湘北桑植-石门一带早中生代褶皱叠加特征及变形机制

杨俊; 罗鹏; 凌跃新; 杨少辉; 柏道远; 魏方辉; 曹顺红; 彭能立

doi:10.19509/j.cnki.dzkq.2021.0605

湘北桑植-石门一带早中生代褶皱叠加特征及变形机制

doi: 10.19509/j.cnki.dzkq.2021.0605

基金项目:

中国地质调查局项目 DD20160029-17

湖南省地勘局科研项目 201901

详细信息

作者简介:
杨俊(1986-), 男, 工程师, 主要从事区域地质调查等方面的研究工作。E-mail: yj011064@163.com

通讯作者:
罗鹏(1987-), 男, 工程师, 主要从事区域地质调查等方面的研究工作。E-mail: 474672721@qq.com

中图分类号: P541
计量
- 文章访问数: 650
- PDF下载量: 193
- 被引次数: 0
出版历程
- 收稿日期: 2020-12-14

Superimposed features and deformation mechanism of Early Mesozoic folds in the Sangzhi-Shimen area, northern Hunan

摘要

摘要: 湘北桑植-石门一带下中生界连续发育一系列侏罗山式褶皱，褶皱叠加特征解析对探索桑植-石门复向斜褶皱变形期次及变形机制具有重要意义，同时对断裂控制褶皱变形的理论研究也具有启示意义。通过对桑植-石门一带地质构造剖面测制及褶皱叠加特征解析，识别出了印支期和早燕山期两期褶皱构造。研究区侏罗系与中三叠统之间的低角度不整合接触、白垩系与前白垩系之间的高角度不整合接触反映了印支运动和早燕山运动两期变形事件，可进一步推断桑植-石门一带褶皱可分为印支运动和早燕山运动两期。印支期褶皱轴迹主要呈北东东向-近东西向；早燕山期褶皱轴迹可分为2组：一组呈北东东向-近东西向；另一组呈北北东向。早燕山期2组褶皱与先期印支期褶皱叠加形成加强型和斜限型2种叠加类型，前者受控于印支期北东东向-近东西向逆断裂的继承性活动；后者受控于早燕山期北西西向区域挤压应力形成的北北东向逆断裂，且受限于先期北东东向-近东西向构造。此变形机制很好地解释了研究区褶皱轴面和逆冲断裂无向东或南东倾斜极性。
- 桑植-石门复向斜 /
- 叠加褶皱 /
- 构造解析 /
- 变形期次 /
- 变形机制
Abstract: A series of Jurassic-type folds have continuously developed in the Mesozoic from the Sangzhi-Shimen area in northern Hunan. The analysis of the fold superimposition characteristics is of great significance to explore the deformation period and deformation mechanism of the Sangzhi-Shimen complex oblique folds, and also for the theoretical study of fold deformation controlled by faults. Based on the measurement of geological structure section and analysis of fold superimposition characteristics in Sangzhi-Shimen area, two fold structures in Indosinian and early Yanshanian were identified. The low-angle unconformity contact between the Jurassic and the Middle Triassic in the study area, and the high-angle unconformity contact between the Cretaceous and the Pre-Cretaceous reflect two deformation events of Indosinian and Early Yanshanian movement. It can be further inferred that the folds in the Sangzhi-Shimen area can be divided into two phases: the Indosinian movement and the early Yanshanian movement.The Indosinian fold axial trace mainly showed NEE to near EW; the early Yanshanian fold axial trace can be divided into two groups, one is NEE-near EW, the other is NNE. Two groups of early Yanshanian folds and pre Indosinian folds are superimposed to form two types of superposed folds, the enhanced type and the oblique limited type. The former is controlled by the inherited activities of the Indosinian NEE-near EW reverse fault; the latter is controlled by NNE trending reverse fault, which formed by NWW trending regional compressive stress in early Yanshanian, and it is limited by the pre NEE-near EW trending structure.This deformation mechanism well explains that the fold axis and thrust fault in the study area have no east or Southeast inclined polarity.
- Sangzhi-Shimen complex syncline /
- superposed fold /
- structural analysis /
- deformation period /
- deformation mechanism

