中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

刘磊; 钟怡江; 陈洪德; 王峻

doi:10.14027/j.cnki.cjxb.2015.06.010

ISSN 1000-0550 CN 62-1038/P

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中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

刘磊, 钟怡江, 陈洪德, 王峻

文章导航 > 沉积学报 > 2015 > 33(6): 1170-1181

刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究[J]. 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

引用本文:

刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究[J]. 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

LIU Lei, ZHONG YiJiang, CHEN HongDe, WANG Jun. Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

Citation:

LIU Lei, ZHONG YiJiang, CHEN HongDe, WANG Jun. Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究[J]. 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

引用本文:

刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究[J]. 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

Citation:

中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

doi: 10.14027/j.cnki.cjxb.2015.06.010

1.
成都理工大学沉积地质研究院成都 610059;
2.
油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059

基金项目: 四川省重点学科构造地质学建设基金项目(编号:SZD0408)、地调项目(编号:1212011220762)与中海油天津分公司项目(编号:CCL2013TJXSBS1880)联合资助

详细信息

作者简介:
刘磊男 1988年出生硕士研究生沉积学与石油地质学研究 E-mail:172058088@qq.com

中图分类号: TE122.1

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文章访问数: 395
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PDF下载量: 1158
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Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China

1.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059;
2.
State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059

摘要

摘要: 中国东部箕状断陷湖盆短轴方向,常常发育扇三角洲和辫状河三角洲,二者均可形成良好的油气储集体,但在岩芯以及地球物理资料的识别上常常容易混淆。通过对它们沉积特征、地球物理资料特征、含油气性和控制因素的对比研究和分析认为:扇三角洲是陡坡带冲积扇直接入湖形成,地震反射特征为楔形前积,沉积物成分成熟度和结构成熟度均低于辫状河三角洲,沉积特征反映重力流和牵引流双重作用;辫状河三角洲是缓坡带辫状河入湖形成的三角洲,向湖盆方向推进较远,地震反射特征为叠瓦前积,沉积特征反映牵引流作用。扇三角洲易形成构造-岩性油气藏和岩性油气藏,有利相带为扇三角洲前缘水下分流河道、席状砂以及前扇三角洲容易发育的滑塌浊积扇;辫状河三角洲易形成地层-岩性油气藏和岩性油气藏,有利相带为辫状河三角洲平原辫状分流河道,辫状河三角洲前缘水下分流河道、河口坝、席状砂以及半深湖中的浊积岩体。古气候变化、构造-古地貌以及湖平面变化速率三者共同作用于扇三角洲和辫状河三角洲的沉积特征,其中构造-古地貌是主控因素。结合二者沉积特征差异,建立了中国东部箕状断陷湖盆扇三角洲和辫状河三角洲沉积模式图,以期能对相似构造背景下扇三角洲和辫状河三角洲的分析与研究提供一定的指导作用。
- 箕状断陷盆地 /
- 扇三角洲 /
- 辫状河三角洲
Abstract: Fan deltas and braided river deltas are widely developed along the direction of minor axis in half-graben rift lake basin of East China. Both of them can form good oil and gas reservoir, but the identifications of them in well core and geophysical data are easy to confuse. Through the comparison and analysis of sedimentary features, geophysical data, oil-gas-bearing and controlling factors, we conclude that fan deltas are formed by alluvial fans running into lake along steep-slope zone and its seismic reflection characters is wedge foreset. The sediment composition maturity and structural maturity of fan deltas are lower than that of braided river deltas. The sedimentary features of fan deltas reflect the gravity current and tractive current sediments combined effection. Braided river deltas are formed by braided river flow into lake far away along gentle slope zone and its seismic reflection characters is imbricate foreset. The sedimentary characters of braided river deltas reflect the tractive current sediments effection. Fan deltas can form fault-lithologic reservoir and lithologic reservoir. Its favorable reservoir zone includes underwater distributary channel, sheet-like sand of fan delta front and slump turbid fan formed in pre-fan delta. Braided river deltas can form strata-lithologic reservoir and lithologic reservoir of which favorable reservoir includes braid-river channel of braid river delta plain and underwater distributary channel, mouth bar, sheet-like sand of braid river delta front. Besides above, turbidity sandstone is also favorable reservoir in fairly deep lake. The sedimentary features of fan deltas and braid river deltas are controlled by palaeoclimate, tectonic-palaeogeomorphology and lake level fluctuations; Tectonic-palaeogeomorphology is the critical factor among them. The depositional model of fan deltas and braided river deltas in half-graben rift lake basin of East China is established by combining the sedimentary features difference between them so as to provide guidance to analysis and research for them in similar geological background.
- half-graben rift lake basin /
- fan delta /
- braided river delta

