川东—武陵地区构造格局及其演化

王宗秀; 李春麟; 李会军; 张林炎; 梁明亮; 谭元隆; 李磊磊; 李涛; 高莉; 郭永岩; 刘艳姣; 鄢犀利

doi:10.12090/j.issn.1006-6616.2019.25.05.068

川东—武陵地区构造格局及其演化

doi: 10.12090/j.issn.1006-6616.2019.25.05.068

王宗秀^{1, 2,},
李春麟^{1, 2, ,},
李会军^{1, 2},
张林炎^{1, 2},
梁明亮^{1, 2},
谭元隆^{1, 2},
李磊磊^{1, 2},
李涛³,
高莉^{1, 4},
郭永岩⁵,
刘艳姣⁶,
鄢犀利^{1, 2}

1.
中国地质科学院地质力学研究所, 北京 100081
2.
中国地质科学院页岩油气调查评价重点实验室, 北京 100081
3.
中国地震局地质研究所, 北京 100029
4.
北京市地质调查研究院, 北京 102206
5.
北京市地质勘察技术院, 北京 100011
6.
深圳市地质局, 广东深圳 518023

基金项目:

中国地质调查项目 DD20160183

中国地质科学院地质力学研究所基本科研业务 JYYWF20181201

详细信息

作者简介:
王宗秀(1959-), 男, 研究员, 博士生导师, 构造地质学专业。E-mail:wangzongxiu@sohu.com

通讯作者:
李春麟(1983-), 男, 助理研究员, 构造地质学专业。E-mail:chunlinlee@cags.ac.cn

中图分类号: P542
计量
- 文章访问数: 320
- HTML全文浏览量: 381
- PDF下载量: 56
- 被引次数: 0
出版历程
- 收稿日期: 2019-08-03
- 修回日期: 2019-09-25
- 刊出日期: 2019-10-28

TECTONIC ARCHITECTURE AND EVOLUTION OF THE EASTERN SICHUAN-WULINGSHAN AREA, SOUTH CHINA

WANG Zongxiu^{1, 2
,},
LI Chunlin^{1, 2
, ,},
LI Huijun^{1, 2},
ZHANG Linyan^{1, 2},
LIANG Mingliang^{1, 2},
TAN Yuanlong^{1, 2},
LI Leilei^{1, 2},
LI Tao³,
GAO Li^{1, 4},
GUO Yongyan⁵,
LIU Yanjiao⁶,
YAN Xili^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Key Laboratory of Shale Oil and Gas Geological Survey, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
Institute of Geology, China Earthquake Administration, Beijing 100029, China
4.
Beijing Institute of Geological Survey, Beijing 102206, China
5.
Beijing Institute of Geo-exploration Technology, Beijing 100011, China
6.
Geological Bureau of Shenzhen, Shenzhen 518023, Guangdong, China

