Comment on barckhausen et al., 2014 - evolution of the South China sea: Revised ages for breakup and seafloor spreading

Jih Hsin Chang, Tung Yi Lee, Ho Han Hsu, Char Shine Liu

研究成果: 雜誌貢獻評論/辯論同行評審

19 引文 斯高帕斯(Scopus)

摘要

We re-examined the cessation of the South China Sea seafloor spreading by using radioactive dating and fossil assemblage of the ETO, and the Te-derived age. The youngest available age for the fragment of the South China Sea is ~15Ma and is more consistent with those suggested by previous studies. Moreover, recent IODP Expedition preliminary results suggested that the hemipelagic claystone layer stratigraphically bounded by igneous sequences of massive lava flow rock is Early Miocene in age. Therefore, the previous interpretations are more inclusive than those provided by Barckhasen etal. (2014) and indicate that a slow spreading ridge was more plausible to have occurred during the seafloor spreading of the South China Sea.

原文英語
頁(從 - 到)676-678
頁數3
期刊Marine and Petroleum Geology
59
DOIs
出版狀態已發佈 - 2015 一月 1

ASJC Scopus subject areas

  • Oceanography
  • Geophysics
  • Geology
  • Economic Geology
  • Stratigraphy

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