Paleomagnetism of Triassic bedded chert from Japan for determining the age of an impact ejecta layer deposited on peri-equatorial latitudes of the paleo-Pacific Ocean: A preliminary analysis

Koji Uno, Daisuke Yamashita, Tetsuji Onoue, Daiki Uehara

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5 Citations (Scopus)

Abstract

Bedded chert samples from the Norian (Upper Triassic) Sakahogi section of the Mino Terrane in the Inuyama area, southwest Japan, have been collected for paleomagnetic study in order to determine the age of an impact ejecta layer interbedded within it and the paleolatitude of its deposition. Thermal demagnetization of the bedded chert samples revealed four distinct remanent magnetization components. The last demagnetized component with both polarities is interpreted to be the primary magnetization, which produced the first magnetostratigraphic data of the middle to upper Norian from Panthalassa, consistent with Tethyan magnetostratigraphic sections. Tie points were derived from paleomagnetic and paleontological data, from which the stratigraphic position of the ejecta layer was compared with the astronomically tuned geomagnetic polarity time scale (APTS). The age of ejecta layer is estimated to be about 212. Ma. This magnetostratigraphic age is consistent with the radiometric age of the Manicouagan impact that formed the second largest known crater in the Phanerozoic at Quebec, Canada. The results of this study, as well as previous studies, suggest that the chert section, which includes the ejecta layer, was deposited within a paleolatitude range of 0.3-14.4°N. This indicates that the material ejected by the Manicouagan impact event reached near the equatorial region of the paleo-Pacific Ocean.

Original languageEnglish
Pages (from-to)59-67
Number of pages9
JournalPhysics of the Earth and Planetary Interiors
Volume249
DOIs
Publication statusPublished - Dec 1 2015

Fingerprint

paleomagnetism
Pacific Ocean
chert
ejecta
Japan
Triassic
Norian
paleolatitude
ocean
polarity
Quebec
magnetization
equatorial regions
demagnetization
remanent magnetization
Phanerozoic
Canada
craters
crater
terrane

All Science Journal Classification (ASJC) codes

  • Astronomy and Astrophysics
  • Geophysics
  • Physics and Astronomy (miscellaneous)
  • Space and Planetary Science

Cite this

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title = "Paleomagnetism of Triassic bedded chert from Japan for determining the age of an impact ejecta layer deposited on peri-equatorial latitudes of the paleo-Pacific Ocean: A preliminary analysis",
abstract = "Bedded chert samples from the Norian (Upper Triassic) Sakahogi section of the Mino Terrane in the Inuyama area, southwest Japan, have been collected for paleomagnetic study in order to determine the age of an impact ejecta layer interbedded within it and the paleolatitude of its deposition. Thermal demagnetization of the bedded chert samples revealed four distinct remanent magnetization components. The last demagnetized component with both polarities is interpreted to be the primary magnetization, which produced the first magnetostratigraphic data of the middle to upper Norian from Panthalassa, consistent with Tethyan magnetostratigraphic sections. Tie points were derived from paleomagnetic and paleontological data, from which the stratigraphic position of the ejecta layer was compared with the astronomically tuned geomagnetic polarity time scale (APTS). The age of ejecta layer is estimated to be about 212. Ma. This magnetostratigraphic age is consistent with the radiometric age of the Manicouagan impact that formed the second largest known crater in the Phanerozoic at Quebec, Canada. The results of this study, as well as previous studies, suggest that the chert section, which includes the ejecta layer, was deposited within a paleolatitude range of 0.3-14.4°N. This indicates that the material ejected by the Manicouagan impact event reached near the equatorial region of the paleo-Pacific Ocean.",
author = "Koji Uno and Daisuke Yamashita and Tetsuji Onoue and Daiki Uehara",
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T1 - Paleomagnetism of Triassic bedded chert from Japan for determining the age of an impact ejecta layer deposited on peri-equatorial latitudes of the paleo-Pacific Ocean

T2 - A preliminary analysis

AU - Uno, Koji

AU - Yamashita, Daisuke

AU - Onoue, Tetsuji

AU - Uehara, Daiki

PY - 2015/12/1

Y1 - 2015/12/1

N2 - Bedded chert samples from the Norian (Upper Triassic) Sakahogi section of the Mino Terrane in the Inuyama area, southwest Japan, have been collected for paleomagnetic study in order to determine the age of an impact ejecta layer interbedded within it and the paleolatitude of its deposition. Thermal demagnetization of the bedded chert samples revealed four distinct remanent magnetization components. The last demagnetized component with both polarities is interpreted to be the primary magnetization, which produced the first magnetostratigraphic data of the middle to upper Norian from Panthalassa, consistent with Tethyan magnetostratigraphic sections. Tie points were derived from paleomagnetic and paleontological data, from which the stratigraphic position of the ejecta layer was compared with the astronomically tuned geomagnetic polarity time scale (APTS). The age of ejecta layer is estimated to be about 212. Ma. This magnetostratigraphic age is consistent with the radiometric age of the Manicouagan impact that formed the second largest known crater in the Phanerozoic at Quebec, Canada. The results of this study, as well as previous studies, suggest that the chert section, which includes the ejecta layer, was deposited within a paleolatitude range of 0.3-14.4°N. This indicates that the material ejected by the Manicouagan impact event reached near the equatorial region of the paleo-Pacific Ocean.

AB - Bedded chert samples from the Norian (Upper Triassic) Sakahogi section of the Mino Terrane in the Inuyama area, southwest Japan, have been collected for paleomagnetic study in order to determine the age of an impact ejecta layer interbedded within it and the paleolatitude of its deposition. Thermal demagnetization of the bedded chert samples revealed four distinct remanent magnetization components. The last demagnetized component with both polarities is interpreted to be the primary magnetization, which produced the first magnetostratigraphic data of the middle to upper Norian from Panthalassa, consistent with Tethyan magnetostratigraphic sections. Tie points were derived from paleomagnetic and paleontological data, from which the stratigraphic position of the ejecta layer was compared with the astronomically tuned geomagnetic polarity time scale (APTS). The age of ejecta layer is estimated to be about 212. Ma. This magnetostratigraphic age is consistent with the radiometric age of the Manicouagan impact that formed the second largest known crater in the Phanerozoic at Quebec, Canada. The results of this study, as well as previous studies, suggest that the chert section, which includes the ejecta layer, was deposited within a paleolatitude range of 0.3-14.4°N. This indicates that the material ejected by the Manicouagan impact event reached near the equatorial region of the paleo-Pacific Ocean.

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