HTML全文

图 1 研究区大地构造位置暨构造纲要图

Q.第四系; K-E.白垩纪-古近纪构造层; T₃-J.晚三叠世-侏罗纪构造层; D-T₂.泥盆纪-中三叠世构造层; Nh-S.南华纪-志留纪构造层; Qb₂B.青白口纪板溪期构造层; Qb₁L.青白口纪冷家溪期构造层; 1.平行不整合接触线; 2.角度不整合接触线；3.背斜轴迹; 4.向斜轴迹; 5.逆断裂; 6.左行平移断裂; 7.右行平移断裂; 8.地质构造剖面; 9.褶皱编号; 10.断裂编号; 11.研究区；12.地名。褶皱编号及名称: f₁.新街背斜; f₂.谷罗山向斜; f₃.砂坝背斜; f₄.淋溪河背斜; f₅.桑植向斜; f₆.人潮溪背斜; f₇: 瑞塔铺向斜; f₈: 石堤向斜; f₉: 教字垭背斜; f₁₀: 长茅山向斜; f₁₁: 三坪背斜; f₁₂: 尹家溪背斜; f₁₃: 天子山向斜; f₁₄: 观音山背斜; f₁₅: 九渡河向斜; f₁₆: 四方台向斜; f₁₇: 雁池背斜; f₁₈: 火连坡向斜; f₁₉: 洞市向斜; f₂₀: 杨家坊向斜; f₂₁: 方石坪背斜; f₂₂: 码头铺背斜; f₂₃: 朱家沟向斜; f₂₄: 英塔背斜; f₂₅: 国太桥背斜; f₂₆: 皂市背斜; f₂₇: 三官寺向斜; f₂₈: 新铺向斜; f₂₉: 长岭向斜; f₃₀: 苗市倒转背斜; f₃₁: 杜家沟倒转向斜; f₃₂: 杉板向斜; f₃₃: 卞家岗向斜。断裂编号及名称: F₁.沙塔坪断裂; F₂.大塔坪断裂; F₃.教字垭断裂; F₄.新桥断裂; F₅.慈利-保靖断裂; F₆.皂市断裂; F₇.新铺断裂; F₈.雁池断裂; F₉.辛银断裂

Figure 1. Geotectonic location and structure outline map of the study area

下载: 全尺寸图片幻灯片

图 2 艾家湾-辛银地质构造剖面(GP01，剖面位置见图 1)

Qhj.全新统橘子洲组；K.白垩系; J₁b.下侏罗统白田坝组; T₂b.中三叠统巴东组; T₁j.下三叠统嘉陵江组; T₁d.下三叠统大冶组; P.二叠系; D.泥盆系; S.志留系; 1.角度不整合接触界线; 2.平行不整合接触界线; 3.断裂及编号; 4.飞来峰; 5.岩层产状；6.皱褶编号

Figure 2. Geological profile of Aijiawan-Xinyin

下载: 全尺寸图片幻灯片

图 3 淋溪河-三官寺地质构造剖面^[27](GP02，剖面位置见图 1, 褶皱同图 1)

T₂b.中三叠统巴东组; T₁j.下三叠统嘉陵江组; T₁d.下三叠统大冶组; P_2-3.中-上二叠统; D.泥盆系; S.志留系; P.奥陶系; ∈.寒武系; S₀.岩层产状；S₁.劈理产状; 1.逆断裂; 2.岩层产状; 3.断裂破碎带；F_r.人潮溪断裂

Figure 3. Geological profile of Linxihe-Sanguansi

下载: 全尺寸图片幻灯片

图 4 瑞塔铺向斜两翼次级褶皱特征

a.瑞塔铺向斜北西翼次级重力滑脱褶皱; b.瑞塔铺向斜北西翼断裂构造形成褶皱

Figure 4. Characteristics of secondary folds on both wings of Ruitapu syncline

下载: 全尺寸图片幻灯片

图 5 教字垭-沙塔坪构造剖面(GP03，剖面位置见图 1，褶皱和断裂同图 1)

F_c.陈家湾断裂

Figure 5. Geological profile of Jiaoziya-Shataping

下载: 全尺寸图片幻灯片

图 6 谷罗山向斜两翼发育次级褶皱

Figure 6. Secondary folds on both wings of the Guluoshan syncline

下载: 全尺寸图片幻灯片

图 7 石门界溪河下侏罗统白田坝组(J₁b)与中三叠统巴东组(T₂b)呈低角度不整合接触

①含砾石英砂岩；②泥岩；③页岩

Figure 7. Low angle unconformity contact relationship between the Jurassic Baitianba Formation and Triassic Badong Formation in Jiexihe, Shimen

下载: 全尺寸图片幻灯片

图 8 石门双溪桥中白垩统罗镜滩组(K₂lj)与下三叠统大冶组(T₁d)呈大角度不整合接触

①砾岩；②泥晶灰岩

Figure 8. High angle unconformity contact relationship between the Cretaceous Luojingtan Formation and Triassic Daye Formation in Shuangxiqiao, Shimen

下载: 全尺寸图片幻灯片

图 9 叠加褶皱分类^[49-50]

Figure 9. Classification of superposed folds

下载: 全尺寸图片幻灯片

图 10 变形机制示意图

(B₁, B₂同图 9)