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[1]	陶金雨, 张昌民, 郭旭光, 朱锐, 潘进, 唐勇. 磨圆度定量表征在扇三角洲沉积微相判别中的应用 . 沉积学报, 2020, 38(5): 956-965. doi: 10.14027/j.issn.1000-0550.2019.111
[2]	蒋庆平, 孔垂显, 李维锋, 邱子刚, 卢志远, 常天全, 刘凯, 陈栋梁, 李胜, 袁晓光. 陆相湖盆大型扇三角洲沉积特征与演化规律 . 沉积学报, 2020, 38(5): 923-932. doi: 10.14027/j.issn.1000-0550.2019.089
[3]	王越. 新疆塔尔朗沟剖面中二叠统扇三角洲混合沉积特征及模式 . 沉积学报, 2019, 37(5): 922-933. doi: 10.14027/j.issn.1000-0550.2018.190
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[5]	赵晨帆, 于兴河, 付超, 韩小琴, 杜永慧. 曲流河三角洲—辫状河三角洲控制因素及演化过程探讨 . 沉积学报, 2019, 37(4): 768-784. doi: 10.14027/j.issn.1000-0550.2018.154
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[7]	黄薇, 吴海波, 李军辉, 刘赫. 海—塔盆地中部断陷带南屯组沉积体系配置及有利相带分析 . 沉积学报, 2016, 34(1): 120-128. doi: 10.14027/j.cnki.cjxb.2016.01.011
[8]	邹妞妞, 史基安, 张大权, 马崇尧, 张顺存, 鲁新川. 准噶尔盆地西北缘玛北地区百口泉组扇三角洲沉积模式 . 沉积学报, 2015, 33(3): 607-615. doi: 10.14027/j.cnki.cjxb.2015.03.019
[9]	赵俊青, 纪友亮, 夏斌, 张善文, 刘宝明. 扇三角洲沉积体系高精度层序地层学研究 . 沉积学报, 2004, 22(2): 302-309.
[10]	鄢继华, 陈世悦, 程立华. 扇三角洲亚相定量划分的思考 . 沉积学报, 2004, 22(3): 443-448.
[11]	高剑波, 钟建华, 徐小林, 温志峰, 黄立功, 刘云田, 江波. 阿尔金断裂为边界的盆地斜坡带扇三角洲 . 沉积学报, 2004, 22(2): 206-215.
[12]	李维锋, 何幼斌, 彭德堂, 王方平, 刘学锋. 新疆尼勒克地区下侏罗统三工河组辫状河三角洲沉积 . 沉积学报, 2001, 19(4): 512-516.
[13]	张春生, 刘忠保, 施冬, 贾爱林. 扇三角洲形成过程及演变规律 . 沉积学报, 2000, 18(4): 521-526.
[14]	周丽清, 吴胜和, 熊琦华, 马晓芬, 郭燕华, 林双运. 吐哈盆地WM油田辫状河三角洲前缘砂体分析 . 沉积学报, 2000, 18(2): 248-252.
[15]	李维锋, 高振中, 彭德堂, 王成善. 库车坳陷中生界三种类型三角洲的比较研究 . 沉积学报, 1999, 17(3): 430-434.
[16]	刘志飞, 王成善. 西藏日喀则地区早白垩世恰布林组辫状河—扇三角洲沉积 . 沉积学报, 1998, 16(3): 6-13.
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[18]	李文厚, 林晋炎, 袁明生, 王武和. 吐鲁番－哈密盆地的两种粗碎屑三角洲 . 沉积学报, 1996, 14(3): 113-121.
[19]	于兴河, 王德发, 孙志华. 湖泊辫状河三角洲岩相、层序特征及储层地质模型──内蒙古贷岱海湖现代三角洲沉积考察 . 沉积学报, 1995, 13(1): 48-58.
[20]	顾家裕, 何斌. 塔里木盆地轮南地区三叠系扇三角洲沉积与储集层研究 . 沉积学报, 1994, 12(2): 54-62.

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中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

doi: 10.14027/j.cnki.cjxb.2015.06.010

1. 成都理工大学沉积地质研究院成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059

基金项目: 四川省重点学科构造地质学建设基金项目(编号:SZD0408)、地调项目(编号:1212011220762)与中海油天津分公司项目(编号:CCL2013TJXSBS1880)联合资助

作者简介:
刘磊男 1988年出生硕士研究生沉积学与石油地质学研究 E-mail:172058088@qq.com

收稿日期: 2014-12-12
修回日期: 2015-01-20
刊出日期: 2015-12-10

中图分类号: TE122.1

关键词:

