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- W2392586093 abstract "Rocks were dredged from 3 stations in central and western Nansha block,southern South China Sea. Large quantities of brown--colored argillaceous and calcareousnodules in dark--grey mud were recovered from the station NS99--l7 at the NE edge of theSunda shelf, indicating the sea level there has raised for more than 150m after the for-mation of the nodules at oxidizing 1ittora1--beach environment possibly during the lastglaciation. At the station NS99--57 of the Kangtai Shoal, highly alterated and porouschalky limestone contalns benthic foraminifera, suggesting an early--middle Miocenereefal buildup. At the station NS99--52 along the slope of a seamount about 55 km NE ofthe Yongshu Reef, reefal limestone with Quaternary calcareous nannofossils and phos-phorite pebbles composed of globigerina and other bioclasts and collophane were collect-ed. Calcareous nannofossils in the pehbles have ages most of Mid Eocene to Oligoceneand subordinary Quaternary. Their phosphoric composition indicates bathyal to pelagicenvironment. These dredged rock samples provide important hard for thestudy of geological history and for the assessment of hydrocarbon potential. In particu-lar, the obtained Paleogene bathyal to pelagic phosphorite near the border of the SWsubbasin of the South China Sea not only verify the widespread existence of Paleogenemarine sediments in the Nansha block, but also provide supplemental evidence for datingthe opening of the South China Sea." @default.
- W2392586093 created "2016-06-24" @default.
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- W2392586093 date "2002-01-01" @default.
- W2392586093 modified "2023-09-25" @default.
- W2392586093 title "PHOSPHATE AND OTHER ROCKS DREDGEDFROM CENTRAL AND WESTERN NANSHA BLOCK,SOUTHERN SOUTH CHINA SEA" @default.
- W2392586093 hasPublicationYear "2002" @default.
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