Figure 10. Diagram of deformation mechanism

下载: 全尺寸图片幻灯片

参考文献(56)

[1]	柏道远, 熊雄, 杨俊, 等. 齐岳山断裂东侧盆山过渡带褶皱特征及其变形机制[J]. 大地构造与成矿学, 2015, 39(6): 1008-1021. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201506003.htm Bai D Y, Xiong X, Yang J, et al. Characteristics and dynamic mechanisms of the folds in the basin-mountain transition zone, east of the Qiyueshan fault[J]. Geotectonica et Metallogenia, 2015, 39(6): 1008-1021(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201506003.htm
[2]	冯常茂, 刘进, 宋立军. 中上扬子地区构造变形带成因机制及有利油气勘探区域预测[J]. 地球学报, 2008, 29(2): 199-204. doi: 10.3321/j.issn:1006-3021.2008.02.010 Feng C M, Liu J, Song L J. Formation mechanism of the tectonic deformation belt and the prognosis of favorable oil and gas exploration areas in the Middle and Upper Yangtze valley[J]. Acta Geoscientia Sinica, 2008, 29(2): 199-204(in Chinese with English abstract). doi: 10.3321/j.issn:1006-3021.2008.02.010
[3]	郭建华, 朱美衡, 刘辰生, 等. 湖南桑植-石门复向斜走廊剖面构造特征分析[J]. 大地构造与成矿学, 2005, 29(2): 215-222. doi: 10.3969/j.issn.1001-1552.2005.02.008 Guo J H, Zhu M H, Liu C S, et al. Structural characteristics of the corridor section in Sangzhi-Shimen synclinore[J]. Geotectonica et Metallogenia, 2005, 29(2): 215-222(in Chinese with English abstract). doi: 10.3969/j.issn.1001-1552.2005.02.008
[4]	刘学锋, 刘成鑫. 渝鄂湘边区构造样式分析[J]. 江汉石油学院学报, 2002, 24(2): 1-4. doi: 10.3969/j.issn.1000-9752.2002.02.001 Liu X F, Liu C X. Analysis of structural styles at the juncture of Chongqing, Hubei and Hunan[J]. Journal of Jianghan Petroleum Institute, 2002, 24(2): 1-4(in Chinese with English abstract). doi: 10.3969/j.issn.1000-9752.2002.02.001
[5]	梅廉夫, 刘昭茜, 汤济广, 等. 湘鄂西-川东中生代陆内递进扩展变形: 来自裂变径迹和平衡剖面的证据[J]. 地球科学: 中国地质大学学报, 2010, 35(2): 161-174. doi: 10.3969/j.issn.1672-6561.2010.02.008 Mei L F, Liu Z Q, Tang J G, et al. Mesozoic intra-continental progressive deformation in western Hunan-Hubei-eastern Sichuan provinces of China: Evience from apatite fission track and balanced cross-section[J]. Earth Science: Journal of China Uviversity of Geosciences, 2010, 35(2): 161-174(in Chinese with English abstract). doi: 10.3969/j.issn.1672-6561.2010.02.008
[6]	王宗秀, 张进, 关会梅, 等. 雪峰山西侧地区构造形变与油气圈闭[J]. 地质通报, 2012, 31(11): 1812-1825. doi: 10.3969/j.issn.1671-2552.2012.11.006 Wang Z X, Zhang J, Guan H M, et al. A discussion on the structural deformation and oil/gas traps on the western side of the Xuefeng Mountain[J]. Geological Bulletin of China, 2012, 31(11): 1812-1825(in Chinese with English abstract). doi: 10.3969/j.issn.1671-2552.2012.11.006
[7]	颜丹平, 汪新文, 刘友元. 川鄂湘边区褶皱构造样式及其成因机制分析[J]. 现代地质, 2000, 14(1): 37-43. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200001007.htm Yan D P, Wang X W, Liu Y Y. Analysis of fold style and its formation mechanism in the area of boundary among Sichuan, Hubei and Hunan[J]. Geoscience, 2000, 14(1): 37-43(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200001007.htm
[8]	颜丹平, 金哲龙, 张维宸, 等. 川渝湘鄂薄皮构造带多层拆离滑脱系的岩石力学性质及其对构造变形样式的控制[J]. 地质通报, 2008, 27(10): 1687-1697. doi: 10.3969/j.issn.1671-2552.2008.10.011 Yan D P, Jin Z L, Zhang W C, et al. Rock mechanical characteristics of the multi-layer detachment fault system and their controls on the structural deformation style of the Sichuan-Chongqing-Hunan-Hubei thin-skinned belt, South China[J]. Geological Bulletin of China, 2008, 27(10): 1687-1697(in Chinese with English abstract). doi: 10.3969/j.issn.1671-2552.2008.10.011