摘要

摘要: 陆内变形是现今大陆动力学研究的重要内容之一。川东-武陵地区位于扬子地块的内部，远离板块边界，是研究陆内变形的绝佳场所。通过野外断裂构造详细的解析、褶皱构造的形态分析以及沉积地层接触关系的研究，建立了川东-武陵地区显生宙构造格局，探讨了多期构造演化过程。晚中生代以来的两次构造作用奠定了研究区的构造格架，认为滑脱层的深度及数量从根本上控制了川东-武陵地区侏罗山式褶皱变形的差异，褶皱与断裂构造几乎同时形成，川东地区的隔挡式褶皱为单层滑脱变形的结果，而武陵地区的褶皱构造是由于多层次滑脱背景下、差异隆升剥蚀造成的不同构造层次褶皱出露的结果。结合区域地质演化，提出川东-武陵地区显生宙时期主要经历了五期构造演化。晚志留-中泥盆世、石炭纪末和中、晚三叠世之交，研究区均以整体的抬升作用为主，不发育任何褶皱构造；晚侏罗-早白垩世发生大规模褶皱-逆冲作用；新生代晚期，受印度与欧亚大陆汇聚作用的影响，区内断裂带走滑方向发生反转，早期构造被强烈改造。
- 陆内变形 /
- 滑脱层 /
- 构造演化 /
- 显生宙 /
- 川东—武陵地区
Abstract: Intracontinental deformation is one of the important contents in continental dynamics research. The eastern Sichuan-Wulingshan area is located in the interior of the Yangtze Block, far away from the plate boundary, which is an excellent place to study the intracontinental dynamics. On basis of kinematic analysis of faults, morphological analysis of the folds, and contact relationship of the sedimentary strata in the field, we established the Phanerozoic tectonic architecture and discussed the multiple evolutions of the eastern Sichuan-Wulingshan area. Two tectonic events since the Late Mesozoic have laid the tectonic framework of the study area. The fold deformation differences of the eastern Sichuan-Wulingshan area were fundamentally controlled by the depth and quantity of decollement layers. Folds and faults were formed at the same time. The ridge-like folds in the eastern Sichuan area were the result of single-layer slip deformation, while the fold structures in the Wulingshan area were the result of the exposure of folds at different structural levels by different uplifts and denudations under the multi-layer slip background. Combining with the regional evolution, we proposed a five-stage tectonic evolution model of the eastern Sichuan-Wulingshan area in the Phanerozoic. The first three stages (Late Silurian-Middle Devonian, the end of the Carboniferous, and the Middle-Late Triassic) were dominated by regional uplift, without any folds. Then, large-scale folds and thrusts were developed at the fourth stage in the Late Jurassic-Early Cretaceous. Ultimately, due to the influence of the convergence of the India continent and Eurasia continent, the slip direction of the fault was reversed and the early structure was strongly reformed in the late Cenozoic.
- intracontinental deformation /
- decollement layer /
- tectonic evolution /
- Phanerozoic /
- eastern Sichuan-Wulingshan area
注释:

责任编辑：范二平

HTML全文

图 1 川东—武陵地区构造格架图

Figure 1. Tectonic framework of the eastern Sichuan-Wulingshan area

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图 2 川东—武陵地区构造剖面

(剖面线位置见图 1)

Figure 2. Cross-section in the eastern Sichuan-Wulingshan area

(position of cross-section lines shown in Fig. 1)

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图 3 断裂带野外照片

a—齐岳山断裂带二叠系灰岩逆冲在三叠系灰岩之上；b—齐岳山断裂带上盘二叠系灰岩牵引褶皱；c—张家界断裂带逆冲作用及上盘牵引褶皱；d—张家界断裂带奥陶系灰岩逆冲在志留系粉砂岩之上

Figure 3. Field photos showing the major faults in eastern Sichuan-Wulingshan area

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图 4 断裂带野外照片

a—郁江断裂带内发育的构造透镜体；b—来凤断裂带内的逆冲剪切布丁构造；c—德江断裂带早期左行走滑；d—德江断裂带晚期大型右行走滑破碎带

Figure 4. Field photos showing the faults in eastern Sichuan-Wulingshan area

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图 5 武陵地区不同构造层次地质剖面图

(剖面线位置见图 1)

Figure 5. Cross-section in different tectonic levels from the eastern Sichuan-Wulingshan area

(position of the cross-section lines shown in Fig. 1)

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图 6 武陵地区褶皱成因模式

Figure 6. Formation mechanism of the folds in the eastern Sichuan-Wulingshan area

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图 7 川东—武陵地区四套滑脱层野外照片

a—震旦系白云岩滑脱变形；b—下寒武统页岩滑脱褶皱；c—下志留统页岩剪切变形；d—下三叠统薄层灰岩滑脱褶皱

Figure 7. Field photos showing the decollement layers in the eastern Sichuan-Wulingshan area

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图 8 川东—武陵地区下三叠统大冶组滑脱褶皱轴面(P)及枢纽(L)赤平投影(下半球投影)

Figure 8. Stereonet plots of the axial surfaces (P) and axes (L) of the decollement folds within the Lower Triassic Daye Formation in the eastern Sichuan-Wulingshan area (lower hemisphere projection)

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图 9 川东—武陵地区代表性地层柱状图

Figure 9. Representative stratigraphic columns in the eastern Sichuan-Wulingshan area

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图 10 川东—武陵地区显生宙构造演化模式图

Figure 10. Schematic illustration of the tectonic evolution of the eastern Sichuan-Wulingshan area

下载: 全尺寸图片幻灯片

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