[1]聂冠军,杨仕升,张沛全.2019.右江地区新生代走滑断裂活动特征及其构造意义.大地构造与成矿学,43(6):1094-1105.doi:10.16539/j.ddgzyckx.2019.06.002
 NIE Guanjun,YANG Shisheng,ZHANG Peiquan and LI Bingsu.2019.Characteristics and Tectonic Significance of Cenozoic Strike-slip Faults in Youjiang Region.Geotectonica et Metallogenia,43(6):1094-1105.doi:10.16539/j.ddgzyckx.2019.06.002
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右江地区新生代走滑断裂活动特征及其构造意义
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2019年43卷06期
页码:
1094-1105
栏目:
构造地质学
出版日期:
2019-12-15

文章信息/Info

Title:
Characteristics and Tectonic Significance of Cenozoic Strike-slip Faults in Youjiang Region
文章编号:
1001-1552(2019)06-1094-012
作者:
聂冠军12 杨仕升12* 张沛全12 李冰溯12
1.广西壮族自治区地震局, 广西 南宁 530022; 2.广西工程防震研究院, 广西 南宁530022
Author(s):
NIE Guanjun12 YANG Shisheng12* ZHANG Peiquan12 and LI Bingsu12
1. Earthquake Administration of Guangxi Zhuang Autonomous Region, Nanning 530022, Guangxi, China; 2. Guangxi Academy of Engineering Shock Prevention, Nanning 530022, Guangxi, China
关键词:
右江地区 走滑断裂 运动学涡度 块体
Keywords:
Youjiang region strike-slip fault vorticity block
分类号:
P542
DOI:
10.16539/j.ddgzyckx.2019.06.002
文献标志码:
A
摘要:
右江地区位于华南、川滇和印支三个活动块体的结合部位, 新生代该区发育一系列北西向左旋走滑断裂及伴生盆地。这些断裂近等间距分布, 将右江地区分割成多个长条形区间, 断裂活动又导致各区间相互发生左行运动。根据这些断裂的走滑错移量以及伴生盆地的拉分量, 计算获得区域应变和动力学涡度。研究结果表明右江地区在新生代整体发生无旋转的简单剪切变形, 其最大主张应变为近南北向。新生代以来, 右江地区先后受到印支块体和川滇块体侧向挤出的影响, 右江地区的单剪变形和区内的北西向断裂活动正是这两个块体共同作用的结果, 同时也是印度–欧亚板块碰撞产生的连锁反应之一。
Abstract:
The Youjing area is in the southwestern most portion of the South China Block, bordering the Indochina Block on the southwest and the Xichuan-Yunnan Block on the northwest. A set of NW-striking transcurrent faults, as well as their associated basins, formed in the area during the Cenozoic. They are approximately evenly spaced and left-lateral. Strain and vorticity analyses of these faults indicate that the study area has undergone irrotational simple-shear deformation, where the maximum principal strain axis has a nearly north direction, as a whole. This deformation mode is likely resulted from the southeastward extrusion of the Indochina Block and the Xichuan-Yunnan Block in response to the Cenozoic India-Eurasia collision.

参考文献/References:

