[an error occurred while processing this directive] 世界地质 2019, 38(4) 988-998 DOI:   10.3969/j.issn.1004-5589.2019.04.010  ISSN: 1004-5589 CN: 22-1111/P

本期目录 | 下期目录 | 过刊浏览 | 高级检索                                                            [打印本页]   [关闭]
基础地质
扩展功能
本文信息
Supporting info
PDF(3880KB)
[HTML全文]
参考文献[PDF]
参考文献
服务与反馈
把本文推荐给朋友
加入我的书架
加入引用管理器
引用本文
Email Alert
文章反馈
浏览反馈信息
本文关键词相关文章
松辽盆地
四方台组
地球化学
古气候
沉积环境
本文作者相关文章
申林
刘招君
胡菲
李建国
赵丁名
万涛
PubMed
Article by Shen L
Article by Liu Z
Article by Hu F
Article by Li J
Article by Zhao D
Article by Wan T
松辽盆地大庆长垣南端上白垩统四方台组古环境特征及演化
申林1,2, 刘招君1,2, 胡菲1,2, 李建国3, 赵丁名1,2, 万涛1,2
1. 吉林大学 地球科学学院, 长春 130061;
2. 吉林省油页岩与共生能源矿产重点实验室, 长春 130061;
3. 中国地质调查局 天津地质调查中心, 天津 300170
摘要: 通过对岩芯的观察和测井资料的研究将松辽盆地北部四方台组划分为2个三级层序,8个四级层序,并识别出辫状河和曲流河2种沉积相和8种沉积微相。层序1(SQ1)低水位体系域时期为辫状河相,发育辫状河河床和泛滥平原(河漫滩)两种亚相;水进体系域时期发育曲流河河床和泛滥平原(河漫滩和河漫湖泊)亚相;高水位体系域时期和水退体系域时期发育曲流河河床和泛滥平原(河漫滩、河漫湖泊和决口扇)亚相。结合泥岩样品的地球化学特征即样品的Sr/Cu、Th/U、Rb/Sr和SiO2/Al2O3比值的变化趋势可知SQ1时期气候干热,SQ2时期干旱程度减弱。根据δCe、V/Cr、V/(V+Ni)、Ni/Co和U/Th的变化趋势可知四方台组时期古水体处于氧化还原过渡-氧化环境,SQ1时期水体氧化性更强。古气候、古水体氧化还原性和沉积相之间具有较好的耦合关系:气候干热时,蒸发作用加剧,水体变浅,水体氧化性增强,发育大量河床亚相沉积;气候干旱程度降低时,蒸发作用减缓,水体变深,水体氧化性减弱,以泛滥平原亚相为主。
关键词 松辽盆地   四方台组   地球化学   古气候   沉积环境  
Paleoenvironment characteristics and evolution of Upper Cretaceous Sifangtai Formation in southern end of Daqing placanticline of Songliao Basin
SHEN Lin1,2, LIU Zhao-jun1,2, HU Fei1,2, LI Jian-guo3, ZHAO Ding-ming1,2, WAN Tao1,2
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Key Laboratory of Oil Shale and Coexistent Energy Minerals of Jilin Province, Changchun 130061, China;
3. Tianjin Center of China Geology Survey, Tianjin 300170, China
Abstract: Based on the observation and analysis of core and well log data, the Sifangtai Formation in the northern part of Songliiao Basin is divided into two third-order sequences and eight fourth-order sequences, with two sedimentary facies and eight sedimentary microfacies identified. The Sequence 1 (SQ1) is braided fluvial facies, developing river bed and flood plain sub-facies in the lowstand systems tract period. Meandering river bed and flood plain (overbank and river flood lake) sub-facies occur during the transgressive systems tract period. Meander-ing river bed and flood plain (overbank, river flood lake and crevasse fan) occur during the highstand systems tract period and the regressive systems tract period. According to the geochemical analysis of mudstone samples, i. e., the variation trend of Sr/Cu, Th/U, Rb/Sr and SiO2/Al2O3, it is indicated that the climate was hot and dry during the SQ1 period, and was weakened during the SQ2 period. The variation trend of δCe, V/Cr, V/(V + Ni), Ni/Co and U/Th show that the palaeo-water body during the Sifangtai Formation period was in the redox transition-oxi-dation environment, and was more oxidized during the SQ1 period. It shows a good coupling relationship between the paleoclimate, the paleowater's oxidation-reduction and sedimentary facies. When the climate is hot and dry, the evaporation intensifies, the water body becomes shallower and the water body is enhanced in oxidation, resulting in the development of a large number of river bed deposits. When the drought decreases, the evaporation slows down, the water body becomes deeper, and the oxidation becomes weaker, so as to be dominated by flood plain sub-faci-es.