[9]	Yan D P, Zhou M F, Song H L, et al. Origin and tectonic significance of a Mesozoic multi-layer over-thrust system within the Yangtze Block (South China)[J]. Tectonophysics, 2003, 361: 239-254. doi: 10.1016/S0040-1951(02)00646-7
[10]	杨坤光, 李学刚, 戴传固, 等. 黔东南隔槽式褶皱成因分析[J]. 地学前缘, 2012, 19(5): 53-60. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201205008.htm Yang K G, Li X G, Dai C G, et al. Analysis of the origin of trough-like folds in southeast Guizhou[J]. Earth Science Frontiers, 2012, 19(5): 53-60(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201205008.htm
[11]	杨坤光, 李学刚, 戴传固, 等. 断层调整与控制作用下的叠加构造变形: 以贵州地区燕山期构造为例[J]. 地质科技情报, 2012, 31(5): 50-56. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201205008.htm Yang K G, Li X G, Dai C G, et al. Superimposition deformation controlled and adjusted by faults: An example from Yanshanian structural deformation in Guizhou Province[J]. Geological Science and Technology Information, 2012, 31(5): 50-56(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201205008.htm
[12]	张必龙, 朱光, 胡召齐, 等. 川东"侏罗山式"褶皱的数值模拟及成因探讨[J]. 地质论评, 2009, 55(5): 701-711. doi: 10.3321/j.issn:0371-5736.2009.05.012 Zhang B L, Zhu G, Hu Z Q, et al. Mumerical modeling and formation mechanism of the eastern Sichuan "Jura-type" folds[J]. Geological Review, 2009, 55(5): 701-711(in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.2009.05.012
[13]	胡召齐, 朱光, 刘国生, 等. 川东"侏罗山式"褶皱带形成时代: 不整合面的证据[J]. 地质论评, 2009, 55(1): 32-42. doi: 10.3321/j.issn:0371-5736.2009.01.004 Hu Z Q, Zhu G, Liu G S, et al. The folding time of the eastern Sichuan "Jura-type" fold belt: Evidence from unconformity[J]. Geological Review, 2009, 55(1): 32-42(in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.2009.01.004
[14]	刘恩山, 李三忠, 金宠, 等. 雪峰陆内构造系统燕山期构造变形特征和动力学[J]. 海洋地质与第四纪地质, 2010, 30(5): 63-74. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201005011.htm Liu E S, Li S Z, Jin C, et al. Yanshanian structural deformation and dynamics of the Xuefengshan intracontinental tectonic system[J]. Marine Geology & Quaternary Geology, 2010, 30(5): 63-74(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201005011.htm
[15]	刘丽萍, 李三忠, 戴黎明, 等. 雪峰山西侧贵州地区中生代构造特征及其演化[J]. 地质科学, 2010, 25(1): 228-242. doi: 10.3969/j.issn.0563-5020.2010.01.019 Liu L P, Li S Z, Dai L M, et al. Structural characteristics and evolution in Guizhou Province, west of Xuefeng Mountain[J]. Chinese Journal of Geology, 2010, 25(1): 228-242(in Chinese with English abstract). doi: 10.3969/j.issn.0563-5020.2010.01.019
[16]	周小军, 李三忠, 王岳军, 等. 雪峰山西侧梵净山-桑植地区构造变形特征[J]. 地球科学: 中国地质大学学报, 2011, 36(6): 985-992. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201106004.htm Zhou X J, Li S Z, Wang Y J, et al. Tectonic features of the Fanjing Mount and Sangzhi area on the west of Xuefeng uplift[J]. Earth Science: Journal of China University of Geoscience, 2011, 36(6): 985-992(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201106004.htm
[17]	柏道远, 蒋启生, 李彬, 等. 湘东北冷家溪群沉积岩地球化学特征及其构造意义[J]. 地质科技通报, 2021, 40(1): 1-13. https://dzkjqb.cug.edu.cn/CN/abstract/abstract10087.shtml Bai D Y, Jiang Q S, Li B, et al. Geochemistry and tectonic implication of the sedimentary rocks in Lengjiaxi Group in northeastern Hunan[J]. Bulletin of Geological Science and Technology, 2021, 40(1): 1-13(in Chinese with English abstract). https://dzkjqb.cug.edu.cn/CN/abstract/abstract10087.shtml
[18]	柏道远, 李银敏, 钟响, 等. 湖南NW向常德-安仁断裂的地质特征、活动历史及构造性质[J]. 地球科学, 2018, 43(7): 2496-2517. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201807022.htm Bai D Y, Li Y M, Zhong X, et al. Geological features, activity history and tectonic attribute of NW-trending Changde-Anren fault in Hunan[J]. Earth Science, 2018, 43(7): 2496-2517(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201807022.htm
