银额盆地查干断陷闭流湖盆层序的控制因素与形成机理

郭彦如

银额盆地查干断陷闭流湖盆层序的控制因素与形成机理

郭彦如

中国石油勘探开发研究院北京 100083

详细信息

作者简介:
郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学

中图分类号: P539.2

计量

文章访问数: 457
HTML全文浏览量: 1
PDF下载量: 445
被引次数: 0

Controls and Formation Mechanism of the Sequences in the Chagan Fault-Depressed Stagnant Lacustrine Depression, Yin-E Basin

GUO Yan-ru

Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083

摘要

摘要: 陆相层序的控制因素与形成机制是陆相层序地层学研究的一项重要内容。断陷闭流湖盆作为一种独特的类型有其自身的特点。对查干凹陷早白垩世断陷闭流湖盆的沉积演化和基准面相对变化曲线的研究表明查干凹陷断陷闭流湖盆层序的控制因素以构造控制因素与气候因素占主导地位,其次是沉积物供应速率和湖平面的变化;在造控制因素与气候因素的双重控制下形成两类层序,一类是断陷气候复合型层序,另一类为气候型层序。
- 查干凹陷 /
- 断陷闭流湖盆 /
- 层序地层学 /
- 控制因素 /
- 形成机制
Abstract: The controlling factors and formation mechanism of the continental sequences are important research field in continental sequence stratigraphy. A fault-depressed stagnant lacustrine basin as a unique basin has its own particular characteristics. In this paper, the author has studied the sedimentary evolution and the base-level changes of the Early Cretaceous fault-depressed stagnant lacustrine basin in Chagan Depression, and then considered that the controlling factors of the sequence in the fault-depressed stagnant lacustrine basin are dominantly the integration of tectonic and climatic factors, and, in the next place, the supply rate of the sediments and lake-level change. Under the control of the double factors, two types of sequences were formed: one was the compound type of fault-depression and climate, and another was climatic type.
- Chagan Depression /
- fault-depressed stagnant /
- lacustrine basin /
- sequence stratigraphy /
- control factor

HTML全文

参考文献(17)

