鄂尔多斯盆地多种能源矿产分布及其构造背景

邓军; 王庆飞; 高帮飞; 徐浩; 周应华

鄂尔多斯盆地多种能源矿产分布及其构造背景

邓军^{1, 2,},
王庆飞^{1, 2},
高帮飞^{1, 2},
徐浩^{1, 2},
周应华^{1, 2}

1.
中国地质大学地质过程与矿产资源国家重点实验室, 北京 100083
2.
中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室, 北京 100083

基金项目:

国家重点基础研究规划项目 2003CB214600

教育部科学技术研究重点项目 0318

详细信息

作者简介:
邓军(1958-), 男, 教授, 博士生导师, 矿床学和构造地质学专业, 主要从事区域构造、成矿流体及成矿动力学的教学和科研工作. E-mail: djun@cug.edu.cn

中图分类号: P617;P542
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出版历程
- 刊出日期: 2006-05-25

Distribution and Tectonic Background of Various Energy Resources in Ordos Basin

DENG Jun^{1, 2
,},
WANG Qing-fei^{1, 2},
GAO Bang-fei^{1, 2},
XU Hao^{1, 2},
ZHOU Ying-hua^{1, 2}

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China

摘要

摘要: 借助“成矿系统”的思维, 探讨鄂尔多斯盆地成矿(藏)系统形成机制及其构造背景.盆地于中生代处于大地构造体制转折的重要阶段, 盆地边缘的造山活动显著, 盆内亦分别于晚三叠世、晚侏罗世与晚白垩世左右发生过3次构造热事件.区域构造体制转换事件导致了多种成藏(矿)作用的发生.盆地内部的构造热事件引发了有机流体的活动, 周缘造山作用产生了向盆内流动的无机含铀热液.有机和无机流体的活动过程中存在相互作用, 有机流体的存在形成氧化-还原障, 导致无机流体关键物理化学参数的转变, 在氧化-还原界面处成矿.突变成矿和界面成矿是多种能源矿产成矿过程的主要机制.
- 鄂尔多斯盆地 /
- 多种能源矿产 /
- 造山作用 /
- 界面成矿
Abstract: The formation process of the various energy resources coexisting system and its regional tectonic background in Ordos basin are analyzed by introducing the "metallogenic system" theory in this paper. The Mesozoic is the important transition period of the regional tectonic regime, during which the orogeny is outstanding around the basin and three rectothermal events took place in the basin. The transition of the tectonic regime induces the occurrence of various accumulating processes of the inorganic and organic fluids, for example, the organic fluid in the basin is activated by the recto-thermal events and the inorganic fluid flowing towards the basin is produced due to the orogeny. The reciprocity between the inorganic and organic fluids happens during their transporting. The existence of the organic fluid produces the redox barrier, which causes the mutation of the physicochemical parameters of the inorganic fluid and the precipitation of the uranium element at the interface. The mutation and interface effects are obvious in the formation of the various energy resources.
- Ordos basin /
- various energy resources /
- orogeny /
- interface mineralization

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图 1 多种能源矿产共存系统演化框架(据翟裕生等, 1999改编)

Fig. 1. Evolution of coexisting system of various energy resources

下载: 全尺寸图片幻灯片

图 2 鄂尔多斯盆地大地构造图(据Liu, 1998; Brian and Bradley, 2002修编)

Ⅰ₁.贺兰山-六盘山构造带; Ⅰ₂.北祁连造山带; Ⅰ₃.中祁连造山带; Ⅰ₄.南祁连构造带; Ⅱ₁.北秦岭造山带; Ⅱ₂.南秦岭造山带; Ⅲ.吕梁山; Ⅳ₁.狼山; Ⅳ₂.大青山; F₁.得力记剪切带; F₂.马鞘山-靖远断裂; F₃.北祁连断裂; F₄.北祁连-北秦岭缝合带; F₅.宝鸡-洛阳栾川断裂; YR.黄河; 1.走滑断裂; 2.山前正断层; 3.逆冲断层; 4.缝合带; 5.地质界线; 6.鄂尔多斯盆地边界(盆地边界据重力梯度带划定); ①.银川地堑; ②.渭河地堑; ③.山西地堑; ④.河套盆地

Fig. 2. Tectonic map of Ordos basin

下载: 全尺寸图片幻灯片

图 3 鄂尔多斯盆地多种能源矿产分布图(据魏永佩和欧阳自远, 2004; 长庆油田公司勘探开发研究院, 2001编制)

1.侏罗纪石油; 2.延长组石油; 3.天然气; 4.铀; 5.延长组生油坳陷; 6. 延长组展布区

Fig. 3. Distribution map of various energy resources in Ordos basin

下载: 全尺寸图片幻灯片

图 4 鄂尔多斯盆地中生代构造热事件与多种能源矿产形成

Fig. 4. Time of the tecto-thermal events and the formation of various energy resources in Ordos basin

下载: 全尺寸图片幻灯片

表 1 鄂尔多斯盆地多种能源矿产分布

Table 1. Distribution of various energy resources in Ordos basin

表 2 鄂尔多斯盆地侏罗纪构造体制转换与煤形成(王双明，1996; 王超勇等，2004)

Table 2. Relationship of the formation of Jurassic coal and the transition of tectonic regime in Ordos basin

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