雪峰山西侧梵净山—桑植地区构造变形特征

周小军; 李三忠; 王岳军; 刘静

doi:10.3799/dqkx.2011.104

雪峰山西侧梵净山—桑植地区构造变形特征

doi: 10.3799/dqkx.2011.104

周小军^{1, 5,},
李三忠²,
王岳军³,
刘静⁴

1.
西南石油大学资源与环境学院, 四川成都 610500
2.
中国海洋大学海洋地球科学学院, 山东青岛 266003
3.
中国科学院广州地球化学研究所, 广东广州 510640
4.
西北大学地质系, 陕西西安 710069
5.
油气藏地质及开发工程国家重点实验, 四川成都 610500

基金项目:

中国石化总公司重大科技攻关项目"中国南方(中上扬子)大陆构造与海相油气前景" G0800-06-ZS281

详细信息

作者简介:
周小军(1978-), 男, 讲师, 主要从事含油气盆地构造解析方向研究.E-mail: zhouxiaojun2000@sina.com

中图分类号: P544
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- 被引次数: 0
出版历程
- 收稿日期: 2011-03-10
- 网络出版日期: 2021-11-10
- 刊出日期: 2011-06-15

Tectonic Features of the Fanjing Mount and Sangzhi Area on the West of Xuefeng Uplift

1.
School of Petroleum Engineering, Southwest Petroleum University, Chengdu 610500, China
2.
College of Marine Geosciences, Ocean University of China, Qingdao 266003, China
3.
Institute of Geochemistry, Chinese Academy of Science, Guangzhou 510640, China
4.
Department of Geology, Northwest University, Xi'an 710069, China
5.
State Key Laboratory of Oil and Gas Reservior Geology and Exploitation, Chengdu 610500, China

摘要

摘要: 梵净山—桑植地区是雪峰山西缘扩展构造带的一部分, 该区构造变形复杂, 阐明该地区构造变形特征, 不但能够更好的认识和理解江南—雪峰隆起带及其周缘的构造变形特征, 而且能够更好的指导我国南方海相油气勘探.本文通过对该区域复杂构造特征的详细解析, 厘定出该区发育了NEE-EW和NE走向两幕印支期变形, 以及NE向和NNE-NS走向两幕燕山期变形.结合区域大地构造背景, 认为印支期的构造变形, 主要与古特提斯洋的关闭、扬子板块与华北板块的剪刀式拼合有关; 燕山期的构造变形, 主要与伊泽奈崎板块和库拉-太平洋板块的俯冲有关.
- 扬子地块 /
- 雪峰隆起 /
- 构造 /
- 褶皱叠加 /
- 不整合 /
- 石油地质
Abstract: Our study area from the Fanjing Mountain to the Sangzhi County is a part of the propagation tectonic zone of the Xuefengshan Precambrian basement. Expounding the deformation in the area facilitates not only the understanding of the deformation in and around the Xuefengshan, but also the exploration in the marine strata in the southern China. Complex history of deformation in the area can be divided into two-stage Indosinian deformation and two-stage Yanshanian deformation. Two-stage Indosinian deformation is of NEE-EW- and NE-striking folding or faulting. Two-stage Yanshanian deformation is of NE- and NNE-NS-striking faulting or folding. Based on the structural analysis and the tectonic setting, this paper suggests that Indosinian deformation mechanism is mainly related to closing of Tethys Ocean and scissor-style collision of South China to North China plates; however, Yanshanian deformation mechanism is mainly related to northwestward subduction of Izanaqi plate and Kula-Pacific plate.
- Yangtze plate /
- Xuefeng uplift /
- tectonics /
- fold superimposition /
- unconformity /
- petroleum geology

HTML全文

图 1 梵净山地区构造简图

Ⅰ.雪峰山核部隆起带；Ⅱ.雪峰山西缘扩展带；Ⅲ.齐岳山隔槽式复合构造带；F₁.慈利-保靖断裂；F₂.龙里-印江断裂

Fig. 1. The structure map of Fanjing Mountain

下载: 全尺寸图片幻灯片

图 2 石门和酉阳附近加里东期平行不整合特征(图例见图 1)

Ⅱ.雪峰山西缘扩展带；Ⅲ.齐岳山隔槽式复合构造带；F₁.慈利-保靖断裂；F₂.龙里-印江断裂

Fig. 2. The Caledonian parallel unconformity near Shimen and Youyang

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图 3 石门和桑植附近印支期不整合特征(图例见图 1)

Ⅰ.雪峰山核部隆起带；Ⅲ.齐岳山隔槽式复合构造带；F₁.慈利-保靖断裂；F₂.龙里-印江断裂

Fig. 3. The Indo-Chinese unconformity near Shimen and Sangzhi

下载: 全尺寸图片幻灯片

图 4 印支期两幕褶皱发育特征

F₁.慈利-保靖断裂；F₂.龙里-印江断裂

Fig. 4. The feature of the two episodes deformation in Indosinian epoch

下载: 全尺寸图片幻灯片

图 5 桑植附近燕山期不整合特征

Fig. 5. The Yanshanian unconformity near Sangzhi

下载: 全尺寸图片幻灯片

图 6 燕山期二幕褶皱特征

F₁.慈利-保靖断裂；F₂.龙里-印江断裂

Fig. 6. The second episode deformation in Yanshan epoch

下载: 全尺寸图片幻灯片

图 7 酉阳—松桃剖面上断层发育特征

Fig. 7. The faults in the Youyang-Songtao profile

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图 8 研究区区印支—燕山期构造变形机制

a.印支期一幕变形机制；b.印支期二幕变形机制；c.燕山一幕变形机制；d.燕山二幕变形机制

Fig. 8. The deformation mechanism from Indosinian epoch to Yanshan epoch in this area

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