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