鄱阳湖盆地的地质演化、新构造运动及其成因机制探讨

杨晓东; 吴中海; 张海军

鄱阳湖盆地的地质演化、新构造运动及其成因机制探讨

杨晓东^{1, 2,},
吴中海^{2, 3, ,},
张海军¹

1.
中国地质大学(北京)地球科学与资源学院, 北京 100083
2.
中国地质科学院地质力学研究所, 北京 100081
3.
国土资源部新构造运动与地质灾害重点实验室, 北京 100081

基金项目:

中国地质调查局地质调查项目 12120114002101

中国地质调查局地质调查项目 DD20160268

国家自然科学基金项目 41571013

国家自然科学基金项目 41171009

详细信息

作者简介:
杨晓东(1991-), 男, 硕士研究生, 专业方向为沉积地质学与环境分析。E-mail:dong6015@qq.com

通讯作者:
吴中海(1974-), 男, 研究员, 从事新构造和活动构造研究。E-mail:wzhh4488@sina.com

中图分类号: P546
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- PDF下载量: 30
- 被引次数: 0
出版历程
- 收稿日期: 2016-03-07
- 刊出日期: 2016-09-28

GEOLOGICAL EVOLUTION, NEOTECTONICS AND GENETIC MECHANISM OF THE POYANG LAKE BASIN

YANG Xiao-dong^{1, 2
,},
WU Zhong-hai^{2, 3
, ,},
ZHANG Hai-jun¹

1.
College of Earth Science and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
Key Lab of Neotectonic Movement and Geohazards, Ministry of Land and Mineral Resources, Beijing 100081, China

摘要

摘要: 综合鄱阳湖盆地的沉积特征和构造活动特点，并结合钻孔及剖面资料，分析了鄱阳湖盆地在东亚地区中新生代大地构造背景下的地质演化过程，总结了控制鄱阳湖盆地发展的主要断裂构造及其特征以及盆地的中新生代沉积古地理演化，最后进一步根据已有资料，总结了区域主要断裂的第四纪活动性及与地震活动的关系，并探讨析了盆地的成因机制。综合研究认为，在中生代，中国东南部的燕山运动事件使一套大致平行的北东-南西向断裂带形成，并在此时期导致了鄱阳湖断陷，形成鄱阳湖沉积盆地的雏形；之后，随着赣江断裂系活动方式的变化，鄱阳湖盆地经历了复杂的构造演化过程；至第四纪，盆地中部发生整体拗陷并持续接受沉积；全新世中期后，演化成现代鄱阳湖。
- 鄱阳湖盆地 /
- 地质演化 /
- 新构造 /
- 活动断裂 /
- 地震
Abstract: Combining with drilling and profile data, this paper synthesizes the sedimentary characteristics and tectonic activity characteristics of the Poyang Lake Basin and discusses the development and evolution of the basin in the tectonic background of East Asia, and also summarizes the main control faults structures and their characteristics in the basin as well as it's paleogeographic evolution in the Mesozoic and Cenozoic. Finally summarizes the main fracture of Quaternary activity and its relationship with seismic activity, and the genetic mechanism of the basin is discussed according to the existing data. Comprehensive study showed that, in the Mesozoic, the movement of Yanshan brought about a set of roughly parallel NE-SW trending fault zones in southeast of China, and resulted in the Poyang lake depression and the embryonic form of Poyang lake sedimentary basin. Then, with the change of the Ganjiang fault mode, Poyang lake basin has experienced a complex evolution process. Until the Quaternary, overall depression occurred in the middle of the basin and it continued to be deposited. After the mid Holocene, it evolved into the modern Poyang Lake.
- the Poyang Lake Basin /
- geological evolution /
- neotectonics /
- active fault /
- earthquake

HTML全文

图 1 江西中北部鄱阳湖盆地地质图

Figure 1. Geological map of the Poyang Lake Basin in centra-north Jiangxi

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图 2 鄱阳湖盆地构造分区简图(据周松源等^[22])

