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物探与化探  2008, Vol. 32 Issue (6): 581-585    
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世界磁异常图
张昌达
中国地质大学 地球物理与空间信息学院, 湖北 武汉 430074
WORLD MAGNETIC ANOMALY MAP
ZHANG Chang-da
Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
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摘要 

第一版的世界磁异常图,此前称为世界数字化磁异常图(WDMAM),于2007年7月在第24届IUGG大会上正式公布。这幅图的编制工作是由国际地磁学与大气物理学协会(IAGA)和世界地质图委员会(CGMW)合作完成,得到联合国教科文组织(UNESCO)赞助,由UNESCO和CGMW出版。这幅图表示的地壳磁异常数据,是50多年来全世界积累的航空、海上和卫星磁测所获得的,汇合成5 km×5 km网格,换算到大地水准面上5 km。WDMAM的公布将进一步推动地壳和上地幔地质构造的研究,并且有助于资源的勘查。第二版WDMAM正在编制中。

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Abstract

The first edition of The Magnetic Anomaly Map of the World, formerly named World Digital Magnetic Anomaly Map (WDMAM), was made public at the 24th IUGG General Assembly in July, 2007. The compilation of the map was conducted jointly by IAGA and CGMW with the support of UNESCO, and the map was published by the UNESCO and the CGMW. The crustal magnetic field anomaly data were obtained from airborne survey, shipborne survey and satellite acquisition all over the world in a period of more than 50 years. The data merged into a composite 5 km×5 km grid and a nominal height above geoid of 5 km. The publication of the WDMAM will give an impetus to researches on the geological structure of the crust and the uppermost lithosphere, and is conducive to resource exploration. The second edition of the WDMAM is now under compilation.

收稿日期: 2008-02-27      出版日期: 2008-12-24
: 

P631

 
作者简介: 张昌达(1933-),男,武汉市人,教授。1954年毕业于吉林大学物理系,1955年毕业于物探研究生班,目前正致力于物探新方法研究。
引用本文:   
张昌达. 世界磁异常图[J]. 物探与化探, 2008, 32(6): 581-585.
ZHANG Chang-da. WORLD MAGNETIC ANOMALY MAP. Geophysical and Geochemical Exploration, 2008, 32(6): 581-585.
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https://www.wutanyuhuatan.com/CN/      或      https://www.wutanyuhuatan.com/CN/Y2008/V32/I6/581

[1] Ravat D,Ghidella M, Maus S, et al .Toward the world digital magnetic anomaly map (WDMAM)[J].Eos Trans AGU, 2003,84(46), Fall Meet Suppl,Abstract GP21D-01.
[2] Hemant K,Thebault E,Mandea M,et al.World digital magnetic anomaly map:progress report[J].Geophysical Research Abstracts, 2006,8:03609.
[3] Purucker M.New frontiers in magnetic field interpretation and modeling: examples from the world digital magnetic anomaly map[J].Eos Trans AGU, 2006,87(52), Fall Mee. Suppl, Abstract GP42A-01 INVITED.
[4] Maus S,Sazonova T,Hemant K,et al.National geophysical data center candidate for the world digital magnetic anomaly Map[J].Geochem Geophys Geosyst, 8, 2007,Q06017, doi:10.1029/2007GC001643.
[5] Korhonen J V and the WDMAM 1.0-team.World digital magnetic anomaly map (WDMAM), First Edition[J].Geophysical Research Abstracts, 2007,9:10406.
[6] Hamoudi M, Thebault E,Lesur V,et al.Geoforschungs zentrum anomaly magnetic map (GAMMA): candidate model for the WDMAM[J].Geophysical Research Abstracts, 2007,9:08414.
[7] Hemant K,Thébault E,Mandea M,et al.Magnetic anomaly map of the world: merging airborne, marine and ground-based data sets[J].Earth and Planetary Science Letters, 2007, 260:1-2, 56-71.
[8] Korhonen J V,Fairhead J D,Hamoudi M,Hemant K, Lesur V,Mandea M,Maus S,Purucker M,Ravat D,Sazonova T,Thebault E.Magnetic Anomaly Map of the World (and associated DVD), Scale:1:50 000 000, 1st edition, Commission for the Geological Map of the World[M].Paris, France,2007.
[9] Maus S,Lühr H,Rother M, et al.Fifth generation lithospheric magnetic field model from CHAMP satellite measurements[M].Geochem Geophys Geosyst, 2007,8(5).
[10] Moritz H.Advanced Physical Geodesy[M].Herbert Wichmann Verlag, Karlsruhe,1980.
[11] Wessel P,Smith W.New improved version of generic mapping tools released[J].EOS transactions of the American Geophysical Union, 1998,79: 579.
[12] Sabaka T J,Olsen N, Purucker M E.Extending comprehensive models of the Earth's magnetic field with Oersted and CHAMP data[J].Geophys J Int, 2004,159:521.
[13] Müller R D,Roest W R,Royer J Y,et al.Digital isochrons of the world's ocean floor[J].J Geophys Res,1997,102:3211.
[14] Gee J S,Kent D V.Source of oceanic magnetic anomalies and the geomagnetic polarity time scale, Chapter 12, in Kono M, ed., Volume 5. Geomagnetism: Treatise on Geophysics[M].Amsterdam, Elsevier, in press, 2007.
[15] Kent D V,Gradstein F M. Jurassic to Recent chronology//Vogt P R,Tucholke B E.The Western North Atlantic Region, Geology of North America Volume M (Geological Society America, Boulder),1986.
[16] Milligan P.World digital magnetic anomaly map now available[J].Preview, 2007,130:16.
[17] Reeves C.The first magnetic anolmaly map of the world [J].The Leading Edge,2008,27(1):32.

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