New Magnetic Anomaly Map of the East Asia with Some Preliminary Tectonic Interpretations

被引:22
作者
Doo, Wen-Bin [1 ]
Hsu, Shu-Kun [1 ]
Armada, Leo [1 ]
机构
[1] Natl Cent Univ, Dept Earth Sci, Jhongli, Taiwan
来源
TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES | 2015年 / 26卷 / 01期
关键词
Magnetic anomaly map; East Asia; West Philippine Basin; South China Sea; Tectonics; SOUTH-CHINA-SEA; NORTHERN CONTINENTAL-MARGIN; RYUKYU SUBDUCTION ZONE; SOUTHEASTERN CHINA; OKINAWA TROUGH; PASSIVE MARGIN; FAULT SYSTEM; EVOLUTION; TAIWAN; MAGMATISM;
D O I
10.3319/TAO.2014.08.19.07(GRT)
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Magnetic data provides basic information for geological and geophysical interpretation. In this study we compile recently collected (57 cruises survey) and old (published and open access) magnetic data. This compilation includes land, marine and aeromagnetic data acquired in the East Asia region. The newly acquired magnetic data are mainly concentrated mainly in the South China Sea (SCS) (especially in the northern continental shelf), the northwestern part of the West Philippine Basin (WPB), and the East China Sea. The updated magnetic dataset is gridded with a spacing of one arc-minute. The new magnetic map provides new insights into the tectonic setting of East Asia. Analysis of the compiled data reveals several regional anomaly patterns: (1) the NE-SW trending high positive magnetic anomaly zone extending from southwest Taiwan to the area about 114.5 degrees E and 22 degrees N is pronounced; but it is less continuous southwest of the Penghu islands. In addition, the orientation of this high linear magnetic zone changes slightly in 118.5 degrees E, 22.5 degrees N from N60 degrees E - N50 degrees E. (2) Between the Gagua Ridge (GR) and the Luzon-Okinawa Fracture Zone (LOFZ) the marine magnetic stripes of the WPB exhibit a NW-SE orientation. This suggests that the seafloor spreading could be related to the first stage of the WPB east of the LOFZ. (3) The Urdaneta and Amami plateaus are associated with high magnetization zones. These high magnetization zones extend northwestward and are subducting beneath the Ryukyu Trench.
引用
收藏
页码:73 / 81
页数:9
相关论文
共 51 条
[1]  
[Anonymous], 1973, Molecular Properties, DOI [DOI 10.1016/B978-0-12-456002-4.X5001-1, DOI 10.1016/B978-0-12-490920-5.X5001-7]
[2]   Segmentation in gravity and magnetic anomalies along the US East Coast passive margin: Implications for incipient structure of the oceanic lithosphere [J].
Behn, MD ;
Lin, J .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2000, 105 (B11) :25769-25790
[3]   A NEW BRANCH OF THE PHILIPPINE FAULT SYSTEM AS OBSERVED FROM AEROMAGNETIC AND SEISMIC DATA [J].
BISCHKE, RE ;
SUPPE, J ;
DELPILAR, R .
TECTONOPHYSICS, 1990, 183 (1-4) :243-264
[4]   Subduction-zone magnetic anomalies and implications for hydrated forearc mantle [J].
Blakely, RJ ;
Brocher, TM ;
Wells, RE .
GEOLOGY, 2005, 33 (06) :445-448
[5]   Improving the quality of marine geophysical track line data: Along-track analysis [J].
Chandler, Michael T. ;
Wessel, Paul .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2008, 113 (B2)
[6]  
Chang M. D., 1992, PET GEOL TAIWAN, V27, P237
[7]  
Chang YC, 2011, J MAR SCI TECH-TAIW, V19, P1
[8]   Crustal evolution of southeastern China: Nd and Sr isotopic evidence [J].
Chen, JF ;
Jahn, BM .
TECTONOPHYSICS, 1998, 284 (1-2) :101-133
[9]  
EMERY KO, 1970, AM ASSOC PETR GEOL B, V54, P44
[10]   International Geomagnetic Reference Field: the eleventh generation [J].
Finlay, C. C. ;
Maus, S. ;
Beggan, C. D. ;
Bondar, T. N. ;
Chambodut, A. ;
Chernova, T. A. ;
Chulliat, A. ;
Golovkov, V. P. ;
Hamilton, B. ;
Hamoudi, M. ;
Holme, R. ;
Hulot, G. ;
Kuang, W. ;
Langlais, B. ;
Lesur, V. ;
Lowes, F. J. ;
Luehr, H. ;
Macmillan, S. ;
Mandea, M. ;
McLean, S. ;
Manoj, C. ;
Menvielle, M. ;
Michaelis, I. ;
Olsen, N. ;
Rauberg, J. ;
Rother, M. ;
Sabaka, T. J. ;
Tangborn, A. ;
Toffner-Clausen, L. ;
Thebault, E. ;
Thomson, A. W. P. ;
Wardinski, I. ;
Wei, Z. ;
Zvereva, T. I. .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2010, 183 (03) :1216-1230