松辽盆地北部湖盆萎缩期层序结构与沉积充填

韩建辉

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松辽盆地北部湖盆萎缩期层序结构与沉积充填

韩建辉

文章导航 > 沉积学报 > 2009 > 27(3): 479-486

韩建辉. 松辽盆地北部湖盆萎缩期层序结构与沉积充填[J]. 沉积学报, 2009, 27(3): 479-486.

引用本文:

韩建辉. 松辽盆地北部湖盆萎缩期层序结构与沉积充填[J]. 沉积学报, 2009, 27(3): 479-486.

HAN JianHui. Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗[J]. Acta Sedimentologica Sinica, 2009, 27(3): 479-486.

Citation:

HAN JianHui. Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗[J]. Acta Sedimentologica Sinica, 2009, 27(3): 479-486.

韩建辉. 松辽盆地北部湖盆萎缩期层序结构与沉积充填[J]. 沉积学报, 2009, 27(3): 479-486.

引用本文:

韩建辉. 松辽盆地北部湖盆萎缩期层序结构与沉积充填[J]. 沉积学报, 2009, 27(3): 479-486.

HAN JianHui. Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗[J]. Acta Sedimentologica Sinica, 2009, 27(3): 479-486.

Citation:

HAN JianHui. Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗[J]. Acta Sedimentologica Sinica, 2009, 27(3): 479-486.

松辽盆地北部湖盆萎缩期层序结构与沉积充填

韩建辉

中国石油大学资源与信息学院北京 102249

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通讯作者:
韩建辉

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文章访问数: 2017
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Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗

HAN JianHui

School of Resource and Information Technology in China University of Petroleum, Beijing 102249

More Information

Corresponding author: HAN JianHui

摘要

摘要: 萎缩期是陆相湖盆演化的重要阶段，但和断陷期、坳陷期相比，对湖泊萎缩期的沉积充填和层序构成的认识非常不足，研究也非常薄弱。松辽盆地的四方台期和明水期是典型的湖盆萎缩期，对其沉积充填和层序构成的研究有助于加深学术界和工业界对这一重要阶段的认识和促进油气勘探。将四方台组、明水组划分为一个超层序，六个三级层序。对比分析了松辽盆地坳陷期与萎缩期地质特征，认为盆地萎缩期为地形平缓的浅水盆地，具有构造幅度低、可容空间小、湖平面升降频繁等特点。层序界面多表现为低角度不整合、低幅上超面以及沉积转换面等；沉积上，该段主要发育河流相、浅水湖泊、浅水三角洲等沉积相。层序结构上，由于没有明显坡折带，故采用两分法划分体系域，包括湖侵体系域(TST)和湖退体系域(RST)；盆地边缘没有明显的的下切谷特征，砂体主要发育于湖侵体系域，很少发育湖底扇。从层序主控因素看，由于构造整体稳定，湖平面变化主要受气候和盆地古地貌影响。
- 松辽盆地 /
- 萎缩期 /
- 层序地层
Abstract: The shrinkage stage is an important part of basin evolution.The research actuality about the sequence stratigraphy of rift basin among faulting stage, depression stage and shrinkage stage shows that there is very little systematic research about the sequence stratigraphy during shrinkage stage, and there is vague understanding of its sequence boundary, structure, and main control factors. In the view of this problem, we carried out a systematic research about the sequence stratigraphy in Sifangtai formation and Mingshui formation which correspond to the shrinkage stage in Songliao basin. One supersequence was defined by two regional unconformities, and it can be divided into six sequences. The comparison and analysis on the geologic feature between depression stage and shrinkage stage in Songliao Basin shows that it is a shallow lake with smooth topography, and its representative characteristics are lowamplitude structure, low accommodation space, frequently up and down of base level, and so on. The representative characteristics of sequence boundary are gentle angular unconformity, lowangle onlap and transfer surface between ascending and falling. The sedimentary facies of this region contain meandering river, meandering river delta, braid river delta, lakes and so on. In their sequence structure, they were divided into two system tract: transgressive system tract and regressive system tract. There is no obvious incised valley in basin margin and few sublacustrine fan was found. Sands are mainly in the transgressive system tract. Because of stable structural setting, sequences were controlled mainly by palaeoclimate and palaeotopography.
- Songliao Basin /
- shrinkage stage /
- sequence stratigraphy