Keywords: Songliao Basin   Sifangtai Formation   geochemistry   paleoclimate   sedimentary environment  
收稿日期 2019-05-24 修回日期 2019-07-06 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2019.04.010
基金项目:

中国地质调查局天津地质调查中心地质调查项目(DD2017128-08(9))

通讯作者: 刘招君(1951),男,教授,博士生导师,主要从事沉积学、层序地层学、石油地质学及油页岩成矿理论研究。E-mail:liuzj@jlu.edu.cn
作者简介:
作者Email: liuzj@jlu.edu.cn

参考文献:
[1] 高远. 晚白垩世松辽盆地古气候演化:博士学位论文[D]. 北京:中国地质大学, 2015. GAO Yuan. Paleoclimatic evolution of the Songliao Basin in the Late Cretaceous:doctor's degree thesis[D]. Bei-jing:China University of Geosciences, 2015.
[2] 杨雷. 松辽盆地晚白垩世古气候变化的测井反演研究:博士学位论文[D]. 北京:中国地质大学, 2018. YANG Lei. Well logging inversion on the paleoclimate change of Late Cretaceous in Songliao Basin:doctor's de-gree thesis[D]. Beijing:China University of Geosci-ences, 2018.
[3] 刘招君, 王东坡, 刘立, 等. 松辽盆地白垩纪沉积特征[J]. 地质学报, 1992(4):327-338. LIU Zhao-jun, WANG Dong-po, LIU Li, et al. Sedi-mentary characteristics of Cretaceous in Songliao Basin[J]. Acta Geological Sinica, 1992(4):327-338.
[4] 吴春阳. 松科1井嫩江组化学地层划分及古气候分析:博士学位论文[D]. 北京:中国地质大学, 2018. WU Chun-yang. Chemical stratigraphic division and pa-leoclimatic analysis of Nenjiang Formation in Songke 1 Well:doctor's degree thesis[D]. Beijing:China Uni-versity of Geosciences, 2018.
[5] 陈路路, 汤超, 李建国, 等. 松辽盆地大庆长垣南端四方台组含铀砂岩岩石学特征及地质意义[J]. 地质调查与究, 2018, 41(1):33-39, 66. CHEN Lu-lu, TANG Chao, LI Jian-guo, et al. Petrolo-gy characteristics of the uranium-bearing layer of Sifantai Formation in Daqing placanticline of Songliao Basin and their geological implications[J]. Geological Survey and Research, 2018, 41(1):33-39, 66.
[6] 肖鹏, 汤超, 魏佳林, 等. 大庆长垣南端四方台组沉积相特征及其与铀富集的关系[J]. 地质调查与研究, 2018, 41(1):18-23. XIAO Peng, TANG Chao, WEI Jia-lin, et al. Sedimen-tary facies of the Sifangtai Formation in the southern Daqing placanticline and its controls to uranium minerali-zation[J]. Geological Survey and Research, 2018, 41(1):18-23.
