,中国科学院地学部邀请近50名有关的学者和专家,在青岛对该图进行了评审。大家一致赞赏编制这一图件的首创精神,认为该图指导思想明确,基础资料扎实,编图方法严谨,图面表达清晰,是目前国内外少有的、水平较高的一张海陆大地构造图。他们建议尽早予以出版,使之对提高我国地质科学研究水平、阐明我国资源能源分布规律和进行区域稳定性分析等方面,作出重要贡献。
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| 关 键 词： | , |
THE MAP OF MARINE AND CONTINENTAL TECTONICS OF CHINA AND ITS ENVIRONS COMPILED |
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| Yi Shanfeng,Shen Hsienehieh.THE MAP OF MARINE AND CONTINENTAL TECTONICS OF CHINA AND ITS ENVIRONS COMPILED[J].Chinese Journal of Geology,1982,0(1):121-122. |
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| Authors: | Yi Shanfeng Shen Hsienehieh |
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| Abstract: | The compilation of the first map of marine and continental tectonics of China and its environs on the scale 1:5,000,000 with Prof.Zhang Wenyou,the prominent geotec-tonist of international publicity,as its chief compiler,has been recently completed.An appraisal meeting for it sponsered by the Geoscience Division,Chinese Academy of Sciences was held in Qingdao in June,1981.Nearly 50 scientists and specialists of related subjects were invited to attend the meeting.This map was accepted by all of the attendants with high evaluation in the authors’initiative,such as in the consistency of the guideline,solidness of the base materials used and the rigorous methodology in the compilation,as well as in the clearness of the map expression.Nearly 30 scientists and research-associates from the Institute of Geology,the Institute of Oceanography and the Oceanology Institute of the South China sea,Aeade-mia Sinica,the Departments of Geology of Peking University and Nanjing University,the Institute of Geology of Xingjiang Geological Bureau,the Hebei Bureau of Seismology and other related institutions took part in the map compiling.At the meeting it is generally agreed that combining the method of the geomechanical and geohistorical analyses this map has made every effort to ascertain the origin and development,the mode of motion and categeories of the faults and their systems,and thus to acquire a comprehensive interpretation of the evolution of continental and oceanic crust and its transitional type.As a result,a considerable promotion has been made in development of the theory of fault-block tectonics.A further consolidation,expansion and gradual consummation of the fault-block theory can be expected on the basis of properly summarized knowledge in forms of a high-qualified map as presented now with abudant data of continental and marine geology,geophysics,deepseated geology and Precambrian,isotope geochronology,petrochemistry and remote sensing geology.At present,a final revision of the above-mentioned map and a series of supplementary maps with the accompanied instruction has been prepared with reference to the helpful comments marked at the meeting and will be published before long by the "Science" Press both in China and abroad to meet the requirements of a wide circle of the relevant fields. |
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