Acta Oceanologica Sinica

, 30:75

The formation and tectonic evolution of Philippine Sea Plate and KPR

  • Yinxia Fang
  • Jiabiao Li
  • Mingbi Li
  • Weiwei Ding
  • Jie Zhang
Article

DOI: 10.1007/s13131-011-0135-2

Cite this article as:
Fang, Y., Li, J., Li, M. et al. Acta Oceanol. Sin. (2011) 30: 75. doi:10.1007/s13131-011-0135-2

Abstract

The Philippine Sea Plate has an extremely special tectonic background. As an oceanic plate, it is almost entirely surrounded by subduction zones with complex internal tectonic features. On the basis of enormous published literature, this paper offers a comprehensive overview of the tectonic and evolution history of the Philippine Basin and the Kyushu-Palau Ridge (KPR) in the Philippine Sea Plate, and discusses the geological features of KPR. Referring to relevant definitions of various “ridges” stipulated in United Nations Convention on the Law of the Sea, so the KPR is believed to be a remnant arc formed during the opening of the Parece Vela and Shikoku Basins in the Philippine Sea Plate. It is a submarine ridge on oceanic plate rather than a submarine elevation. And thus, it is not a natural component of the Japan continental margin.

Key words

Philippine Sea Plate West Philippine Basin KPR submarine ridge 

Copyright information

© The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg 2011

Authors and Affiliations

  • Yinxia Fang
    • 1
  • Jiabiao Li
    • 1
  • Mingbi Li
    • 1
  • Weiwei Ding
    • 1
  • Jie Zhang
    • 1
  1. 1.The Second Institute of OceanographyState Oceanic AdministrationHangzhouChina

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