陈洪德, 曾允孚. 1990. 右江沉积盆地的性质及演化讨论. 岩相古地理, 11(1): 28-37.
蔡舜天, 郭亦秋. 1984. 广西百色盆地石油地质概述. 石油与天然气地质, 5(4): 362-371.
戴传固, 秦守荣, 陈建书, 卢定彪. 2013. 试论贵州深部隐伏断裂特征. 地质科技情报, 32(6): 1-13.
丁国瑜, 卢演俦. 1991. 中国岩石圈动力学概论. 北京: 地震出版社: 142-153.
杜远生, 黄宏伟, 黄志强, 徐亚军, 杨江海, 黄虎. 2009. 右江盆地晚古生代-三叠纪盆地转换及其构造意义. 地质科技情报, 28(6): 10-15.
广西壮族自治区地质矿产局. 1985. 广西壮族自治区地质志. 北京: 地质出版社: 713-852.
广西壮族自治区地方志编纂委员会. 1990. 广西通志(地震志). 桂林: 广西人民出版社: 10-28.
黄虎, 杜远生, 杨江海, 陶平, 黄宏伟, 胡丽沙, 谢春霞. 2012. 水城-紫云-南丹裂陷盆地晚古生代硅质沉积物地球化学特征及其地质意义. 地质学报, 86(12): 1994-2010.
侯建军, 白太绪. 1993. 伸展型构造盆地形成与演化的几何学和运动学研究//北京大学地质系. 岩石圈地质科学. 北京: 地震出版社: 43-51.
侯建军, 刘锡大, 游象照, 秦火保. 1993. 桂西活动走滑断裂系的地表变形组合特征及其与地震活动的关系.地震学报, 15(1): 119-122.
柯成熙. 1984. 挤出构造——一种新的中国构造观. 四川地震, 40(4): 40-42.
林金录. 1988. 华南地块和印支地块相对运动的古地磁证据. 地震地质, 10(3): 3-9.
刘锡大, 侯建军, 游象照. 1987. 右江断裂带的新构造活动. 地震研究, 10(2): 175-183.
苗崇刚, 李伟琦, 李青春. 2015. 广西简明地震信息手册. 南宁: 接力出版社: 1-40.
毛健全, 顾尚义, 张启厚. 1999. 右江-南盘江裂谷构造格局. 贵州地质, 16(3): 188-194.
宋方敏, 李传友, 陈献程, 张兰凤. 2004. 右江断裂带晚更新世活动的若干地质地貌证据及位移速率. 地震地质, 26(4): 611-620.
吴继远. 1983. 广西中新生代陆相盆地地质特征与构造演化. 中国区域地质, 6(1): 111-121.
王国芝, 胡瑞忠, 苏文超, 朱赖民. 2002. 滇-黔-桂地区右江盆地流体流动与成矿作用. 中国科学(D辑), 32(S1): 78-86.
汪一鹏, 沈军, 王琪, 熊熊. 2003. 川滇块体的侧向挤出问题. 地学前沿, 10(S1): 188-192.
徐锡伟, 程佳, 许冲, 陈桂华. 2014. 青藏高原块体运动模型与地震活动主体地区讨论: 鲁甸和景谷地震的启示. 地震地质, 36(4): 1116-1134.
云南省地质矿产局. 1990. 云南省区域地质志. 北京: 地质出版社: 558-562.
游象照. 1982. 广西活动性断裂的特征及其与地震关系. 华南地震, 2(3): 7-14.
杨振宇. 2001. 红河断裂两侧早第三纪古地磁研究及其地质意义. 地质学报, 75(1): 35-44.
张国伟, 郭安林, 王岳军, 李三忠, 董云鹏, 刘少峰, 何登发, 程顺有, 鲁如魁, 姚安平. 2013. 中国华南大陆构造与问题. 中国科学: 地球科学, 43(10): 1553- 1582.
张进江. 2005. 印度与欧亚大陆汇聚过程中走滑体系的活动历史及其地质意义. 中生代以来中国大陆板块作用过程学术研讨会.
张继淹. 2002. 广西地质构造稳定性分析与评价. 广西地质, 15(3): 1-7.
张连生, 钟大赉. 1996. 从红河剪切带走滑运动看东亚大陆新生代构造. 地质科学, 31(4): 327-341.
曾允孚, 刘文均, 陈洪德, 郑荣才, 张锦泉. 1995. 华南右江复合盆地的沉积构造演化. 地质学报, 69(2): 113- 123.
曾允孚, 刘文均. 1993. 华南右江盆地沉积构造演化. 北京: 地质出版社: 1-96.
赵仲如. 1981. 广西南宁盆地的脊椎动物化石及下第三系. 古脊椎动物与古人类, 19(3): 218-227.
Cheistie-Blick N and Biddle K T. 1985. Deformation and basin formation along strike-slip faults. The Society of Economic Paleontologists and Mineralogists, 37: 1-34.
Daly M C, Chorowicz J and Fairhead J D. 1989. Rift basin evolution in Africa: The influence of reactivated steep basement shear zones // Cooper M A and Williams G D. Inversion Tectonics. Geological Society, London, Special Publications, 44: 309-344.
Dorsey R J and Umhoefer P J. 2012. In?uence of sediment input and plate-motion obliquity on basin development along an active oblique-divergent plate boundary: Gulf of California and Salton Trough // Busby C and Azor A. Tectonics of Sedimentary Basins: Recent Advances. Blackwell Publishing Ltd: 209-225.
Guodun K, Gengjiao C and Yunfa C. 2004. New information on the tertiary biostratigraphy of the Ningming basin, Guangxi. Journal of Stratigraphy, 28(4): 362-367.