[7] 刘华健, 金若时, 李建国, 等. 松辽盆地北部含铀岩系沉积物源及铀源分析研究进展[J]. 地质调查与研究, 2017, 40(4):281-289. LIU Hua-jian, JIN Ruo-shi, LI Jian-guo, et al. Ad-vance in research for sedimentary and uranium source a-nalysis of the uranium-bearing series in northern Songliao Basin[J]. Geological Survey and Research, 2017, 40(4):281-289.
[8] 徐增连, 汤超, 李建国, 等. 松辽盆地北部三肇凹陷四方台组层序地层及其与砂岩型铀矿化的关系[J]. 地质调查与研究, 2018, 41(1):24-32. XU Zeng-lian, TANG Chao, LI Jian-guo, et al. Se-quence stratigraphy of the Sifangtai Formation and its rela-tionship with uranium mineralization in the Sanzhao de-pression, northern Songliao Basin[J]. Geological Sur-vey and Research, 2018, 41(1):24-32.
[9] 万涛, 刘招君, 胡菲, 等. 松辽盆地北部上白垩统四方台组河流相层序沉积特征[J]. 大庆石油地质与开发, 2018, 37(5):1-7. WAN Tao, LIU Zhao-jun, HU Fei, et al. Sedimentary characteristics of the fluvial sequence of Upper Cretaceous Sifangtai Formation in North Songliao Basin[J]. Petro-leum Geology & Oilfield Development in Daqing, 2018, 37(5):1-7.
[10] 钟延秋, 马文娟. 松辽盆地北部中、新生代构造运动特征及对砂岩型铀矿的控制作用[J]. 地质找矿论丛, 2011, 26(4):411-416. ZHONG Yan-qiu, MA Wen-juan. Mesozoic, Cenozoic tectonic movements and the control on sandstone-hosted uranium deposit in North Songliao Basin[J]. Contribu-tions to Geology and Mineral Resources Research, 2011, 26(4):411-416.
[11] 赵忠华, 白景萍, 赖天功. 松辽盆地北部反转构造与砂岩型铀矿成矿作用[J]. 铀矿地质, 2018, 34(5):274-279. ZHAO Zhong-hua, BAI Jing-ping, LAI Tian-gong. Re-versal structure and its relation to metallization of sand-stone type uranium deposit in northern Songliao Basin[J]. Uranium Geology, 2018, 34(5):274-279.
[12] 宋朔, 刘招君, 孙平昌, 等. 红色泥岩层系地球化学特征及物源分析:以松辽盆地东南隆起区上白垩统姚家组为例[J]. 世界地质, 2015, 34(3):774-785. SONG Shuo, LIU Zhao-jun, SUN Ping-chang, et al. Geochemical characteristics and sediment provenance a-nalysis of red mudstone formation:a case study of Upper Cretaceous Yaojia Formation of southeastern uplift area in Songliao Basin[J]. Global Geology, 2015, 34(3):774-785.
[13] 肖鹏, 金若时, 汤超, 等. 松辽盆地北部大庆长垣南端上白垩统四方台组物源体系分析[J]. 石油实验地质, 2018, 40(4):493-501. XIAO Peng, JIN Ruo-shi, TANG Chao, et al. Prove-nance system of the Late Cretaceous Sifangtai Formation in the south of Daqing placanticline of the northern Songliao Basin[J]. Petroleum Geology & Experiment, 2018, 40(4):493-501.
[14] 王国栋, 程日辉, 王璞臖, 等. 松辽盆地松科1井上白垩统四方台组沉积序列厘米级精细刻画:岩性·岩相·旋回[J]. 地学前缘, 2011, 18(6):263-284. WANG Guo-dong, CHENG Ri-hui, WANG Pu-jun, et al. Centimeter-scale sedimentary sequence description of Upper Cretaceous Sifangtai Formation:lithostratigra-phy, facies and cyclostratigraphy, based on the scien-tific drilling (SKI) borehole in the Songliao Basin[J]. Earth Science Frontiers, 2011, 18(6):263-284.