[19]	孟庆秀, 张健, 耿建珍, 等. 湘中地区冷家溪群和板溪群锆石U-Pb年龄、Hf同位素特征及对华南新元古代构造演化的意义[J]. 中国地质, 2013, 40(1): 191-216. doi: 10.3969/j.issn.1000-3657.2013.01.014 Meng Q X, Zhang J, Geng J Z, et al. Zircon U-Pb age and Hf isotope compositions of Lengjiaxi and Banxi Groups in middle Hunan Province: Implications for the Neoproterozoic tectonic evolutionin South China[J]. Geology in China, 2013, 40(1): 191-216(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2013.01.014
[20]	柏道远, 贾宝华, 刘伟, 等. 湖南城步火成岩锆石SHRIMP U-Pb年龄及其对江南造山带新元古代构造演化的约束[J]. 地质学报, 2010, 84(12): 1715-1726. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201012001.htm Bai D Y, Jia B H, Liu W, et al. Zircon SHRIMP U-Pb dating of the igneous rocks from Chengbu, Hunan: Constraints on the Neoproterozoic tectonic evolution of Jiangnan Orogenic Belt[J]. Acta Geologica Sinica, 2010, 84(12): 1715-1726(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201012001.htm
[21]	王剑, 刘宝珺, 潘桂棠. 华南新元古代裂谷盆地演化: Rodinia超大陆解体的前奏[J]. 矿物岩石, 2001, 21(3): 135-145. doi: 10.3969/j.issn.1001-6872.2001.03.021 Wang J, Liu B J, Pan G T. Neoproterozoic rifting history of South China significance to Rodinia breakup[J]. Mineral Petrol., 2001, 21(3): 135-145(in Chinese with English abstract). doi: 10.3969/j.issn.1001-6872.2001.03.021
[22]	陈洪德, 侯明才, 许效松, 等. 加里东期华南的盆地演化与层序格架[J]. 成都理工大学学报: 自然科学版, 2006, 33(1): 1-8. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200601000.htm Chen H D, Hou M C, Xu X S, et al. Tectonic evolution and sequence stratigraphic framework in South China during CaledonianJ\]. Journal of Chengdu University of Technology: Science & Technology Edition, 2006, 33(1): 1-8(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200601000.htm
[23]	葛祥英, 牟传龙, 周恳恳, 等. 湖南奥陶纪沉积演化特征[J]. 中国地质, 2013, 40(6): 1829-1841. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201306013.htm Ge X Y, Mo C L, Zhou K K, et al. Characteristics of Ordovician sedimentary evolution in Hunan Province[J]. Geology in China, 2013, 40(6): 1829-1841(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201306013.htm
[24]	湖南省地质矿产局. 湖南省岩石地层[M]. 武汉: 中国地质大学出版社, 1997. Bureau of Geology and Mineral Resources of Hunan Province. Stratigraphy (lithostractic) of Hunan Province[M]. Wuhan: China University of Geosciences Press, 1997(in Chinese).
[25]	湖南省地质调查院. 中国区域地质志·湖南志[M]. 北京: 地质出版社, 2017. Hunan Institute of Geology Survey. The regional geology of China, Hunan Province[M]. Bejing: Geological Publishing House, 2017(in Chinese).
[26]	柏道远, 李长安, 王先辉, 等. 第四纪洞庭盆地澧县凹陷构造活动特征及动力学机制探讨[J]. 地球学报, 2010, 31(1): 43-55. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201001008.htm Bai D Y, Li C A, Wang X H, et al. Tectonic activities and dynamic mechanisms of the Quaternary Lixian Sag of Dongting Basin[J]. Acta Geoscientica Sinica, 2010, 31(1): 43-55(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201001008.htm
[27]	魏方辉, 马爱军, 杨少辉, 等. 1: 5万官地坪地区区域地质矿产调查成果报告[R]. 长沙: 湖南省地质调查院, 2016. Wei F H, Ma A J, Yang S H, et al. Report of 1: 50000 regional geological and mineral surveying Guandiping area[R]. Changsha: Hunan Insitute of Geology Survey, 2016(in Chinese).
[28]	柏道远, 黄建中, 刘耀荣, 等. 湘东南及湘粤赣边区中生代地质构造发展框架的厘定[J]. 中国地质, 2005, 32(4): 557-570. doi: 10.3969/j.issn.1000-3657.2005.04.004 Bai D Y, Huang J Z, Liu Y R, et al. Framework of Mesozoic tectonic evolution in southeastern Hunan and the Hunan-Guangdong-Jiangxi border area[J]. Geology in China, 2005, 32(4): 557-570(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2005.04.004