Figure 2. Tectonic divisions of the Poyang Lake Basin

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图 3 盆地内部地震构造解释图^[11](剖面位置见图 2)

T₁—南雄组三段(K₂n³)底面；T₂—南雄组二段(K₂n²)底面；T₃—南雄组一段(K₂n¹)底面；T₄—周家店组(K₂z)底面；T₅—冷水坞组(K₁l)底面(即前白垩系顶面)；走滑断裂：Fa—赣江断裂主枝(南昌—丁坊)；Fa′—赣江断裂副枝(新建—坪湖)；Fb—进贤—石门街断裂主枝(进贤—长山)；Fb′—进贤—石门街断裂副枝(钟陵—石门街)

Figure 3. Seismic structural interpretation in the Poyang Lake Basin

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图 4 白垩—古近系地层序列特征^[11]

Figure 4. Stratigraphic sequence and sedimentary features of the Cretaceous and Paleogene

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图 5 鄱阳湖盆地地质演变简图(据文献[14]，[22]修改)

Ⅰ—早白垩世拉分盆地雏形出现；Ⅱ—晚白垩—古近纪盆地稳定扩张阶段；Ⅲ—新近纪—第四纪盆地萎缩，呈整体拗陷阶段，受多条断裂影响；Fa—赣江断裂；Fb—进贤—石门街断裂

Figure 5. Geological evolution sketch of the Poyang Lake Basin

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图 6 第四纪各时期鄱阳湖盆地剖面图^[33]

Figure 6. Section maps of Poyang Lake Basin during the Quaternary period

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图 7 鄱阳湖东西两侧沉积垂向特征^{[45, 47]}

Figure 7. Vertical characteristics of the deposition in the east and west of Poyang Lake

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图 8 鄱阳湖周缘全新世沉积剖面图^[47]

Figure 8. Holocene sedimentary profile of Poyang Lake periphery

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图 9 江西省北部断裂与地震分布简图

① 武宁-铜鼓断裂; ② 九江-靖安断裂; ③ 湖口-吉安断裂(渊赣江断裂冤); ④ 宜丰-新建断裂; ⑤ 余干-鹰潭断裂; ⑥ 抚河断裂; ⑦ 宜春-东乡断裂; ⑧ 余干-婺源断裂

Figure 9. The distribution of earthquakes and faults in the north Jiangxi

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图 10 西太平洋白垩纪以来的活动演变示意图^[25]

1-早白垩世岩浆岩; 2-断陷盆地沉积; 3-新生代玄武岩; TLF-郯庐断裂带; QDO-秦岭大别造山带; SLO-苏鲁造山带

Figure 10. A sketch map showing plate motion evolution in West Pacific area since Cretaceous

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表 1 各类沉积体系的时间域^[47]

Table 1. Time domain of sedimentary systems

沉积体系	时间域/a
冲积扇—扇三角洲	12000~4100
辫状河	4100~2000
曲流河	2000~1700
破坏型三角洲	1700~250
建设型三角洲	250~今

下载: 导出CSV

表 2 赣北地区主要活动断裂基本特征^[21]

Table 2. Characteristics of main active faults in northern Jiangxi

断裂名称	长度/km	走向	活动性质	活动强度	最新活动
九江—靖安断裂	150	NNE	右旋走滑	一般	晚更新世
宜丰—新建断裂	97	NE	右旋走滑	一般	全新世
武宁—铜鼓断裂	100	NE	右旋逆冲走滑	一般	全新世
湖口—吉安断裂	227	NE	右旋走滑	一般	全新世
余干—婺源断裂	110	NE	右行走滑	一般
抚河断裂	220	NW	左旋走滑	不明显
余干—鹰潭断裂	260	NW	左旋走滑	一般	全新世
宜春—东乡断裂	400	EW	右行走滑	一般

下载: 导出CSV

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