<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     naa a22        4500</leader>
  <controlfield tag="001">510754481</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180411083117.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">180411e20130801xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s13131-013-0338-9</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s13131-013-0338-9</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Sand wave deposition in the Taiwan Shoal of China</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Yi Hu, Jian Chen, Jiang Xu, Liming Wang, Haidong Li, Huaishan Liu]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">The Taiwan Shoal is the convex terrain in the southern Taiwan Strait, the largest strait in China. In 2006 and 2007, 21 samples and more than 200-km sub-bottom data as well as 80-km near shore side-scan sonar data were gotten, which gave an initial image of the boundaries of the Taiwan Shoal and revealed the internal structure of the sand waves in this area. The results showed that the major component of the sediment samples was sand, and sand waves occurred everywhere in this area, which closely followed the range of the Taiwan Shoal as we know. The western boundary of the Taiwan Shoal thus reaches the 30 m isobaths near the shore, and as a result, its area potentially covers approximately 12 800-14 770 km2. The sand waves have different shapes under the complex ocean dynamics, and the height of sand waves in the near shore is usually smaller than that in the Taiwan Shoal. The number of sand waves ranged from1-5 per kilometer, with more waves in the isobath-intensive area, suggesting the importance of topography for the formation of sand waves. The stratigraphic structure under the seabed has parallel bedding or cross bedding, and large dipping groove bedding can be seen locally in different parts, which may be the result of terrestrial deposition since the Late Pleistocene.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg, 2013</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">sand waves</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">sub-bottom profile</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">grain size</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Taiwan Shoal</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Hu</subfield>
   <subfield code="D">Yi</subfield>
   <subfield code="u">College of Geosciences, Ocean University of China, 266100, Qingdao, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Chen</subfield>
   <subfield code="D">Jian</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Xu</subfield>
   <subfield code="D">Jiang</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Wang</subfield>
   <subfield code="D">Liming</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Li</subfield>
   <subfield code="D">Haidong</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Liu</subfield>
   <subfield code="D">Huaishan</subfield>
   <subfield code="u">College of Geosciences, Ocean University of China, 266100, Qingdao, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Acta Oceanologica Sinica</subfield>
   <subfield code="d">Springer Berlin Heidelberg</subfield>
   <subfield code="g">32/8(2013-08-01), 26-34</subfield>
   <subfield code="x">0253-505X</subfield>
   <subfield code="q">32:8&lt;26</subfield>
   <subfield code="1">2013</subfield>
   <subfield code="2">32</subfield>
   <subfield code="o">13131</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s13131-013-0338-9</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/s13131-013-0338-9</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Hu</subfield>
   <subfield code="D">Yi</subfield>
   <subfield code="u">College of Geosciences, Ocean University of China, 266100, Qingdao, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Chen</subfield>
   <subfield code="D">Jian</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Xu</subfield>
   <subfield code="D">Jiang</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Wang</subfield>
   <subfield code="D">Liming</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Li</subfield>
   <subfield code="D">Haidong</subfield>
   <subfield code="u">Third Institute of Oceanography, State Oceanic Administration, Coast and Ocean Environmental Geology Open Laboratory, 361005, Xiamen, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Liu</subfield>
   <subfield code="D">Huaishan</subfield>
   <subfield code="u">College of Geosciences, Ocean University of China, 266100, Qingdao, China</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Acta Oceanologica Sinica</subfield>
   <subfield code="d">Springer Berlin Heidelberg</subfield>
   <subfield code="g">32/8(2013-08-01), 26-34</subfield>
   <subfield code="x">0253-505X</subfield>
   <subfield code="q">32:8&lt;26</subfield>
   <subfield code="1">2013</subfield>
   <subfield code="2">32</subfield>
   <subfield code="o">13131</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