Huang H, Du Y S, Huang Z Q, Yang J H, Huang H W, Xie C X and Hu L S. 2013b. Depositional chemistry of chert during late Paleozoic from western Guangxi and its implication for the tectonic evolution of the Youjiang Basin. Science China: Earth Sciences, 56(3): 479-493.
Huang H, Du Y S, Yang J H, Huang H W, Tao P, Huang Z Q, Yu W C and Guo H. 2013a. Geochemistry of the Late Paleozoic cherts in the Youjiang Basin: Implications for the basin evolution. Geochemistry and Sedimentary Environment, 2(4): 402-421.
Liu M, Yang Y Q, Shen Z K, Wang S M and Wang M. 2007. Active tectonics and intracontinental earthquakes in China: The kinematics and geodynamics. Special Paper of the Geological Society of America, 425: 299- 318.
Nixon C W, Sanderson D J and Bull J M. 2011. Deformation within a strike-slip fault network at Westward Ho!, Devon UK: Domino vs conjugate faulting. Journal of Structural Geology, 33(5), 833-843.
O’driscoll E S T. 1986. Observations of the lineament-ore relation. Philosophical Transactions of the Royal Society, 317(1539): 195-218.
Peacock D P and Sanderson D J. 1993. Estimating strain from fault slip using a line sample. Journal of Structural Geology, 15(12): 1513-1516.
Pubellier M, Rangin C and Phung V P. 2003. The Cao Bang-Tien Yen fault implications on the relationships between the Red River and the South China coast belt. Advances in Natural Sciences, 4(4): 347-361.
Replumaz A and Tapponnier P. 2003. Reconstruction of the deformed collision zone Between India and Asia by backward motion of lithospheric blocks. Journal of Geophysical Research, 108(B6): 1-24.
Sylvester A G. 1988. Strike-slip faults. Geological Society of America Bulletin, 100: 1666-1703.
Tapponnier P, Peltzer G, Le Dain A Y, Armijo R and Cobbold P. 1982. Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine. Geology, 10(12): 611-616.
Umhoefer P J, Schwennicke T, Del Margo M T, Ruiz Geraldo G and Ingle J C. 2007. Transtensional fault-termination basins: An important basin type illustrated by the Pliocene San Jose island basin and related basins in the southern Gulf of California, Mexico. Basin Research, 19: 297-322.
Wysocka A. 2009. Sedimentary environments of the Neogene basins associated with the Cao Bang-Tien Yen Fault, NE Vietnam. Acta Geologica Polonica, 59(1): 45-69.
Wallis S R. 1995. Vorticity analysis and recognition of ductile extension in the Sanbagawa belt, SW Japan. Journal of Structural Geology, 17(8): 1077-1093.
Xypolias P. 2009. Some new aspects of kinematic vorticity analysis in naturally deformed quartzites. Journal of Structural Geology, 31(1): 3-10.
Xypolias P. 2010. Vorticity analysis in shear zones: A review of methods and applications. Journal of Structural Geology, 32(12): 2072-2092.

备注/Memo

备注/Memo:
收稿日期: 2017-12-07; 改回日期: 2018-03-12 项目资助: 中国地震局地震科技星火计划项目(XH192001Y)和广西科技计划项目(桂科AB17195022)联合资助。 第一作者简介: 聂冠军(1987–), 男, 博士, 从事构造地质学研究。Email: nieguanjun123@163.com 通信作者: 杨仕升(1960–), 男, 博士, 教授级高级工程师。Email: yangss01@163.com
更新日期/Last Update: 2019-12-15