旋扭构造研究的进展

李东旭; 宋立才; 张林炎

doi:10.12090/j.issn.1006-6616.2019.25.05.080

旋扭构造研究的进展

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

基金项目:
中国地质科学院地质力学研究所基本科研业务费（DZLXJK201613）

详细信息

作者简介: 李东旭(1933-), 男, 教授, 博士生导师, 长期从事构造地质学、地质力学教学与科研。E-mail:dxlee18@126.com

中图分类号: P552

责任编辑：吴芳

收稿日期: 2019-08-28

修回日期: 2019-09-29

刊出日期: 2019-10-31

PROGRESS IN RESEARCH ON ROTATION-SHEAR STRUCTURE

1.
China University of Geosciences(Beijing), Beijing 100083, China

2.
Institude of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

Received Date: 28 August 2019

Revised Date: 29 September 2019

Publish Date: 31 October 2019

摘要

摘要:
文章综述了中国地质学家对旋扭构造研究的历史与成果，也介绍了国外相关研究成果。李四光先生通过四篇论著奠定了旋扭构造的理论基础。在后来的研究和找矿实践、多种模拟仿真新方法试验以及力学解析中进一步丰富了旋扭构造的研究内容，深化了对旋扭构造几何学、运动学特征与动力学机制等的认识，提出了有些旋扭构造是螺旋运动的结果及旋扭构造的形成很可能与地球旋转动力问题有关；特别是在找矿勘探方面取得的成功和经济效益，提高了成矿理论认识的水平。文章最后提出今后研究旋扭构造应注意的问题。
- 旋扭构造 /
- 螺旋运动 /
- 旋扭构造控矿 /
- 旋扭构造模拟 /
- 旋扭构造力学解析 /
- 旋扭构造动力学
Abstract:
This paper reviews the history and progress of geomechanics research on rotation-shear structure in China. It also reflects the relevant research results abroad. J.S.Lee laid the theoretical foundation of rotation-shear structure through four theses. The subsequent research and ore-prospecting practice, as well as a variety of new methods for simulation tests and mechanical analysis, further enrich the research contents of rotation-shear structure, deepen the understanding on rotation-shear structure geometry, characteristics of kinematics and dynamics mechanism, proposing the idea that some rotation-shear structures are the results of spiral motion, and the formation of rotation-shear structure is likely to be related to the Earth rotation dynamics. Especially the success and economic benefit achieved in prospecting and exploration have improved the understanding on metallogenic theory. Finally, the paper puts forward the problems that should be paid attention to in the future study of the rotation-shear structure.

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图 1 微型帚状构造(牛口峪大南坡一块滚石)

Figure 1.

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图 2 牛口峪旋扭构造图^{[5, 8]}

Figure 2.

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图 3 房山地区地质图^{[7, 9]}

Figure 3.

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图 4 大南坡小旋扭构造砥柱

Figure 4.

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图 5 大南坡小型旋扭构造砥柱及周缘断裂^[6]

Figure 5.

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图 6 骰子沟轴近水平的小型旋扭构造

Figure 6.

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图 7 骰子沟中旋轴近于水平的小型旋扭构造^{[5, 8]}

Figure 7.

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图 8 轴近直立的旋扭构造导生出低序次轴近水平的旋扭构造三维模式^[8]

Figure 8.

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图 9 牛口峪西沟小型旋扭构造序次、复合关系露头图解

Figure 9.

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图 10 房山岩体与北岭向斜构造^[6-7]

Figure 10.

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图 11 房山岩体斜冲侵位水平分力^[7]

Figure 11.

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图 12 凤凰山帚状构造^[7-8]

Figure 12.

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图 13 铜陵地块中S状褶皱群^[12]

Figure 13.

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图 14 沿北东向轴旋转的北西西向褶皱及其形状和产状^[12]

Figure 14.

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图 15 河北邯邢矿山村构造草图^[13]

Figure 15.

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图 16 凤凰山岩体内部及接触带旋扭构造形迹及形成动力条件^[16]

Figure 16.

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图 17 伴随有右螺旋上升流变过渡的理想示意图^{[8, 17]}

Figure 17.

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图 18 迁安铁矿轴近水平的小型旋扭构造^[8]

Figure 18.

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图 19 乌克兰地盾克里沃罗格构造省萨卡萨杂诺斯科环装花岗岩穹隆构造图^[8]

Figure 19.

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图 20 老君山地区变质核杂岩和旋转构造图^[8]

Figure 20.

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图 21 老君山变质核杂岩的构造演化^[8]

Figure 21.

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图 22 涡旋构造地幔柱运动学示意图^{[8, 46]}

Figure 22.

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图 23 临汾陆核出露的区域构造样式及其运动状态示意图^{[8, 46]}

Figure 23.

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图 24 岩石圈旋转构造体系复合现象略图^[47]

Figure 24.

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图 25 差速旋转、岩石圈单元的滑移和蠕动的主要线路^{[8, 24]}

Figure 25.

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图 26 环球螺旋形扭转断裂系统^[48]

Figure 26.

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图 27 北半球大陆边缘反S状造山带三维模式图^[8]

Figure 27.

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图 28 阿尔卑斯—喜马拉雅—印尼反S状旋扭构造连锁造山带^[8]

Figure 28.

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