JOPC ›› 2016, Vol. 18 ›› Issue (2): 173-184. doi: 10.7605/gdlxb.2016.02.013

• LITHOFACIES PALAEOGEOGRAPHY AND SEDIMENTOLOGY • Previous Articles     Next Articles

Palaeo-water characteristics of the Member 1 of Paleogene Shahejie Formation in southern Nanpu sag, Bohai Bay Basin

Du Qingxiang1,2, Guo Shaobin2, Shen Xiaoli1, Cao Zhonghong3, Zhang Xiaolong3, Li Yuanshu3   

  1. 1 College of Earth Science and Engineering,Shandong University of Science and Technology,Qingdao 266590,Shandong
    2 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083
    3 Research Institute of Exploration and Development,Jidong Oilfield Company,PetroChina, Tangshan 063004,Hebei
  • Received:2015-01-27 Online:2016-04-01 Published:2016-04-01
  • Contact: Guo Shaobin,born in 1962,is a professor and Ph.D. supervisor. He is mainly engaged in sequence stratigraphy,reservoir and petroleum resource prediction and evaluation. E-mail: guosb58@126.com.
  • About author:Du Qingxiang,born in 1984,is a postdoctor in Shandong University of Science and Technology. His major is mineral resource prospecting and exploration. E-mail: geoduqingxiang@qq.com.

渤海湾盆地南堡凹陷南部古近系沙河街组一段古水体特征*

杜庆祥1,2,郭少斌2,沈晓丽1,曹中宏3,张晓龙3,李媛姝3   

  1. 1 山东科技大学地球科学与工程学院,山东青岛 266590
    2 中国地质大学(北京)能源学院,北京 1000833 中国石油冀东油田公司勘探开发研究院,河北唐山 063004
  • 通讯作者: 郭少斌,男,1962年生,教授,博士生导师,主要从事层序地层、储集层和油气资源预测与评价工作。E-mail: guosb58@126.com。
  • 作者简介:杜庆祥,男,1984年生,博士后,矿产普查与勘探专业。E-mail: geoduqingxiang@qq.com。

Abstract: The palaeo-water characteristics of the Paleogene Shahejie Formation in Nanpu sag of Bohai Bay Basin was poorly studied. Taking the Member 1 of Shahejie Formation in southern Nanpu sag as an example,we studied the palaeosalinity and palaeo-water depth by many means. Based on special algae fossils and chemical element ratios including Sr/Ba and Rb/K,the palaeosalinity was interpreted as brackish water to semi ̄saline water. The palaeoclimate was humid with fluctuation by analyzing Sr/Cu ratio and sporopollen fossils. The relative palaeo-water depth was reconstructed according to the change of Mn/Fe ratio,kerogen types,algae fossils and Tulotomoides. By synthetic analysis with the authigenic clay minerals,sedimentary structure and sedimentary facies,the palaeo-water depth interval was calculated by weighted average method. The results show that it was shallow water sedimentary environment with the quantitative palaeo-water depth ranging from 4,m to 15,m during the depositional period of the top of middle submember of Member 1 of Shahejie Formation in Nanpu sag. During the depositional period of lower submember of Member 1 of Shahejie Formation, the palaeo-water depth changed from 4 m to 30 m. It is indicated that the palaeosalinity and palaeo-water depth depended relatively on the palaeoclimate and ancient terrain background.

摘要: 渤海湾盆地南堡凹陷古近系沙河街组的古水体特征研究程度较低。以南堡凹陷南部为例,采用多种方法,分析了沙河街组一段沉积时期水体的古盐度和古水深。根据Sr/Ba值、Rb/K值和特殊藻类化石,认为其古盐度为微咸—半咸。通过Sr/Cu值和孢粉化石2种手段,恢复了研究区沙河街组一段沉积时期的古气候,认为其为潮湿气候但存在干湿波动。根据Mn/Fe值变化、干酪根类型和藻类化石以及似瘤田螺的发现,恢复了该时期的相对古水深,并结合自生黏土矿物、沉积构造和沉积相等,通过加权平均值的方法定量计算古水深,得出研究区沙一段中亚段顶部沉积时期水体较浅,为4~15,m,而沙一段下亚段沉积时期水体较深,为4~30,m。综合分析认为,南堡凹陷南部沙河街组一段沉积时期的古盐度和古水深在一定程度上取决于古气候条件和古地形背景。

关键词: 古盐度, 古气候, 古水深, 古近系, 渤海湾盆地

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