[15] 张雷, 王英民, 李树青, 等. 松辽盆地北部四方台组-明水组高精度层序地层特征与有利区带预测[J]. 中南大学学报(自然科学版), 2009, 40(6):1679-1688. ZHANG Lei, WANG Ying-min, LI Shu-qing, et al. High-resolution sequence stratigraphic characteristic and favorable hydrocarbon accumulation prediction of Sifang-tai to Mingshui Formation in the north of Songliao Basin[J]. Journal of Central South University (Science and Technology Edition), 2009, 40(6):1679-1688.
[16] 刘招君, 董清水, 王嗣敏, 等. 陆相层序地层学导论与应用[M]. 北京:石油工业出版社, 2002:126-130. LIU Zhao-jun, DONG Qing-shui, WANG Si-min, et al. Introduction and application of terrestrial sequence stratigraphy[M]. Beijing:Petroleum Industry Press, 2002:126-130.
[17] 王益友, 郭文莹, 张国栋. 几种地球化学标志在金湖凹陷阜宁群沉积环境中的应用[J]. 同济大学学报, 1979(2):51-60. WANG Yi-you, GUO Wen-ying, ZHANG Guo-dong. Application of several geochemical markers in sedimen-tary environment of Funing Group in Jinhu sag[J]. Journal of Tongji University, 1979(2):51-60.
[18] Nesbitt H W, Young G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites[J]. Nature, 1982, 299(5885):715-717.
[19] 徐小涛, 邵龙义. 利用泥质岩化学蚀变指数分析物源区风化程度时的限制因素[J]. 古地理学报, 2018, 20(3):515-522. XU Xiao-tao, SHAO Long-yi. Limiting factors in utili-zation of chemical index of alteration of mudstones to quantify the degree of weathering in provenance[J]. Journal of Palaeogeography, 2018, 20(3):515-522.
[20] 张威, 穆克华, 崔之久, 等. 云南拱王山地区全新世以来的环境变化记录[J]. 地球与环境, 2007(4):343-350. ZHANG Wei, MU Ke-hua, CUI Zhi-jiu, et al. Record of the environmental change since Holocene in the region of Gongwang mountain, Yunnan Province[J]. Earth and Environment, 2007, 35(4):343-350.
[21] Nickel E. Lakes chemistry, geology, physics[J]. Engineering Geology, 1981, 17(1/2):72-74.
[22] 贾建亮. 基于地球化学-地球物理的松辽盆地上白垩统油页岩识别与资源评价:博士学位论文[D]. 长春:吉林大学, 2012. JIA Jian-liang. Research on the recognition and resource evaluation of the Upper Cretaceous oil shale based on ge-ochemistry-geophysics technique in the Songliao Basin (NE, China):doctor's degree thesis[D]. Changchun:Jilin University, 2012.
[23] 马奂奂, 刘池洋, 张龙, 等. 鄂尔多斯盆地延长组长7段沉积岩元素地球化学特征及沉积环境分析[J]. 现代地质, 2019, 33(4):872-882. MA Huan-huan, LIU Chi-yang, ZHANG Long, et al. Geochemical characteristics and depositional environ-ment implications of sedimentary rocks in the Chang 7 member of Yanchang Formation in the Ordos Basin[J]. Geoscience, 2019, 33(4):872-882.
[24] 焦养泉, 吴立群, 杨生科, 等. 铀储层沉积学:砂岩型铀矿勘查与开发的基础[M]. 北京:地质出版社, 2006:98-105. JIAO Yang-quan, WU Li-qun, YANG Sheng-ke, et al. Uranium reservoir sedimentology:the basis for ex-ploration and development of sandstone-type uranium de-posits[M]. Beijing:Geological Publishing House, 2006:98-105.
[25] Eldcrficld H, Greaves M J. The rare earth elements in seawater[J]. Nature, 1982, 296(5854):214-219.