[1]	徐怀大.从地震地层学到层序地层学--油气盆地的定性化与定量化描述. 北京:石油工业出版社,1997[Xu Huaida. From seismic stratigraphy to sequence stratigraphy: a qualitative and quantitative description about petroleum oil and gas-bearing basins. Beijing: Petroleum Industry Press,1997]
[2]	徐怀大.陆相层序地层学研究中的某些问题. 石油与天然气地质,1997,18(2):83～89[Xu Huaida. Some issues on the study of continental sequence stratigraphy. Oil & Gas Geology, 1997,18(2):83～89]
[3]	魏魁生.二连盆地白垩系非海相沉积层序地层特征. 地球科学,1994,19[Wei Kuisheng. Characteristics of the Cretaceous non-marine sequence stratigraphy in Erlian Basin. Earth Science, 1994,19]
[4]	魏魁生, 徐怀大,雷怀玉, 等.非海相层序地层学--以松辽盆地为例.北京:地质出版社,1996[Wei Kuisheng, Xu Huaida, Lei Huaiyu, et al. Non-marine sequence stratigraphy: a case study in Songliao Basin. Beijing: Geological Publishing House, 1996]
[5]	樊太亮,李庆谋.沉积基准面变化分析技术及应用. 石油与天然气地质,1997,18(2):108～113[Fan Tailiang, Li Qingmu. Analytical technique and application of deposited base-level change. Oil & Gas Geology, 1997,18(2):108～113]
[6]	纪友亮,张世奇,等. 陆相断陷湖盆层序地层学. 北京: 石油工业出版社,1996[Ji Youliang, Zhang Shiqi, et al.Sequence stratigraphy of continental fault-depressed lacustrine basin. Beijing: Petroleum Industry Press, 1996]
[7]	张荣红,余素玉,邬金华. 陆相湖盆中沉积物供给因素对层序地层分析的影响-以东营凹陷下第三系为例. 地球科学,1997,22(2):139～144 [Zhang Ronghong, Yu Suyu, Wu Jinhua. Influence for sequence stratigraphic analysis of sedimentary supply factors of in continental lacustrine basins: a case of the Lower Tertiary in Dongying Depression. Earth Science, 1997,22(2):139～144]
[8]	冯有良,李思田,解习农. 陆相断陷盆地层序形成动力学及层序地层模式. 地学前缘,2000,7(3):119～132 [Feng Youliang, Li Sitian, Xie Xilong. Forming dynamics of sequences and sequence stratigraphic models in the continental fault-depressed basins. Earth Science Frontier,2000,7(3):119～132]
[9]	胡受权,郭文平,颜其彬,等. 试论控制断陷湖盆陆相层序发育的影响因素. 沉积学报,2001,19(2):256～162 [Hu Shouquan, Guo Wenping, Yan Qibing, et al. Control factors of continental sequence growth in fault-depressed basin. Acta Sedimentologica Sinica, 2001,19(2):256～162]
[10]	郑荣才,彭军,吴朝容. 陆相盆地基准面旋回的级次划分和研究意义.沉积学报,2001,19(2):249～254[Zheng Rongcai, Pen Jun, Wu Chaorong. Classification and research significace of base-level cycles in the continental basin. Acta Sedimentologica Sinica, 2001,19(2):249～254]
[11]	Galloway W E. Genetic stratigraphic sequences in basin analysis: architecture and genesis of flooding surface bounded depositional units. AAPG Bulletin, 1989,73:125～142
[12]	Hunt D, Tucker M E. Stranded parasequences and the forced regressive wedge systems tract: deposition during base-level fall-reply. Sedimentary Geology,1995,95:147～160
[13]	Posamentier H W, Jervey M T, Vail P R. Eustatic controls on clastic deposition Ⅱ--sequence and systems tract models. In: Wilgus C K, et al. eds. Sea-level changes-an integrated approach. SEPM Special Publication, 1988,42:125～154
[14]	Posamentier H W, Allen G P, et al. Forced regressions in a sequence stratigraphic framework: concepts, examples, and exploration significance. AAPG Bulletin,1992, 76:1687～1709
[15]	Vail P R, Mitchum R M. Seismic stratigraphy and global changes in sea level from coastal onlap. In: Payton C E, ed. Seismic Stratigraphy-Application to Hydrocarbon Exploration. AAPG, Memoir, 1977, 26:51～212
[16]	郭彦如,于均民,樊太亮.查干凹陷下白垩统层序地层格架与沉积演化.石油与天然气地质,2002,23(2):166～169[Guo Yanru, Yu Junmin, Fan Tailiang. Sequence stratigraphic framework and sedimentary evolution of the Lower Cretaceous in the Chagan Depression.Oil & Gas Geology, 2002,23(2):166～169]
[17]	郭彦如,李天顺,商平.内蒙古银额盆地火山特征与识别. 地球学报,1999,20(增刊):97～102[Guo Yanru, Li Tianshun, Shang Ping. Characteristics and identification of volcanic rocks in Yin-E Basin, Mongolia. Acta Geoscientia Sinica,1999,20(Suppl.):97～102]