[29]	柏道远, 贾宝华, 王先辉, 等. 湘中盆地西部构造变形的运动学特征及成因机制[J]. 地质学报, 2013, 87(12): 1791-1802. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201312002.htm Bai D Y, Jia B H, Wang X H, et al. Kinematics of tectonic deformations of the western Xiangzhong Basin and its tectonic mechanisms[J]. Acta Geologica Sinica, 2013, 87(12): 1791-1802(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201312002.htm
[30]	柏道远, 贾宝华, 钟响, 等. 湘东南印支运动变形特征研究[J]. 地质论评, 2012, 58(1): 19-29. doi: 10.3969/j.issn.0371-5736.2012.01.002 Bai D Y, Jia B H, Zhong X, et al. Study on the deformation of Indosinian Movement in southeastern Hunan[J]. Geological Review, 2012, 58(1): 19-29(in Chinese with English abstract). doi: 10.3969/j.issn.0371-5736.2012.01.002
[31]	柏道远, 姜文, 钟响, 等. 湘西沅麻盆地中新生代构造变形特征及区域地质背景[J]. 中国地质, 2015, 42(6): 1851-1875. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201506014.htm Bai D Y, Jiang W, Zhong X, et al. Mesozoic-Cenozoic structural deformation characteristics of Yuanling-Mayang Basin and regional tectonic setting[J]. Geology in China, 2015, 42(6): 1851-1875(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI201506014.htm
[32]	柏道远, 熊雄, 姜文. 湘中南大庙口地区构造变形特征及其对区域页岩气构造保存条件的启示[J]. 地质科学, 2018, 53(2): 510-530. Bai D Y, Xiong X, Jiang W. Geological structure characteristics of Damiaokou area in central-southern Hunan and their significance toregional shale gas preservation conditions[J]. Chinese Journal of Geology, 2018, 53(2): 510-530(in Chinese with English abstract).
[33]	张国伟, 郭安林, 董云鹏, 等. 大陆地质与大陆构造和大陆动力学[J]. 地学前缘, 2011, 18(3): 1-12. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103003.htm Zhang G W, Guo A L, Dong Y P, et al. Continental geology, tectonics and dynamics[J]. Earth Science Frontiers, 2011, 18(3): 1-12(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201103003.htm
[34]	柏道远, 陈建成, 孟德保, 等. 湖南炎陵印支期隔槽式褶皱形成机制[J]. 地球科学与环境学报, 2006, 28(4): 10-14. doi: 10.3969/j.issn.1672-6561.2006.04.002 Bai D Y, Chen J C, Meng D B, et al. Forming mechanism of indosinian trouhg-like folds in Yanling region, Hunan[J]. Journal of Earth Sciences and Environment, 2006, 28(4): 10-14(in Chinese with English abstract). doi: 10.3969/j.issn.1672-6561.2006.04.002
[35]	柏道远, 黄建中, 王先辉, 等. 湖南邵阳-郴州北西向左旋走滑暨水口山-香花岭南北向构造成因[J]. 中国地质, 2006, 33(1): 56-63. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200601005.htm Bai D Y, Huang J Z, Wang X H, et al. Sinistral strike-slip motion of the NW-trending Saoyang-Chenzhou fault and genesis of the N-S-trending Shuikoushan-Xianghualing tectonic zone in Hunan[J]. Geology in China, 2006, 33(1): 56-63(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200601005.htm
[36]	柏道远, 李建清, 周柯军, 等. 祁阳山字型构造质疑[J]. 大地构造与成矿学, 2008, 32(3): 265-275. doi: 10.3969/j.issn.1001-1552.2008.03.002 Bai D Y, Li J Q, Zhou K J, et al. Query of Qiyang E-type tectonic system in Hunan[J]. Geotectonica et Metallogenia, 2008, 32(3): 265-275(in Chinese with English abstract). doi: 10.3969/j.issn.1001-1552.2008.03.002
[37]	柏道远, 熊雄, 杨俊, 等. 雪峰造山带中段地质构造特征[J]. 中国地质, 2014, 41(2): 399-418. doi: 10.3969/j.issn.1000-3657.2014.02.008 Bai D Y, Xiong X, Yang J, et al. Geological structure characteristics of the middle segment of the Xuefeng Orogen[J]. Geology in China, 2014, 41(2): 399-418(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2014.02.008
