Wang Jiliang et al. (2000): Age estimation of the mid-Pleistocene microtektite event in the South China Sea; a case showing the complexity of the sea-land correlation

Leg/Site/Hole:
ODP 124 772
Identifier:
2001-058018
georefid

Creator:
Wang Jiliang
Tongji University, Laboratory of Marine Geology, Shanghai, China
author

Zhao Quanhong
author

Cheng Xinrong
author

Wang Rujian
author

Wang Pinxian
author

Identification:
Age estimation of the mid-Pleistocene microtektite event in the South China Sea; a case showing the complexity of the sea-land correlation
2000
Chinese Science Bulletin
Science Press, Beijing, China
45
24
2277-2280
The present study confirms the stratigraphical position of microtektite layer being clearly located below the Brunhes/Matuyama (B/M) boundary. Based on the sedimentation rate derived from the stable isotopic and magnetic data of ODP Site 772A, cores 17957 and 17959 in the South China Sea, the age of the mid-Pleistocene impact event was estimated at 10-12 ka earlier than the Brunhes-Matuyama polarity reversal. However, the microtektites were found above the measured B/M boundary in the loess profile due to the downward deviation of the measured B/M boundary from its true position. This demonstrates the complexity of paleo-magnetic records in the loess profiles which, in turn, causes the confusion in the sea-land stratigraphic correlation.
English
Serial
Coverage:Geographic coordinates:
North:16.3900
West:119.4200East: 119.4200
South:16.3900

Quaternary geology; Geochronology; Brunhes Chron; case studies; Cenozoic; cores; geochronology; Leg 124E; magnetization; Matuyama Chron; microtektites; middle Pleistocene; natural remanent magnetization; North Pacific; Northwest Pacific; Ocean Drilling Program; ODP Site 772; Pacific Ocean; paleomagnetism; Pleistocene; Quaternary; remanent magnetization; South China Sea; tektites; upper Cenozoic; upper Quaternary; West Pacific;

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