[26] 彭治超, 李亚男, 张孙玄琦, 等. 主微量元素地球化学特征在沉积环境中的应用[J]. 西安文理学院学报(自然科学版), 2018, 21(3):108-111. PENG Zhi-chao, LI Ya-nan, ZHANGSUN Xuan-qi, et al. Application of the geochemical characteristics of the major and trace elements in the sedimentary environment[J]. Journal of Xi'an University (Natural Science Edi-tion), 2018, 21(3):108-111.
本刊中的类似文章
1.李晓鹏, 孙景贵, 刘阳, 王清海, 任泽宁, 谷小丽.延边闹枝铜金矿区中生代火山岩锆石U-Pb年代学、地球化学及其地质意义[J]. 世界地质, 2020,39(3): 528-543
2.廖宇斌, 李碧乐, 孙永刚, 杨佰慧, 高歌悦, 刘国文.柴达木盆地北缘锡铁山铅锌矿区辉长岩锆石U-Pb年代、岩石地球化学和Hf同位素特征[J]. 世界地质, 2020,39(3): 495-508
3.何泽宇, 申俊峰, 王来明, 李国武, 刘汉栋, 张华锋, 杜佰松, 吴晋超.胶东宋家沟金矿中基性脉岩锆石U-Pb年代学、地球化学及其地质意义[J]. 世界地质, 2020,39(3): 509-527
4.贾雨东, 王德海, 王新宇, 巴燕·夏木提汗, 郭忆茹.天津蓟州雾迷山组与洪水庄组沉积环境与地球化学特征[J]. 世界地质, 2020,39(3): 569-577
5.侯艳平, 任延广, 孙丽, 张海军, 吴海波, 彭威, 李敬生.海拉尔盆地东明凹陷明D2井白垩系沉积特征及沉积环境分析[J]. 世界地质, 2020,39(2): 332-343
6.陈海潮, 王璞珺, 衣健, 武成智, 王寒非, 孙松, 王文华.长白山火山碎屑喷出物和熔岩地球化学特征及其对构造环境的指示意义[J]. 世界地质, 2020,39(2): 294-305
7.王新宇, 王德海, 王思琳, 王金娜, 刘奇, 贾雨东.松辽盆地南部永平油田泉四段油气成藏条件分析[J]. 世界地质, 2020,39(2): 388-397
8.王剑平, 王会胜, 唐秀念, 李绪俊.福建政和地区熊山岩体锆石U-Pb定年、地球化学特征及其成矿意义[J]. 世界地质, 2020,39(2): 250-260
9.王颖, 徐仲元, 董晓杰, 王师捷, 石强.内蒙古得耳布尔地区中生代中-晚期火山岩的年代学、地球化学特征及其地质意义[J]. 世界地质, 2020,39(2): 261-281
10.陈木森, 董永胜, 王鹏森, 王成志.辽东黄花甸地区古元古代变辉绿岩的特征及成因[J]. 世界地质, 2020,39(2): 306-321
11.冷庆磊, 黄玉龙, 冉波, 张甲明, 王璞珺.火山碎屑岩储层溶蚀孔隙发育特征与控制因素:以松辽盆地南部陆家堡凹陷下白垩统为例[J]. 世界地质, 2020,39(2): 368-378
12.周佳和, 徐聪.“两宽一高”地震勘探技术在复杂油气勘探中的应用[J]. 世界地质, 2020,39(2): 422-428
13.孙永刚, 李碧乐, 王聚胜, 王永胜, 张旭, 詹天宇.吉林中部江密峰花岗闪长岩锆石U-Pb年代学和岩石地球化学特征[J]. 世界地质, 2019,38(4): 931-943
14.万传彪, 孙跃武, 薛云飞, 金玉东, 张昕, 李倜.松辽盆地杜101井晚古生代地层划分与对比[J]. 世界地质, 2019,38(4): 889-899
15.贾海明, 景妍, 王清海, 兰丽雪, 井佳浩.大兴安岭中段罕达盖地区早白垩世花岗岩的成因及其地质意义[J]. 世界地质, 2019,38(4): 921-930

Copyright by 世界地质