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【期刊论文】The Global Stratotype Section and Point (GSSP) of The Permian-Triassic Boundary
殷鸿福, Yin Hongfu, Zhang Kexin, Tong Jinnan, Yang Zunyi, Wu Shunbao
Reprinted from Episodes Vol. 24, No. 2, pp. 102-114, 2001,-0001,():
-1年11月30日
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【期刊论文】TETHYS—AN ARCHIPELAGIC OCEAN MODEL
殷鸿福, YIN Hongfu
Proc. 30 Int'l Geol Congr. Vol. 11, pp. 91-97,-0001,():
-1年11月30日
Three models for Tethys are discussed. Based on recent data from China and adjacent areas, it is concluded that an archipelagic ocean model for Tethys accords with paleomagnetic and biogeographic data that Eurasia and Gondwana were widely apart, and also accords with sedimentary data that deep ocean deposits were few, because the vast distance were filled by islands.
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殷鸿福, H. Yin, W. C. Sweet, B. E. Glenister, G. Konnar, H. Kozur, N. D. Newell, J. Sheng, Z. Yang, Y. D. Zakharov
Newsl. Stratigr. 34 (2) 81-108, 2 Pl., 3 Fig., 3Tab. Berlin Stuttgart, 11, 12, 1996,-0001,():
-1年11月30日
The base of bed 27c in the Meishan section Changxing County, Zhejiang Province, China, is recommended as GSSP for the basal boundary of the Triassic System. The Meishan section is easily accessible, well exposed, and records continuous marine sedimentation from the Changxingian(latest Permian) into the Early Triassic. The global boundary stratotype point is placed at the first occurrence of the conodont species Hindeodus parvus in the evolutionary lineage latidentatus-parvus-turgida-isarcica, which is transitional between Hindeodus and Isarcicella. Integrated stratigraphic study of the Meishan section includes radiometric dating, and chemo, sequence, eco, and event-stratigraphy. The latter involves the records of possible impact events as well as volcanic, anoxic, and transgressive events. The latter three studies have identified events the appear to be recorded on a pan-Tethyan or even a global scale.
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