An integrated biostratigraphy (conodonts and foraminifers) and chronostratigraphy (paleomagnetic reversals, magnetic susceptibility, elemental chemistry, carbon isotopes and geochronology) for the Permian-Upper Triassic strata of Guandao section, Nanpanjiang Basin, south China


Lehrmann D. J., Stepchinski L., ALTINER D., Orchard M. J., Montgomery P., Enos P., ...Daha Fazla

JOURNAL OF ASIAN EARTH SCIENCES, cilt.108, ss.117-135, 2015 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 108
  • Basım Tarihi: 2015
  • Doi Numarası: 10.1016/j.jseaes.2015.04.030
  • Dergi Adı: JOURNAL OF ASIAN EARTH SCIENCES
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.117-135
  • Anahtar Kelimeler: Permian-Triassic, Biostratigraphy, Conodonts, Foraminifera, Carbon isotopes, Paleomagnetic, Geochronology, China, GEOMAGNETIC POLARITY TIMESCALE, GUIZHOU PROVINCE, GREAT BANK, LAGENIDE FORAMINIFERS, ZIRCON GEOCHRONOLOGY, STRATOTYPE SECTION, MARINE ECOSYSTEMS, BIOTIC RECOVERY, MASS EXTINCTION, POINT GSSP
  • Orta Doğu Teknik Üniversitesi Adresli: Evet

Özet

The chronostratigraphy of Guandao section has served as the foundation for numerous studies of the end-Permian extinction and biotic recovery in south China. Guandao section is continuous from the Permian-Triassic boundary to the Upper Triassic.