[an error occurred while processing this directive] 世界地质 2019, 38(4) 889-899 DOI:   10.3969/j.issn.1004-5589.2019.04.001  ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
松辽盆地
杜101井
二叠系
哲斯组
腕足化石
一心组
杜尔伯特板岩
本文作者相关文章
万传彪
孙跃武
薛云飞
金玉东
张昕
李倜
PubMed
Article by Wan C
Article by Sun Y
Article by Xue Y
Article by Jin Y
Article by Zhang X
Article by Li T
松辽盆地杜101井晚古生代地层划分与对比
万传彪1,2,3, 孙跃武2, 薛云飞1,3, 金玉东1,3, 张昕1,3, 李倜1,3
1. 大庆油田有限责任公司 勘探开发研究院, 黑龙江 大庆 163712;
2. 东北亚生物演化与环境教育部重点实验室(吉林大学), 长春 130026;
3. 中国石油集团碳酸盐岩储层重点实验室 大庆油田研究分室, 黑龙江 大庆 163712
摘要: 前人将杜101井1 662.2~2 200.0 m井段自下而上划分为"杜尔伯特组"和"一心组",但两组之间的自然电位(SP)、自然伽马(GR)、深感应电阻率(RILD)和中感应电阻率(RILM)曲线没有出现明显突变,应合并为一组,依据岩性自下而上可划分为3段:下段(砂砾岩段)、中段(砂砾岩-泥灰岩段)和上段(泥灰岩-粉砂岩段)。其中,上段产双壳类化石Casmogoriophora sp.、Parallelodon cf.tenuistriatusParallelodon sp.,腕足类化石Spirif erella persaranaenaSpirif erella sp.、Lamnimargus peregrinaStenoscisma cf.zhesiensisAthyis sp.等,地质时代为中二叠世。该井段岩性和古生物特征,可与松辽盆地西缘乌兰浩特-孙吴地区的哲斯组对比,因此,将松辽盆地西缘的哲斯组引入盆地内,作为松辽盆地井下哲斯组的次层型剖面。
关键词 松辽盆地   杜101井   二叠系   哲斯组   腕足化石   一心组   杜尔伯特板岩  
Late Paleozoic stratigraphic division and correlation in Well Du 101 in Songliao Basin
WAN Chuan-biao1,2,3, SUN Yue-wu2, XUE Yun-fei1,3, JIN Yu-dong1,3, ZHANG Xin1,3, LI Ti1,3
1. Institute of Exploration and Development, Daqing Oilfield Company Ltd., Daqing 163712, Heilongjiang, China;
2. Key Laboratory for Evolution of Past Life and Environment in Northeast Asia(Jilin University), Ministry of Education, Changchun 130026, China;
3. Key Laboratory of Carbonate Reservoir, CNPC, Daqing 163712, Heilongjiang, China
Abstract: The strata in the depth of 1 662.2~2 200.0 m in Well Du 101 were divided and named as Duerbert and Yixin formations in ascending order. However, there is no sharp change between the two units on well logs, such as the spontaneous potential (SP), gamma ray (GR), deep and medium induction resistivity (RILD, RILM). Thus, they should be combined into one formation. Based on the lithology, three members can be identi-fied from bottom to top, i.e. the lower glutenite member, the middle glutenite-marlstone member, and the upper marlstone-siltstone member. Abundant marine fossils have been discovered in the upper member, including bivalves (Casmogoriophora sp., Parallelodon cf. tenuistriatus, Parallelodon sp.) and brachiopods (Spiriferella per-saranaena, Spiriferella sp., Lamnimargus peregrina, Stenoscisma cf. zhesiensis, Athyis sp.), which indicates Mid-dle Permian age. Since the lithology and fossils in Well Du 101 can be correlated to those of Zhesi Formation out-cropped in the Ulanhot-Sunwu area on the western margin of Songliao Basin, the Zhesi Formation is used in Songli-ao Basin, and the strata in Well Du 101 (depth 1 662.2~2 200.0 m) is suggested as a para-stratotype of the Zhesi Formation in the basin.
Keywords: Songliao Basin   Well Du 101   Permian   Zhesi Formation   brachiopods   Yixin Formation   Duer-bert slate  
收稿日期 2019-10-17 修回日期 2019-11-19 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2019.04.001
基金项目:

国家自然科学基金项目(31670215)

通讯作者: 孙跃武(1966),教授,从事古生物学与地层学研究。E-mail:sunyuewu@jlu.edu.cn
作者简介:
作者Email: sunyuewu@jlu.edu.cn

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