Episodes

Vol. 29 No.4 December 2006

Journal of International Geoscience

Published by the International Union of Geological Sciences

by Liangshu Shu1, Michel Faure2, Shaoyong Jiang1, Qun Yang3, and Yujing Wang3

SHRIMP zircon U-Pb age, litho- and biostratigraphic
analyses of the Huaiyu Domain in South China
〞 Evidence for a Neoproterozoic orogen, not Late Paleozoic-Early Mesozoic collision

1 State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China.
2 ISTO, Universit谷 d'Orl谷ans, B. P. 6759, 45067 Orl谷ans, Cedex 2, France.
3 Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China.

Abstract

In the last few decades, the Late Paleozoic每Early Mesozoic tectonic evolution of South China has been quite controversial. The focus of debate is on both the age of ophiolites and the Late Paleozoic每Early Mesozoic geological and geodynamic environment. The Huaiyu Domain is located in the NE part of South China and exposes numerous significant geological features that are keys to understand the tectonics of South China. In this paper, we present some new evidence on stratigraphy, petrology and SHRIMP zircon U-Pb geochronology, and together with other geological and geochemical data available in the literature, and the following conclusions are suggested: 1) The eastern Jiangnan ophiolites belt, dated at 858㊣11 Ma by SHRIMP zircon U-Pb method, was generated during the Neoproterozoic, but not the Late Paleozoic; 2) The sedimentary rocks associated with these oceanic rocks do not contain radiolarians but Neoproterozoic acritarchs; 3) During Permian每Early Triassic times, the Huaiyu Domain was dominantly characterized by a shallow sea depositional environment since deep sea sediments are absent; and 4) The pre-Devonian tectonics of South China has been reworked by late polyphase tectonism through the Triassic and the Cretaceous periods. A Late Paleozoic每Early Mesozoic deep marine domain floored by oceanic crust never existed in the study area. The geochronological and structural data do not comply with a Late Paleozoic每 Early Mesozoic South China Ocean.

﹛

    RETURN