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[1]	秦健铭, 陈积权, 高远, 席党鹏, 王成善. 松辽盆地晚白垩世陆表古温度定量重建 . 沉积学报, 2020, 38(4): 759-770. doi: 10.14027/j.issn.1000-0550.2019.079
[2]	曹怀仁, 胡建芳, 席党鹏, 彭平安, 雷艳. 松辽盆地后金沟剖面烃源岩地球化学特征及其古环境重建 . 沉积学报, 2015, 33(5): 1043-1052. doi: 10.14027/j.cnki.cjxb.2015.05.020
[3]	杜锦霞. 松辽盆地北部青山口组重力流特征研究及其地质意义 . 沉积学报, 2015, 33(2): 385-393. doi: 10.14027/j.cnki.cjxb.2015.02.018
[4]	张晨晨, 张顺, 魏巍, 吴朝东. 松辽盆地嫩江组凝缩层形成机制及其地质意义 . 沉积学报, 2015, 33(5): 891-898. doi: 10.14027/j.cnki.cjxb.2015.05.005
[5]	陈方文, 卢双舫, 丁雪. 松辽盆地齐家—古龙凹陷中浅层烃源岩生烃量评价 . 沉积学报, 2014, 32(6): 1181-1187.
[6]	. 松辽盆地嫩江组层序构型及其沉积演化 . 沉积学报, 2013, 31(05): 920-927.
[7]	. 松辽盆地扶新隆起带南部扶余油层沉积特征及沉积模式探讨 . 沉积学报, 2012, 30(4): 706-715.
[8]	. 松辽盆地北部地层水同位素特征及其地质意义 . 沉积学报, 2012, 30(2): 399-404.
[9]	. 松辽盆地十屋断陷十屋地区营城组物源体系探讨 . 沉积学报, 2011, 29(6): 1096-1104.
[10]	孙雨. 松辽盆地红岗北地区扶余油层岩性油藏特征及控制因素分析 . 沉积学报, 2009, 27(4): 760-768.
[11]	张世广. 高分辨率层序地层学在储层宏观非均质性研究中的应用——以松辽盆地朝阳沟油田朝1—朝气3区块扶余油层为例 . 沉积学报, 2009, 27(3): 458-469.
[12]	辛仁臣. 湖盆无曝露缓坡带层序界面特征及成因——以松辽盆地他拉哈地区上白垩统为例 . 沉积学报, 2008, 26(1): 77-85.
[13]	楼章华. 沉积盆地地下水动力场特征研究①——以松辽盆地为例 . 沉积学报, 2006, 24(2): 193-201.
[14]	王颖, 王英民, 王晓洲, 辛仁臣, 赵志魁, 赵占银. 松辽盆地西部坡折带的成因演化及其对地层分布模式的控制作用 . 沉积学报, 2005, 23(3): 498-506.
[15]	冯子辉, 冯志强, 刘伟, 王雪, 关秋华. 松辽盆地北部深层凝析油及油型气的成因研究 . 沉积学报, 2004, 22(S1): 45-49.
[16]	邹才能, 王兆云, 徐冠军, 吴小洲, 孙效东, 王建伟. 松辽盆地西斜坡稠油特征及成因 . 沉积学报, 2004, 22(4): 700-706.
[17]	辛仁臣, 蔡希源, 王英民. 松辽坳陷深水湖盆层序界面特征及低位域沉积模式 . 沉积学报, 2004, 22(3): 387-392.
[18]	王立武, 李建忠, 王兆云, 卢宗盛. 松辽盆地保乾三角洲前缘带演变及其勘探意义 . 沉积学报, 2003, 21(3): 404-408.
[19]	杨玉峰, 王占国, 张维琴. 松辽盆地湖相泥岩地层有机碳分布特征及层序分析 . 沉积学报, 2003, 21(2): 340-344.
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松辽盆地北部湖盆萎缩期层序结构与沉积充填

韩建辉

中国石油大学资源与信息学院北京 102249

通讯作者: 韩建辉

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2009-06-10

关键词:

松辽盆地 /

萎缩期 /

层序地层

摘要: 萎缩期是陆相湖盆演化的重要阶段，但和断陷期、坳陷期相比，对湖泊萎缩期的沉积充填和层序构成的认识非常不足，研究也非常薄弱。松辽盆地的四方台期和明水期是典型的湖盆萎缩期，对其沉积充填和层序构成的研究有助于加深学术界和工业界对这一重要阶段的认识和促进油气勘探。将四方台组、明水组划分为一个超层序，六个三级层序。对比分析了松辽盆地坳陷期与萎缩期地质特征，认为盆地萎缩期为地形平缓的浅水盆地，具有构造幅度低、可容空间小、湖平面升降频繁等特点。层序界面多表现为低角度不整合、低幅上超面以及沉积转换面等；沉积上，该段主要发育河流相、浅水湖泊、浅水三角洲等沉积相。层序结构上，由于没有明显坡折带，故采用两分法划分体系域，包括湖侵体系域(TST)和湖退体系域(RST)；盆地边缘没有明显的的下切谷特征，砂体主要发育于湖侵体系域，很少发育湖底扇。从层序主控因素看，由于构造整体稳定，湖平面变化主要受气候和盆地古地貌影响。

English Abstract

Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗

HAN JianHui

School of Resource and Information Technology in China University of Petroleum, Beijing 102249

Corresponding author: HAN JianHui

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2009-06-10

Keywords:

Abstract: The shrinkage stage is an important part of basin evolution.The research actuality about the sequence stratigraphy of rift basin among faulting stage, depression stage and shrinkage stage shows that there is very little systematic research about the sequence stratigraphy during shrinkage stage, and there is vague understanding of its sequence boundary, structure, and main control factors. In the view of this problem, we carried out a systematic research about the sequence stratigraphy in Sifangtai formation and Mingshui formation which correspond to the shrinkage stage in Songliao basin. One supersequence was defined by two regional unconformities, and it can be divided into six sequences. The comparison and analysis on the geologic feature between depression stage and shrinkage stage in Songliao Basin shows that it is a shallow lake with smooth topography, and its representative characteristics are lowamplitude structure, low accommodation space, frequently up and down of base level, and so on. The representative characteristics of sequence boundary are gentle angular unconformity, lowangle onlap and transfer surface between ascending and falling. The sedimentary facies of this region contain meandering river, meandering river delta, braid river delta, lakes and so on. In their sequence structure, they were divided into two system tract: transgressive system tract and regressive system tract. There is no obvious incised valley in basin margin and few sublacustrine fan was found. Sands are mainly in the transgressive system tract. Because of stable structural setting, sequences were controlled mainly by palaeoclimate and palaeotopography.

韩建辉. 松辽盆地北部湖盆萎缩期层序结构与沉积充填[J]. 沉积学报, 2009, 27(3): 479-486.

引用本文:

韩建辉. 松辽盆地北部湖盆萎缩期层序结构与沉积充填[J]. 沉积学报, 2009, 27(3): 479-486.

HAN JianHui. Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗[J]. Acta Sedimentologica Sinica, 2009, 27(3): 479-486.

Citation:

HAN JianHui. Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗[J]. Acta Sedimentologica Sinica, 2009, 27(3): 479-486.

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松辽盆地北部湖盆萎缩期层序结构与沉积充填

通讯作者:
韩建辉

计量

Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗

Corresponding author: HAN JianHui

计量

目录

松辽盆地北部湖盆萎缩期层序结构与沉积充填

中国石油大学资源与信息学院北京 102249

通讯作者: 韩建辉

English Abstract

Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗

School of Resource and Information Technology in China University of Petroleum, Beijing 102249

Corresponding author: HAN JianHui

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松辽盆地北部湖盆萎缩期层序结构与沉积充填

通讯作者: 韩建辉

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Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗

Corresponding author: HAN JianHui

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出版历程

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松辽盆地北部湖盆萎缩期层序结构与沉积充填

中国石油大学资源与信息学院 北京 102249

通讯作者: 韩建辉

English Abstract

Sequence Structure and Depositional Filling of Northern Songliao Basin During Shrinkage Stage〖HT5SS〗

School of Resource and Information Technology in China University of Petroleum, Beijing 102249

Corresponding author: HAN JianHui

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通讯作者:
韩建辉

中国石油大学资源与信息学院北京 102249