4.7 Article

Hainan mantle plume produced late Cenozoic basaltic rocks in Thailand, Southeast Asia

Journal

SCIENTIFIC REPORTS
Volume 8, Issue -, Pages -

Publisher

NATURE PUBLISHING GROUP
DOI: 10.1038/s41598-018-20712-7

Keywords

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Funding

  1. Scientific and Technological Innovation Project - Qingdao National Laboratory for Marine Science and Technology [2016ASKJ05]
  2. National Natural Science Foundations of China [41776070, U1606401, 41230960, 41322036]
  3. National Programme on Global Change and Air-Sea Interaction [GASI-GEOGE-02, GASI-01-02-01-04]
  4. AoShan Talents Program
  5. Young scholar of Shuxingbei fund of FIO [2016S01]
  6. Taishan Scholarship from Shandong Province
  7. Australian Research Council
  8. Qingdao National Laboratory for Marine Science and Technology

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Intraplate volcanism initiated shortly after the cessation of Cenozoic seafloor spreading in the South China Sea (SCS) region, but the full extent of its influence on the Indochina block has not been well constrained. Here we present major and trace element data and Sr-Nd-Pb-Hf isotope ratios of late Cenozoic basaltic lavas from the Khorat plateau and some volcanic centers in the Paleozoic Sukhothai arc terrane in Thailand. These volcanic rocks are mainly trachybasalts and basaltic trachyandesites. Trace element patterns and Sr-Nd-Pb-Hf isotopic compositions show that these alkaline volcanic lavas exhibit oceanic island basalt (OIB)-like characteristics with enrichments in both large-ion lithophile elements (LILE) and high field strength elements (HFSEs). Their mantle source is a mixture between a depleted Indian MORB-type mantle and an enriched mantle type 2 (EMII). We suggest that the post-spreading intraplate volcanism in the SCS region was induced by a Hainan mantle plume which spread westwards to the Paleozoic Sukhothai arc terrane.

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