[1]	赵鑫, 卢政环, 廖飞燕, 时阳, 郭浩, 肖露, 赖锦, 李美俊, 龚承林. 福山凹陷流沙港组储层品质控制因素与优质储层预测 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.085
[2]	吴高奎, 张忠民, 陈华, 郭荣涛, 孔凡军, 宫越, 徐海, 张德民. 下刚果盆地中新统重力流沉积演化及控制因素 . 沉积学报, 2023, 41(1): 73-84. doi: 10.14027/j.issn.1000-0550.2022.032
[3]	操应长, 燕苗苗, 葸克来, 吴松涛, 朱宁, 朱如凯. 玛湖凹陷夏子街地区三叠系百口泉组砂砾岩储层特征及控制因素 . 沉积学报, 2019, 37(5): 945-956. doi: 10.14027/j.issn.1000-0550.2019.002
[4]	刘杰, 苏明, 乔少华, 沙志彬, 吴能友, 杨睿. 珠江口盆地白云凹陷陆坡限制型海底峡谷群成因机制探讨 . 沉积学报, 2016, 34(5): 940-950. doi: 10.14027/j.cnki.cjxb.2016.05.013
[5]	张金友. 陆相坳陷盆地烃源岩内致密砂岩储层含油性主控因素——以松辽盆地北部中央坳陷区齐家凹陷高台子油层为例 . 沉积学报, 2016, 34(5): 991-1002. doi: 10.14027/j.cnki.cjxb.2016.05.018
[6]	王朋, 柳广弟, 曹喆, 苏惠, 牛子铖, 张婧雅, 罗文斌. 查干凹陷下白垩统稠油地球化学特征及成因分析 . 沉积学报, 2015, 33(6): 1265-1274. doi: 10.14027/j.cnki.cjxb.2015.06.019
[7]	. 深水湖盆沉积砂体的层序地层分析——以四川侏罗系为例 . 沉积学报, 2013, 31(05): 798-806.
[8]	操应长. 东营凹陷西部沙四上亚段滩坝砂体有效储层的物性下限及控制因素 . 沉积学报, 2009, 27(2): 230-237.
[9]	杨俊生. 苏丹Muglad盆地Fula坳陷白垩系Abu Gabra组层序地层及沉积体系 . 沉积学报, 2008, 26(6): 994-1004.
[10]	严德天王华王家豪王清晨. 库车前陆盆地白垩系层序地层样式及控制因素分析 . 沉积学报, 2006, 24(06): 841-848.
[11]	张小莉. 惠民凹陷临邑洼陷岩性油藏控制因素分析 . 沉积学报, 2006, 24(2): 289-293.
[12]	明海会, 金振奎, 金之钧, 杨明慧, 陈祥. 泌阳凹陷安棚油田深层系油气分布规律及控制因素 . 沉积学报, 2005, 23(2): 329-336.
[13]	杨占龙, 郭精义, 陈启林, 宋广寿, 黄刚. 银根盆地查干凹陷火山沉积岩岩相特征及其识别标志 . 沉积学报, 2005, 23(1): 67-72.
[14]	朱筱敏, 康安, 王贵文. 陆相坳陷型和断陷型湖盆层序地层样式探讨 . 沉积学报, 2003, 21(2): 283-287.
[15]	杨剑萍, 许正豪, 姜在兴, 操应长, 陈发亮. 山东惠民凹陷中央隆起带古近系沙河街组层序地层特征及控制因素研究 . 沉积学报, 2003, 21(4): 670-674.
[16]	岳伏生, 马龙, 李天顺. 查干凹陷下白垩统碎屑岩储层成岩演化与油气成藏 . 沉积学报, 2002, 20(4): 644-649.
[17]	金振奎, 邹元荣, 蒋春雷, 由伟丰. 大港探区奥陶系岩溶储层发育分布控制因素 . 沉积学报, 2001, 19(4): 530-535.
[18]	林春明, 钱奕中. 浙江沿海平原全新统气源岩特征及生物气形成的控制因素 . 沉积学报, 1997, 15(S1): 70-75.
[19]	王维纲, 吕炳全. 小尺度的碳酸盐岩层序地层学分析——塔里木盆地桑塔木断垒带奥陶系层序地层学研究 . 沉积学报, 1997, 15(4): 24-29.
[20]	吴元燕, 刘震, 王伟华, 费安玮, 刘洛夫. 歧北凹陷沙河街组层序地层学研究 . 沉积学报, 1996, 14(1): 167-175.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 457
HTML全文浏览量: 1
PDF下载量: 445
被引次数: 0

姓名
邮箱
手机号码
标题
留言内容
验证码

留言板

银额盆地查干断陷闭流湖盆层序的控制因素与形成机理

作者简介:
郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学

计量

Controls and Formation Mechanism of the Sequences in the Chagan Fault-Depressed Stagnant Lacustrine Depression, Yin-E Basin

计量

目录

银额盆地查干断陷闭流湖盆层序的控制因素与形成机理

中国石油勘探开发研究院北京 100083

作者简介:
郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学

English Abstract

Controls and Formation Mechanism of the Sequences in the Chagan Fault-Depressed Stagnant Lacustrine Depression, Yin-E Basin

Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

银额盆地查干断陷闭流湖盆层序的控制因素与形成机理

作者简介: 郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学

计量

出版历程

Controls and Formation Mechanism of the Sequences in the Chagan Fault-Depressed Stagnant Lacustrine Depression, Yin-E Basin

计量

出版历程

目录

银额盆地查干断陷闭流湖盆层序的控制因素与形成机理

中国石油勘探开发研究院 北京 100083

作者简介: 郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学

English Abstract

Controls and Formation Mechanism of the Sequences in the Chagan Fault-Depressed Stagnant Lacustrine Depression, Yin-E Basin

Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学

中国石油勘探开发研究院北京 100083

作者简介:
郭彦如,男 1962年出生,高级地质师,工学博士,石油地质及层序地层学