箕状断陷盆地 /

扇三角洲 /

辫状河三角洲

摘要: 中国东部箕状断陷湖盆短轴方向,常常发育扇三角洲和辫状河三角洲,二者均可形成良好的油气储集体,但在岩芯以及地球物理资料的识别上常常容易混淆。通过对它们沉积特征、地球物理资料特征、含油气性和控制因素的对比研究和分析认为:扇三角洲是陡坡带冲积扇直接入湖形成,地震反射特征为楔形前积,沉积物成分成熟度和结构成熟度均低于辫状河三角洲,沉积特征反映重力流和牵引流双重作用;辫状河三角洲是缓坡带辫状河入湖形成的三角洲,向湖盆方向推进较远,地震反射特征为叠瓦前积,沉积特征反映牵引流作用。扇三角洲易形成构造-岩性油气藏和岩性油气藏,有利相带为扇三角洲前缘水下分流河道、席状砂以及前扇三角洲容易发育的滑塌浊积扇;辫状河三角洲易形成地层-岩性油气藏和岩性油气藏,有利相带为辫状河三角洲平原辫状分流河道,辫状河三角洲前缘水下分流河道、河口坝、席状砂以及半深湖中的浊积岩体。古气候变化、构造-古地貌以及湖平面变化速率三者共同作用于扇三角洲和辫状河三角洲的沉积特征,其中构造-古地貌是主控因素。结合二者沉积特征差异,建立了中国东部箕状断陷湖盆扇三角洲和辫状河三角洲沉积模式图,以期能对相似构造背景下扇三角洲和辫状河三角洲的分析与研究提供一定的指导作用。

English Abstract

Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059;

2. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059

Received Date: 2014-12-12
Rev Recd Date: 2015-01-20
Publish Date: 2015-12-10

Keywords:

Abstract: Fan deltas and braided river deltas are widely developed along the direction of minor axis in half-graben rift lake basin of East China. Both of them can form good oil and gas reservoir, but the identifications of them in well core and geophysical data are easy to confuse. Through the comparison and analysis of sedimentary features, geophysical data, oil-gas-bearing and controlling factors, we conclude that fan deltas are formed by alluvial fans running into lake along steep-slope zone and its seismic reflection characters is wedge foreset. The sediment composition maturity and structural maturity of fan deltas are lower than that of braided river deltas. The sedimentary features of fan deltas reflect the gravity current and tractive current sediments combined effection. Braided river deltas are formed by braided river flow into lake far away along gentle slope zone and its seismic reflection characters is imbricate foreset. The sedimentary characters of braided river deltas reflect the tractive current sediments effection. Fan deltas can form fault-lithologic reservoir and lithologic reservoir. Its favorable reservoir zone includes underwater distributary channel, sheet-like sand of fan delta front and slump turbid fan formed in pre-fan delta. Braided river deltas can form strata-lithologic reservoir and lithologic reservoir of which favorable reservoir includes braid-river channel of braid river delta plain and underwater distributary channel, mouth bar, sheet-like sand of braid river delta front. Besides above, turbidity sandstone is also favorable reservoir in fairly deep lake. The sedimentary features of fan deltas and braid river deltas are controlled by palaeoclimate, tectonic-palaeogeomorphology and lake level fluctuations; Tectonic-palaeogeomorphology is the critical factor among them. The depositional model of fan deltas and braided river deltas in half-graben rift lake basin of East China is established by combining the sedimentary features difference between them so as to provide guidance to analysis and research for them in similar geological background.

刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究[J]. 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

引用本文:

刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究[J]. 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010

Citation:

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中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

doi: 10.14027/j.cnki.cjxb.2015.06.010

作者简介:
刘磊男 1988年出生硕士研究生沉积学与石油地质学研究 E-mail:172058088@qq.com

计量

Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China

计量

目录

中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

doi: 10.14027/j.cnki.cjxb.2015.06.010

1. 成都理工大学沉积地质研究院成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059

作者简介:
刘磊男 1988年出生硕士研究生沉积学与石油地质学研究 E-mail:172058088@qq.com

English Abstract

Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059;

2. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059

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中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

doi: 10.14027/j.cnki.cjxb.2015.06.010

作者简介: 刘磊 男 1988年出生 硕士研究生 沉积学与石油地质学研究 E-mail:172058088@qq.com

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出版历程

Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China

计量

出版历程

目录

中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究

doi: 10.14027/j.cnki.cjxb.2015.06.010

1. 成都理工大学沉积地质研究院 成都 610059; 2. 油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059

作者简介: 刘磊 男 1988年出生 硕士研究生 沉积学与石油地质学研究 E-mail:172058088@qq.com

English Abstract

Contrastive Research of Fan Deltas and Braided River Deltas in Half-graben Rift Lake Basin in East China

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059; 2. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059

全文HTML

目录

友情链接

期刊在线

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作者简介:
刘磊男 1988年出生硕士研究生沉积学与石油地质学研究 E-mail:172058088@qq.com

1. 成都理工大学沉积地质研究院成都 610059;

2. 油气藏地质及开发工程国家重点实验室(成都理工大学) 成都 610059

作者简介:
刘磊男 1988年出生硕士研究生沉积学与石油地质学研究 E-mail:172058088@qq.com

1. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059;

2. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation(Chengdu University of Technology), Chengdu 610059