Late Cretaceous stratigraphy, Songliao Basin, NE China: SK1 cores

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• 作者：Xiaoqiao Wan ; Jing Zhao ; Robert W. Scott ; Pujun Wang ; Zihui Feng ; Qinghua Huang ; Dangpeng Xi
• 关键词：Late Cretaceous ; Biostratigraphy ; Chronostratigraphy ; Songliao Basin
• 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
• 出版年：2013
• 出版时间：1 September, 2013
• 年：2013
• 卷：385
• 期：Complete
• 页码：31-43
• 全文大小：532 K

文摘

The Songliao Basin is the largest Cretaceous oil and gas-producing lacustrine basin in China, with its greatest aerial extent in the middle Cretaceous. A coring program (SK1) has to date yielded 2485.89 m of continuous core (96.46 % recovery) and provides significant material for Cretaceous research. The sequence of the core consists mainly of lacustrine sandstone, dark grey mudstone, shale and oil-shale. The Upper Cretaceous stratigraphic section has been subdivided into the Quantou, Qingshankou, Yaojia, Nenjiang, Sifangtai and Mingshui formations in ascending order. Late Cretaceous microfossils are diverse and abundant. A detailed biostratigraphic study has subdivided the sequence into high precision biozones: 21 ostracode assemblages, 10 phytoplankton assemblages, 7 palynological zones and 4 charophyta assemblages, respectively. In addition, marine foraminifera were first discovered from the basin. Three ²⁰⁶Pb/²³⁸U ages and one ⁴⁰Ar/³⁹Ar age were analysed. Ten local magnetozones have been recognised in the SK1 (North), and two magnetozones have been indicated in the SK1 (South). Based on biostratigraphy, high-resolution magnetostratigraphy and SIMS U-Pb zircon analyses, the SK1 stratigraphy is correlated with Upper Cretaceous stages in the International Geologic Time Scale. The upper part of the Quantou Formation is the lower Turonian; the Qingshankou Formation is the upper Turonian-lower Coniacian; the Yaojia Formation is from the upper Coniacian to middle Santonian; the Nenjiang Formation is the upper Santonian to middle Campanian; the Sifangtai Formation is limited to the upper Campanian; and the Mingshui Formation is the uppermost Campanian to Maastrichtian. It is likely that the upper part of the Mingshui Formation belongs to the Paleocene, and the K/Pg boundary is within the Member 2 of the Mingshui Formation around the depth of 328 m by new micropalaeontologic and magnetostratigraphic data.