[38]	柏道远, 钟响, 贾朋远, 等. 雪峰造山带靖州盆地断裂构造及其形成背景探讨[J]. 大地构造与成矿学, 2013, 37(2): 173-183. doi: 10.3969/j.issn.1001-1552.2013.02.001 Bai D Y, Zhong X, Jia P Y, et al. The faults in Jinzhou Basin and their tectonic settings[J]. Geotectonica et Metallogenia, 2013, 37(2): 173-183(in Chinese with English abstract). doi: 10.3969/j.issn.1001-1552.2013.02.001
[39]	柏道远, 钟响, 贾朋远, 等. 雪峰造山带南段构造变形研究[J]. 大地构造与成矿学, 2014, 38(3): 512-529. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201403003.htm Bai D Y, Zhong X, Jia P Y, et al. Study on the deformation in the southern Xuefeng Orogenic Belt[J]. Geotectonica et Metallogenia, 2014, 38(3): 512-529(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201403003.htm
[40]	柏道远, 邹宾微, 赵龙辉, 等. 湘东太湖逆冲推覆构造基本特征研究[J]. 中国地质, 2009, 36(1): 53-64. doi: 10.3969/j.issn.1000-3657.2009.01.003 Bai D Y, Zou B W, Zhao L H, et al. Basic characteristics of the Taihu thrust system in eastern Hunan[J]. Geology in China, 2009, 36(1): 53-64(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2009.01.003
[41]	柏道远, 倪艳军, 李送文, 等. 江南造山带北部早中生代岳阳-赤壁断褶带构造特征及变形机制研究[J]. 中国地质, 2009, 36(5): 996-1009. doi: 10.3969/j.issn.1000-3657.2009.05.005 Bai D Y, Ni Y J, Li S W, et al. A geometrical and kinematic analysis of the Early-Mesozoic Yueyang-Chibi fold-thrust belt in southern Jiangnan Orogen[J]. Geology in China, 2009, 36(5): 996-1009(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2009.05.005
[42]	徐政语, 林舸, 刘池阳, 等. 从江汉叠合盆地构造形变特征看华南与华北陆块的拼贴过程[J]. 地质科学, 2004, 39(2): 284-295. doi: 10.3321/j.issn:0563-5020.2004.02.015 Xu Z Y, Lin G, Liu C Y, et al. A discussion on amalgamation course between the South China and north China blocks: Evidences from deformational characters in the Jianghan Superimposed Basin[J]. Chinese Journal of Geology, 2004, 39(2): 284-295(in Chinese with English abstract). doi: 10.3321/j.issn:0563-5020.2004.02.015
[43]	张岳桥, 徐先兵, 贾东, 等. 华南早中生代从印支期碰撞构造体系向燕山期俯冲构造体系转换的形变记录[J]. 地学前缘, 2009, 16(1): 234-247. doi: 10.3321/j.issn:1005-2321.2009.01.026 Zhang Y Q, Xu X B, Jia D, et al. Deformation record of the change from Indosinian collision-related tectonic system to Yanshanian subduction-related tectonic system in South China during the Early Mesozoic[J]. Earth Science Frontiers, 2009, 16(1): 234-247(in Chinese with English abstract). doi: 10.3321/j.issn:1005-2321.2009.01.026
[44]	魏方辉, 杨少辉, 赵伟, 等. 石门-桑植复向斜若干个不整合面特征及其对构造演化过程和盆地属性的启示[J]. 地层学杂志, 2018, 42(1): 75-89. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201801010.htm Wei F H, Yang S H, Zhao W, et al. Late Early Paleozoic-Mesozoic stratigraphic unconformities in the Shimen-Sangzhi synclinorium and their implications for tectonic and basin evolution[J]. Journal of Stratigraphy, ,2018, 42(1): 75-89(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201801010.htm
[45]	柏道远, 钟响, 贾朋远, 等. 湘东南晚三叠世-侏罗纪沉积特征及盆地性质和成因机制[J]. 地质力学学报, 2011, 17(4): 338-349. doi: 10.3969/j.issn.1006-6616.2011.04.004 Bai D Y, Zhong X, Jia P Y, et al. Sedimentary characteristics, basin type and dynamic mechanisms during Late Triassic-Jurassic in soueastern Hunan[J]. Journal of Geomechanics, 2011, 17(4): 338-349(in Chinese with English abstract). doi: 10.3969/j.issn.1006-6616.2011.04.004
[46]	舒良树, 周新民. 中国东南部晚中生代构造作用[J]. 地质论评, 2002, 48(3): 249-260. doi: 10.3321/j.issn:0371-5736.2002.03.004 Shu L S, Zhou X M. Late Mesozoic tectonism of southeast China[J]. Geological Review, 2002, 48(3): 249-260(in Chinese with English abstract). doi: 10.3321/j.issn:0371-5736.2002.03.004
