地质编图与GIS制图专栏

中国海域1:100万地质地球物理MapGIS制图

展开
  • 1. 国土资源部海洋油气资源与环境地质重点实验室, 青岛 266071;
    2. 青岛海洋地质研究所, 青岛 266071;
    3. 广州海洋地质调查局, 广州 510075;
    4. 中国国土资源航空物探遥感中心, 北京 100083;
    5. 青岛麦普吉科技有限公司, 青岛 266071
温珍河(1963-),男,硕士,研究员,主要从事海洋区域地质编图、石油地质资源评价、海洋地理信息系统等研究工作.E-mail:wenzhh@sina.com

收稿日期: 2011-07-15

  修回日期: 2011-12-01

  网络出版日期: 2011-12-25

基金资助

国土资源地质大调查专项"我国海域1:100万地质地球物理系列图"工作项目(1212010511302).

Digital Compilation of 1 :1 000 000 Geological and Geophysical Map Series of China and Adjacent Regions on MapGIS Platform

Expand
  • 1. The Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology, Qingdao 266071, China;
    2. Qingdao Institute of Marine Geology, Qingdao 266071, China;
    3. Guangzhou Marine Geological Survey, Guangzhou 510075, China;
    4. China Aero Geophysical Survey and Remote Sensing Center, Beijing 100083, China;
    5. Qingdao Technical Company of MAPGIS, Qingdao 266071, China

Received date: 2011-07-15

  Revised date: 2011-12-01

  Online published: 2011-12-25

摘要

中国海域1:100万地质地球物理系列图包括布格重力异常图、空间重力异常图、磁力异常图、表层沉积物分布图和区域构造图5种图件.利用数字化编图技术对新旧资料进行同化处理和标准化处理,在编图的过程中,采取多种技术手段确保编图质量,并进行了GIS数据库的构建工作.地理底图和各专题图件均在MapGIS基础平台上以点、线、面三种图元类型表示,根据实际材料和图面内容进行分层设计、分层构建、统一成图的技术路线,为日后资料使用和图件修编奠定了良好基础.以MapGIS为平台,可以很好地完成地质地球物理系列编图任务.

本文引用格式

温珍河, 张训华, 杨金玉, 尹延鸿, 邱燕, 王乃东, 张明 . 中国海域1:100万地质地球物理MapGIS制图[J]. 地球信息科学学报, 2011 , 13(6) : 750 -757 . DOI: 10.3724/SP.J.1047.2011.00750

Abstract

We try to summarize the techniques used for digital map compilation for the marine territory of China in this paper. The new version of 1:1000000 geological and geophysical map series of China Seas and Adjacent Regions include five maps, i.e. the Bouguer gravity anomaly map, spatial gravity anomaly map, magnetic anomaly map, surface sediment distribution map and regional geotectonic map. The mapping area also covers part of the land and adjacent areas in addition to China seas. The geological and geophysical maps have not been renewed since the last map series published 20 years ago. And the maps published then were drawn by hands. Either precision or quality is not able to meet the demand of users. This time, we compile maps with MapGIS as a platform. Various equipments, such as computers, advanced digitizers and other facilities, are adopted for the map compilation. At first, we, using digital map compilation technology, standardized and unified all the data, including both the old and new data, and the data collected with different methods and from different channels. Rationale fitting technique and reliable coordinates transform are used to guarantee the quality of the maps. In the process of map compilation, a GIS database has been constructed. All the maps, including the base map and specific maps, were drawn on the MapGIS platform using point, line and polygons as legends and layers were designed and constructed according to the data available and the contents the maps need. The use of the MapGIS platform made us possible to ensure the precision of the maps and enhance the efficiency of map compilation. It is believed that the compilation and publication of the new version of 1:1 000 000 Geological and Geophysical Map Series of China Seas and Adjacent Regions will certainly help the readers better understand the basic geological regulations of China.

参考文献

[1] 刘光鼎 主编.中国海区及邻域地质地球物理系列图(1:5 000 000)[M].北京:科学出版社,1992.

[2] 许厚泽,王海瑛,陆洋,等.利用卫星测高重力数据推求中国近海及邻域大地水准面起伏和重力异常研究[J].地球物理学报.1999,42(4):445-471.

[3] 张明华, 张家强.现代卫星测高重力异常分辨能力分析及在海洋资源调查中的应用[J].物探与化探.2005,29 (4): 296-303.

[4] 黄谟涛,翟国君,管铮,等.利用卫星测高重力数据反演海洋重力异常研究[J].测绘学报.2001,30(2):179-184.

[5] 辽宁省地质矿产局.辽宁省区域地质志[M].北京:地质出版社,1989.

[6] 山东省地质矿产局.山东省区域地质志[M].北京:地质出版社,1991.

[7] 江苏省地质矿产局.江苏省及上海市区域地质志[M].北京:地质出版社,1984.

[8] 浙江省地质矿产局.浙江省区域地质志[M].北京:地质出版社,1989.

[9] 福建省地质矿产局.福建省区域地质志[M].北京:地质出版社,1985.

[10] 安徽省地质矿产局.安徽省区域地质志[M].北京:地质出版社,1987.

[11] 武汉中地数码科技有限公司.MAPGIS地理信息系统使用手册-数字制图篇.2008.

[12] 韩坤英,丁孝忠,范本贤,等.MAPGIS在建立地质图数据库中的应用[J].地球学报,2005,26(6):587-590.

[13] 李勤,王万银,崔莉.MapGIS在地球物理数据成图中的应用[J].地球科学与环境学报,2008,30(2):200-203.

[14] 郝天珧,刘伊克,徐万哲.黄海和邻区重磁场及区域构造特征[J].地球物理学进展,1998,13(1):27-39.

[15] 邱燕.南海中南部表层沉积物黏土矿物分布及控制因素[J].海洋地质与第四纪地质,2007,27(5):2-7.

[16] 邱燕,彭学超,朱本铎,等.南海1:100万永暑礁幅海洋区域地质调查成果[J].地质通报,2006,25(3): 419-425.

[17] 尹延鸿,张训华,温珍河,等.中国东部海区及邻域区域构造图的编制方法及地质构造单元划分[J].海洋学报,2008,30(6):99-105.

[18] 周蒂,刘海龄,陈汉宗.南沙海区及其周缘中-新生代岩浆活动及构造意义[J].大地构造与成岩学,2005,29(3):354-363

[19] 张翀,吴世敏,丘学林.南海南部海区前陆盆地形成与演化[J].海洋地质与第四纪地质,2007,27(1):61-70

[20] 万天丰.中国东部中、新生代板内变形构造应力场及其应用[M].北京:地质出版社,1993.

[21] Chia-Yen Ku, Shu-Kun Hsu. Crustal Structure and Deformation at the Northern Manila Trench between Taiwan and Luzon Islands[J]. Tectonophysics, 2009,466:229-240.

[22] Jean-Claude Sibuet, Shu-Kun Hsu, Xavier Le Pichon, et al. East Asia Plate Tectonics since 15 Ma: Constraints from the Taiwan Region[J]. Tectonophysics, 2002,344:103-134.

[23] Wang T K, Chen M K, Lee C S and Xia K Y. Seismic Imaging of the Transitional Crust across the Northeastern Margin of the South China Sea[J]. Tectonophysics, 2006,412:237-254.
文章导航

/