[47]	舒良树, 周新民, 邓平, 等. 中国东南部中、新生代盆地特征与构造演化[J]. 地质通报, 2004, 23(9/10): 876-884. https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2007.htm Shu L S, Zhou X M, Deng P, et al. Geological features and tectonic evolution of Meso-Cenozoic basins in southeastern China[J]. Geological Bulletin of China, 2004, 23(9/10): 876-884(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD2004Z2007.htm
[48]	徐先兵, 张岳桥, 贾东, 等. 华南早中生代大地构造过程[J]. 中国地质, 2009, 36(3): 573-593. doi: 10.3969/j.issn.1000-3657.2009.03.007 Xu X B, Zhang Y Q, Jia D, et al. Early Mesozoic geotectonic processes in South China[J]. Geology in China, 2009, 36(3): 573-593(in Chinese with English abstract). doi: 10.3969/j.issn.1000-3657.2009.03.007
[49]	孙东, 刘树根, 邓宾, 等. 米仓山与龙门山接合部叠加褶皱特征及构造演化[J]. 成都理工大学学报: 自然科学版, 2011, 38(2): 156-168. doi: 10.3969/j.issn.1671-9727.2011.02.007 Sun D, Liu S G, Deng B, et al. Superposed fold characteristics and structural evolution in the junction area of Longmenshan Mountains and Micangshan Mountains in the southwest of China[J]. Journal of Chengdu University of Technoogy: Science & Technology Edition, 2011, 38(2): 156-168(in Chinese with English abstract). doi: 10.3969/j.issn.1671-9727.2011.02.007
[50]	曾广乾, 梁恩云, 陈勋, 等. 湘南江永地区多期褶皱的变形特征及叠加关系[J]. 地质科技情报, 2019, 38(4): 153-165. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904016.htm Zeng G Q, Liang E Y, Chen X, et al. Structural style and superposed relationship of multi-period folds in Jiangyong area, southern Hunan Province[J]. Geological Science and Technology Information, 2019, 38(4): 153-165(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904016.htm
[51]	陈剑, 卢华复, 于景宗, 等. 断层相关褶皱的几何学模型及其应用[J]. 地球学报, 2005, 26(1): 89-92. doi: 10.3321/j.issn:1006-3021.2005.01.014 Chen J, Lu H F, Yu J Z, et al. Geometric models of falt-related folds and their application[J]. Acta Geoscientica Sinica, 2005, 26(1): 89-92(in Chinese with English abstract). doi: 10.3321/j.issn:1006-3021.2005.01.014
[52]	何登发, John S, 贾承造. 断层相关褶皱理论与应用研究新进展[J]. 地学前缘, 2005, 12(4): 353-364. doi: 10.3321/j.issn:1005-2321.2005.04.004 He D F, John S, Jia C Z. New advances in theory and application of fault-related folding[J]. Earth Science Frontier, 2005, 12(4): 353-364(in Chinese with English abstract). doi: 10.3321/j.issn:1005-2321.2005.04.004
[53]	齐小兵, 翟文建, 章泽军. 慈利-保靖断裂带的性质及其演化[J]. 地质科技情报, 2009, 28(2): 54-59. doi: 10.3969/j.issn.1000-7849.2009.02.010 Qi X B, Zhai W J, Zhang Z J. Geological properties and evolution of Cili-Baojing fault zone[J]. Geological Science and Technology Information, 2009, 28(2): 54-59(in Chinese with English abstract). doi: 10.3969/j.issn.1000-7849.2009.02.010
[54]	杨坤光, 何良伦, 刘雨, 等. 黔西逆冲滑脱构造及其对铅锌矿床的控制[J]. 地质科技通报, 2020, 39(1): 149-156. https://dzkjqb.cug.edu.cn/CN/abstract/abstract9935.shtml Yang K G, He L L, Liu Y, et al. The thrust-decollement structure in western Guizhou and its control of Pb-Zn deposit[J]. Bulletin of Geological Science and Technology, 2020, 39(1): 149-156(in Chinese with English abstract). https://dzkjqb.cug.edu.cn/CN/abstract/abstract9935.shtml
[55]	易顺华, 袁晏明. 层间滑动褶皱研究新见解[J]. 地质科技情报, 2006, 25(1): 59. doi: 10.3969/j.issn.1000-7849.2006.01.021 Yi S H, Yuan Y M. New views on the study of interlayer sliding folds[J]. Geological Science and Technology Information, 2006, 25(1): 59(in Chinese with English abstract). doi: 10.3969/j.issn.1000-7849.2006.01.021
[56]	张旭亮, 何登发. 桑植-石门复向斜的形成与演化[J]. 地质科学, 2018, 53(1): 269-288. https://www.cnki.com.cn/Article/CJFDTOTAL-JSZD201801003.htm Zhang X L, He D F. Formation and evolution of Sangzhi-Shimen complex syncline[J]. Chinese Journal of Geology, 2018, 53(1): 269-288(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-JSZD201801003.htm